CHAPTER IX.

MADRAS.

"Catamarans" and "Masuli" Boats.--Difficulty of Disembarkation,

and Plans for remedying it.--History.--Brahminism.--Festival

in Honour of Vishnù.--Employment of Heathens under a Christian

Government.--Politics and Religion.--Laws of Brahminic Faith.--

The Observatory.--Museum of Natural History and Zoological

Garden.--Academy of Fine Arts.--Medical School.--Infirmary.--

Orphan Asylum.--Dr. Bell.--Lancastrian Method of Teaching

Children first Applied in Madras.--Colonel Mackenzie's

Collection of Indian Inscriptions and MSS.--The Palace of the

former Nabob of the Coromandel Coast.--Journey by Rail to

Vellore.--_Féte_ given by the Governor in Guindy Park.--Visit

to the Monolithic Monuments of Mahamalaipuram.--Excursion to

Pulicat Lake.--Madras Club.--_Féte_ in Honour of the Members

of the _Novara_ Expedition.--"Tiffin" and Dance on Board.--

Departure from Madras.--Zodiacal Light.--Shrove Tuesday in the

Tropics.--Arrival at the Island of Kar-Nicobar. 424

LIST OF ILLUSTRATIONS.

VOL. I.

PAGE

The Track Of The Austrian Imperial Frigate

Novara. _frontispiece_

Letter. iii

Letter Continued. iv

Notes. xvi

Departure. 1

Gun-room of the _Novara_. 4

Plate: Vertical Section of the Frigate

"Novara". 7

Geodetical and Astronomical Instruments. 10

Look-out Man. 11

Track from Triest To Madeira. 11

"Palinurus". 16

Seamen off duty. 21

View of Gibraltar from Seaward. 28

Rock of Gibraltar. 29

Rock Cavern in Gibraltar. 34

South Gate, Gibraltar. 38

Inhabitant of Frangola. 47

Cape Trafalgar. 52

Loo Rock (Madeira). 57

Scene in Madeira. 58

Bridge over the Ribeiro Seco. 70

Carapuça, or Cap worn by the Natives of

Madeira. 91

Cathedral of Madeira. 95

Sleigh party in Madeira. 97

Village of Fayal. 99

"El Homem em pié". 101

Erica Trees. 103

Track From Madeira to Rio Di Janeiro. 107

Cape Frio. 120

The Quay at Rio. 121

Island of Paquità, Bay of Rio. 156

Track from Rio Di Janeiro to the Cape

Of Good Hope. 182

Cabo Tormentoso. 195

Cape Town. 196

Rifle Volunteer _Fête_ at Stellenbosch. 217

Paine's Kloef as it was. 220

Paine's Kloef as it is. 220

Crossing the Breede River. 226

Hot Springs of Brand Vley. 227

Hottentot Huts at Genaadendal. 233

Church and Mission Houses of the Moravian

Settlement at Genaadendal. 237

Tomb of a Malay Prophet at Zandvliet. 245

Interior of the Mausoleum. 246

Tsetse Fly. 252

Track from the Cape Of Good Hope to St. Paul's

Island. 259

Arrival at St. Paul. 266

View of St. Paul. 267

Distant view of Crater-Basin of St. Paul. 275

Rainy day at St. Paul. 300

Track from St. Paul to Point De Galle (Ceylon). 309

Cingalese Canoe. 344

View of Adam's Peak from Colombo. 345

Buddha Temple near Galle. 353

Interior of a House at Galle. 359

Track from Point De Galle To Madras. 418

Masuli Boat at Madras. 423

View of Madras (and Proposed Pier). 424

The Holy Mountain. 458

The god Ganeza. 461

Bivouac at Mahamalaipuran. 464

Bas-relief on one of the Monolith Temples. 467

Entrance to One of the Temples. 470

Track from Madras to the Nicobar Islands. 480

Arrival at Kar-Nicobar. 482

[Illustration: LETTER.]

Transcriber's Note: The text of the letter above, along with supplemental

address information, are in the first volume of the German edition:

Sr. Hochwohlgeboren

dem Herrn Oberst von Wüllerstorf,

kais. kön. Linienschiffs-Capitän,

Befehlshaber S. Maj. Fregatte Novara,

Ritter hoher Orden &c. &c. &c.

in

Triest.

Hochwohlgeborener Herr,

Hochzuverehrender Herr Oberst, k. k. Linien-Schiffs-Capitän.

Ew. Hochwohlgeb. wollen, als Befehlshaber Sr. Maj. Fregatte Novara, die zu

einem großen, edeln, das deutsche Vaterland und die Wissenschaft ehrenden

Unternehmen durch kaiserliche Huld bestimmt ist, den Ausdruck meiner

Verehrung nachsichtsvoll empfangen, indem ich, von der Zeit naher Abfahrt

in halber Genesung bedrängt, es wage, Ihnen einige _physikalische_ und

_geognostische Erinnerungen_ ganz gehorsamst vorzulegen, von denen Einiges

vielleicht den ausgezeichneten Gelehrten, die die Expedition zu begleiten

das Glück haben, von Nuzen sein kann. Ich würde dies Wenige nicht

angeboten haben, wenn eine so genädige und liebenswürdige Aufforderung Sr.

kaiserl. Hoheit des Herrn Erzherzogs Ferdinand Maximilian mich nicht dazu

bestimmt hätte. Was ich Nautisches über Richtung und Temperatur der

Meeresströhmungen, über die magnetischen Curven eingeflochten habe, muß

ich besonders _Ihrer_ Nachsicht empfehlen. Wenn man erinnert, scheint man

belehren zu wollen, und von dieser Anmaßung bin ich weit entfernt. Da kein

Entwurf, keine Abschrift meiner, wenigstens fleißigen, mit Zahlen

überladenen Arbeit existirt, so wäre es vielleicht vorsichtig, sie von

Jemand, der der behandelten Gegenstände kundig ist, abschreiben zu lassen.

Meine gelehrten und mir lieben Freunde Dr. Ferdinand Hochstetter, Dr. Karl

Scherzer und Dr. Robert Lallemant, der mich bei seiner letzten Durchreise

durch Berlin, um mir sein wichtiges Werk über das Gelbe Fieber in der

Tropenzone zu geben, verfehlt hat, wage ich dringend Ihrem besonderen

Schuze und Wohlwollen zu empfehlen.

Mit der innigsten Verehrung und den heißesten Wünschen für den Erfolg

eines so schön vorbereiteten Unternehmens

Ew. Hochwohlgeboren

gehorsamster

Al. Humboldt.

Berlin, den 7. April 1857 Nachts.

PHYSICAL AND GEOGNOSTIC SUGGESTIONS,

BY

ALEXANDER VON HUMBOLDT.

In compliance with the gracious invitation which H.I.H. the Archduke

Ferdinand Maximilian was pleased to address to me from Trieste (December

12th, 1856), and as yet barely recovered from an indisposition, I jot down

these hasty notes, without presuming to give definite instructions, such

as those I drew up, conjointly with M. Arago, for the guidance of the

French expeditions, or for Lord Minto, then First Lord of the Admiralty,

on the occasion of the Antarctic Voyage of Discovery of Sir James Ross

(1840-43). The following pages consist simply of hints which may possibly

prove serviceable to the distinguished and highly informed gentlemen, who

have the good fortune to sail on board the Imperial Frigate, _Novara_,

under the command of Commodore von Wüllerstorf. With two of these savans,

Dr. Ferdinand Hochstetter and Dr. Karl Scherzer, I have had the pleasure,

here in Berlin, to agree verbally on various subjects.

As I do not exactly know what course it is intended the _Novara_ shall

follow in navigating the Atlantic, nor in what meridian it is proposed to

cross the Equator, (in conformity with the sound and useful directions of

my friend Lieut. Maury, of Washington), on her voyage to Rio de Janeiro,

nor how near she shall keep to Cape San Roque and Fernando de Noronha, I

must content myself with inviting the attention of the voyagers in a

general way to the temperature of the sea, as also to the variations and

aberrations of the magnetic curves, and their currents.

A lower degree of temperature is usually observed W. of the Canaries, and

Cape Verde Islands, commencing with the Salvages, the thermometer

indicating as low as 72°·7 Fahr. This has been already ascertained by Mr.

Charles Deville, in his chart of temperature on the voyage "aux Antilles,

à Ténériffe et à Fogo." I consider this diminution of temperature results

from the North Guinea current, bringing with it cold water from the north

southwards as far as the Bight of Biafra and the River Gaboon, at which

point it is encountered by an opposite current flowing northwards along

the south-western coast of Africa from Loando and Congo.

In 1825, Captain Duperrey had accurately laid down the point of

intersection of the magnetic, with the terrestrial equator. In 1837, we

learned from Sabine's investigations of magnetic inclination near the

Island of St. Thomas (on the Equator, adjoining the above portion of the

coast of Africa), that this point of intersection had already shifted

four degrees to the westward. A period of twenty years having elapsed

since Sabine's expedition for determining observations with the pendulum,

it would be most desirable that fresh investigations should be made in

that neighbourhood, for the purpose of verifying the secular changes of

all magnetic curves, especially with regard to their variation. In 1840,

the line of no declination in America began 9° 30' E. of South Georgia,

whence it ran to the S.E. coast of Brazil, near Cape Frio, thus traversing

the mainland of South America only between the latter point and the

parallel of 0° 36' S., when it leaves the continent a little to the east

of Gran Parà, near Cape Tigioca, cutting the terrestrial equator again,

but in 50° 6' W. According to Bache's Map of Equal Magnetic Declination,

it reaches the coast of North America near Cape Fear, to the south-west of

Cape Lookout. This line, along which the magnetic declination is _nil_,

extends to a point in Lake Erie, 2° 40' W. of Toronto, where the

declination is already 1° 27' W.[2]

[Footnote 2: Wherever, in this paper, it is not precisely expressed to the

contrary, the scale of the Centigrade Thermometer, the longitude from the

Meridian of Paris, the French foot (_pied du roi_=12·79 inches English),

and the geographical mile, 15 to a degree of the Equator, measuring 3807

"toises," are meant.]

It is evident from the observations of Captains Beechey and Findley, and

still more particularly from those of the French Captain Kerhallet, that

the remarkable subdivision of the main equinoctial current, flowing from

east to west into two branches, one directed to the N.W., the other to the

S.S.W., commences at a considerable distance from the Capes of St. Roque

and St. Augustin. This bifurcation has always, and with good reason, been

ascribed to the protruding convexity of the South American continent at

these two promontories. It would be an important step gained in verifying

the theory of currents, could the precise distance be ascertained by

chronometer. It is apparently like an "_actio in distans_," probably a

phenomenon of what is known as "packing." As the frigate, on leaving Rio

de Janeiro is to make for the Cape of Good Hope, the opportunity will

present, should she steer sufficiently southerly, for many interesting

observations with respect to the _connecting current_ W.N.W. and E.S.E.

which encounters that from Madagascar and Mozambique, close to the Cape,

more especially with regard to the temperature of the sea.

If the frigate is intended to approach the small cluster of islands of

Fernando de Noronha, E. of Pernambuco (Lat. 3° 50' S.), I would recommend

to that excellent geognostic, Dr. Hochstetter, the hornblendic phonolithe

rock found there, far from a volcanic crater, but with trachytic dykes and

basaltic amygdaloid. The flat little island of St. Paul (Peñedo de San

Pedro), 1° N. Lat., singular to say, is not volcanic at all, containing,

like the Malouin or Falkland Islands, slaty green-stone passing into

serpentine.

Should the frigate alter her course and cross the Equator more to the

eastward, without touching at Rio de Janeiro, she might possibly fall in

with the Marine Volcanic region, (Lat. 0° 20' S., Long. 22° W.), which

has quite lately become famous again by the U. S. Expedition of the Brig

_Dolphin_ (1854), commanded by Lieutenant Lee. On 19th May, 1806, columns

of black smoke were seen issuing from the sea by Krusenstern, and volcanic

ashes were gathered, after a singular bubbling of the sea from 1748 to

1836, according to careful investigations by Daussy.

As the frigate is commissioned to visit Ceylon and the Nicobar Islands,

she cannot sail direct from the Cape to Australia; and the hope must

therefore be abandoned of her visiting the small basaltic islands, known

as Prince Edward's (47° 2' S., 38° E.), and Possession (46° 28' S., 47°

30' E.), belonging to the Crozet's Group, or the two islands, long

confounded with each other, of Amsterdam (Lat. 37° 48' S.) and St. Paul

(Lat. 38° 38' S.) The latter island, the more southerly of the two, (a

very characteristic drawing of which was given by Willem de Vlaming so far

back as 1696), is supposed to be volcanic, not only by its form, which

will at once remind the geologist of Santorin, Barren Island, and

Deception Island, (one of the New Shetland group), but also in consequence

of the eruption of steam, and the flames occasionally observed there.

As for Amsterdam, which consists of a single densely-wooded mountain, the

puzzle remains for solution as to how, during the expedition of

D'Entrecasteaux in 1792, the whole island seemed, during two entire days,

enveloped in smoke; whereas, on landing there, the naturalists of that

expedition were satisfied that the mountain was not an active volcano,

and that the columns of steam issued out of the ground near the shore! As

yet, the phenomenon remains entirely unexplained.

If we examine any map of the Indian Ocean, we may trace the continuation

of the Sunda group from Sumatra, N.W., through the Nicobar, and Great and

Little Andaman Islands, and thence through the volcanoes of Barren Island,

Narcondam and Cheduba, nearly parallel with the coasts of Malacca and

Tenasserim, all on the eastern part of the Bay of Bengal. The minor

volcanoes just enumerated will present valuable opportunities of

geological enquiry.

Along the coasts of Orissa and Coromandel, the western portion of the Bay

of Bengal is quite free of islands, Ceylon, like Madagascar presenting

rather the type of a continent.

Off the W. coast of the peninsula of India, (that is opposite the

Neilgherrie hills, and the coast of Canara and Malabar), there is a series

of three archipelagoes, extending from 14° N. to 8° S., viz., the

Laccadives, the Maldives, and the Chagos, which appears, as it were,

continued through the banks of Sahia di Malha, and Cargados Carajos, to

the volcanic group of the Mascarenhas and Madagascar. As the first-named

archipelagoes, so far as is yet known, consist solely of coral, and are,

consequently, true "atolls," or reef-lagoons, the bottom of the ocean

should be examined over a large extent, adopting the ingenious hypothesis

of Darwin, that it is to be considered _as an area of subsidence_, rather

than an elevated region.

It would also be a matter of great importance to get observations

respecting terrestrial magnetism, particularly so as to define the

position of a given segment of the magnetic equator. Capt. Elliott, as the

result of his comprehensive studies, (1846-49), ascertained that the

magnetic equator passes through the north end of Borneo, and thence nearly

due W. to the northern extremity of Ceylon. In this region the curve of

minimum intensity is nearly parallel to the magnetic equator, which

intersects the Continent of Africa near Cape Guardafui--according to

Rochet d'Héricourt, in lat. 10° 7' N., long. 38° 5'. E. Between this point

and the Bight of Biafra nothing is known.

The South Asiatic islands comprise Formosa, the Philippines, the Sunda

group, and the Moluccas. The great and little Sunda Islands and the

Moluccas embrace 109 volcanoes, with fiery eruptions, and 10 what are

called mud-volcanoes. This is not a mere estimate, but is the result of an

enumeration by Junghuhn, who, within the last year (1856), has returned to

Java, and thoroughly equipped by M. Pahud, Governor-General of the Indian

Netherlands, will be of great assistance to the Imperial Expedition.

An exact mineralogical determination of the volcanic rocks (trachytes) is

unfortunately wanting everywhere.

The most active volcano of Sumatra is the Gunung Merapi (8980 feet), which

must not be confounded with a volcano in Java, of the same name. That of

Sumatra was ascended by Dr. L. Horner, and Dr. Korthals in 1834. We may

pronounce Indrapura (11,500 feet, but this measurement is very uncertain),

and Gunung Pasoman (9010 feet), the Ophir of our maps, to be utterly

unknown geologically. The highest of the Java volcanoes is Gunung Semeru

(11,480 feet), ascended by Junghuhn in 1844, 1220 feet higher than the

Etna. The largest craters of the 45 which are disposed in a line along the

shores of Java, are Gunung Tengger, and Gunung Raou. Dr. Junghuhn has

recently given the outlines of each separate volcano in his splendid

topographical and geological map of Java, in four sheets, published in

1856, which does great credit to the Dutch Government.

The following subjects are worthy of special attention while the frigate

is at Java.

1. The curious phenomenon of the ribbed surface. (_Vide_ Junghuhn, Java,

Part II., p. 608.)

2. The disposition, as yet unaccounted for, of a series of

regularly-shaped hills, formed by the mud-streams ejected in the year 1822

by the volcano of Gunung Galungung. (_Vide ut suprà_, pp. 127-731.)

3. The ejection of water by the Gunung Idjen, on 21st January, 1817, (pp.

707, and 717-121).

4. The erroneousness of the assertion that the volcanoes of the Island of

Java do not emit streams of real lava.

It must be admitted that the mighty Javanese volcano, Gunung Merapi,

already alluded to, has not, within the historic period, presented any

coherent compact streams of lava, but mere fragments and boulders;

although in 1837, lines of fire were seen running uninterruptedly from

the top down the sides of the cones in eruption. But each of the three

volcanoes, Tengger, Idjen, and Slamat, present examples of black lava

currents, descending as far as the tertiary strata.

Streams of stone-boulders, red-hot, similar to those of the Cotopaxi, but

scarcely touching each other, flowed from Gunung Lamorgan on 6th July,

1838.

No active volcano is known in the island of Borneo. The highest mountain

of the whole island, perhaps of the whole insular world of Southern Asia,

is the Hina Baïlu (12,850 feet?) on the northern point of Borneo. It is as

yet unexplored. According to Dr. Lewis Horner, son of the astronomer of

the Krusenstern expedition, there occur among the syenite and serpentine

mountain range of Rathus, on the S.E. of the island, deposits yielding

gold (which has even been worked by diggings), diamonds, platinum,

iridium, and osmium,--presenting, in fact, a similar association to those

of the Ural mountains. No mention is made of palladium. Rajah (now Sir

James) Brooke describes in the province of Sarawak in Borneo, a low hill,

Gunung Api ("hill of fire" in Malay), the slags of which attest former

volcanic activity. A visit to Borneo would be of very great service.

There are eleven volcanoes in Celebes, and six in Flores, all active.

It is still uncertain whether the conical mountain Wawari, or Atiti,

which is more generally known as the volcano of the island of Amboyna,

ever poured out anything except hot mud (1674), or whether it should be

merely classed as a _solfatara_. The main group of the South Asiatic

Islands is connected through the Moluccas and the Philippines with the

Papua and Pellew islands, and the Caroline Archipelago of the South Sea.

The most important geological fact to be remarked with reference to the

island of Formosa, abounding in mineral coals, is the break in the line of

direction of the open vents, when, instead of N.E. to S.W., the central

line follows the meridian line, which it pursues nearly as far as 6° S.,

passing through Formosa and the Philippine Islands (Luzon and Mindanao),

respecting which deviation nothing certain is known, and in which region

every mountain of conical shape, or outline is invariably set down as a

volcano, even though there should be no indications of a crater. The

Sooloo Archipelago forms the connecting link between the islands of Borneo

and Mindanao, the long, narrow island of Palawan, constituting that

between Borneo and Mindoro.

The Island of Yesso, separated from that of Niphon by the Straits of

Sangar, or Tsugar, and from the islands of Krafto (Saghalien) and Tschoka,

or Tarakai, by the Straits of La Pérouse, connects, through its North

Eastern Cape, with the archipelago of the Kuriles. From Broughton's

Southern Vulcan Bay up to its northernmost point, Yesso is traversed by an

uninterrupted range of volcanoes--a fact the more worthy of being

recorded, as in the expedition of La Pérouse there were found red porous

lavas, as well as wide areas, covered with slags, in the Baie des

Castries, in the narrow island of Krafto (Saghalien), which is, as it

were, merely a continuation of Yesso. In our own day these regions command

a higher interest, from a political point of view, more especially since

Russia, dissatisfied with the situation of Okhotsk, at the sanded mouth of

the Amoor, was anxious, after the destruction of Petropaulowski, on the

coast of Kamtschatka, to obtain, on the S.E. coast, a harbour suitable

for a military station.

Among the three islands which form the main portion of the Japanese

Empire, six volcanoes are known to have had eruptions in the historic

period. The volcano, Fusi Jama, in Niphon, province of Suruga (Lat. 35°

18' N., Long. 136° 15' E., altitude 11,675 feet), is said to have risen

out of the plain 286 years before the Christian era. Its last eruption was

in 1707. The volcano, Asama Jama, in the district of Saku, between the

meridians of the two capitals, Miaco and Jeddo, was last in eruption in

1783. On the island of Kiusiu, adjoining the peninsula of Corea, four

volcanoes are situated, from one of which, called Wanzen, there was a most

destructive eruption in 1793.

The beautiful work of Commodore Perry, U.S.N., detailing his mission to

Japan, on the part of the United States Government, in 1852, containing

excellent photographs of races, as also drawings by the Berlin artist,

Wilhelm Heine, does not, as yet, comprise the scientific results of that

expedition.

Proceeding northwards, the volcanoes are more densely crowded, and are

found arranged in series. Of the fifty-four which I enumerated as still in

activity among the islands of Eastern Asia, there are thirty-four on the

Aleutian, and ten on the Kurile Islands. The Peninsula of Kamtschatka

contains nine volcanoes, which have been in activity within the historic

period. Lying under the 54th and 60th degrees of northern latitude, we see

a long strip of sea-bottom between two continents undergoing a perpetual

process of destruction and re-arrangement.

The South Sea, the superficial extent of which is one-sixth greater than

that of the entire solid crust of our planet, actually presents a smaller

number of active volcanoes, less vents for communication between the

centre of the earth and its atmospheric envelope, than the single Island

of Java! Out of 40 volcanic cones, including those which are extinct, only

26 have been seen in eruption during the historic period. They are not

scattered at random, but, on the contrary, as was pointed out by Mr. James

Dana, the ingenious geologist of the great United States Exploring

Expedition, under the command of Capt. Wilkes (1838-42), they have been

thrown up, at widely extending clefts, communicating by submarine mountain

systems. They are arranged in groups and distinct regions, analogous to

the mountain chains of Central Asia and Armenia (in the district of the

Caucasus), and belong to two quite distinct systems, one running S.E. to

N.W., the other S.S.W. to N.N.E.

In the Hawaiian Archipelago (or Sandwich Island group), we find Mauna Loa,

according to Wilkes, 12,900 feet in height, which does not present any

cone of volcanic scoriæ (resembling, in this particular, the volcanoes of

the Eifel), but has emitted streams of lava. The lava basin of Killauea,

13,000 feet in its greatest, by 4800 in its smallest diameter, is not a

_solfatara_, but a true lateral vent on the flank of the powerful Mauna

Loa itself, exactly resembling the less elevated sheet of lava of Arak.

Mauna Kea is 180 feet higher than Mauna Loa, but is extinct. Tafoa and

Amangura, in the Tonga group, are still in eruption, the last discharge of

lava having occurred in July, 1847. The volcano of Tanna was in full

eruption during Capt. Cook's Voyage of Discovery in 1774, as was also the

volcano of Ambrym, west of Malicollo in the archipelago of the New

Hebrides. At the south point of New Caledonia, lies Matthew's Rock, a

small smoking rocky island. The volcano of Santa Cruz, N.N.W. of Tina

Kora, with periodical eruptions occasionally occurring at intervals of 10

minutes, had been already noticed as a volcano by Mendana, so far back as

1595. In the Salomon Archipelago, there is found the volcano of Sesarga,

while others are said to be in full activity in the Marianas or Ladrones,

just like those of Guguan, Pagon, and El Volcan Grande de Asuncion, which

appear to have broken forth along a line that follows the meridian. In New

Britannia, three conical mountains were observed vomiting streams of lava,

by Tasman, Carteret, and Labillardière. There are two volcanoes in full

activity on the north-east coast of New Guinea, opposite Admiralty

Islands, which themselves are so rich in obsidian. In New Zealand,

numerous regions abound in basaltic and trachytic rocks. Of active

volcanoes there are Puhia-i-Wakati (the volcano of White Island), and the

lofty cone of Tongariro (5816 feet). To the absence of centres of volcanic

agency in New Caledonia, where sedimentary formations and seams of coal

have recently been discovered, is ascribed the vast development of coral

reefs. Dana was the first to ascend the Peak of Tafua, in the Island of

Upolu, one of the Samoa group, not to be confounded with the still active

volcano of Tafoa, south of Amangura, in the Tonga Archipelago. Dana found

in it a crater overgrown with thick forest. So, too, on the isolated Vaihu

or Easter Island group, there is found a range of conical mountains with

craters, but inactive.

Of the volcanic groups of the South Sea, the most violent is the farthest

east, adjoining the shores of the New World, viz., the archipelago of the

Gallipagos, which consists of five considerable islands, very admirably

described by Darwin. There are streams of lava down to the very shore of

the sea, but no pumice. Some of the trachytic lavas are said to abound

with crystals of albite. It is important to examine whether or not this

is oligoclase, as on Teneriffe, Popocatepetl, and Chimborazo; or

labradorite, as on Etna and Stromboli. Palagonite, exactly similar to that

of Iceland or in Italy, was discovered by Bunsen in the specimens of tufa

from Chatham Island, one of the Gallipagos.

New Holland does not show any signs of recent volcanic activity, except at

its most southern point (Australia Felix), at the foot of the Grampian

Mountains. N.W. from Port Philip, as also towards the Murray River, there

are numbers of volcanic cones and sheets or flows of lava.

It would be of great interest and utility to observe the relative

inclinations of the Magnetic and the Geographical Equators, by means of

the dip of the magnetic needle, though this will be rendered more

difficult, from the fact of the ship's course being easterly, that is,

contrary, to the Equinoctial current. As regards the low temperature of

the current, which I discovered in 1802, running up from 40° S. to the

Gallipagos along the coast of South America, and then turning westward, it

would be highly important to investigate whether in the eastern part of

the South Sea in 7° N. and between 117° and 140° W., there really exists

in every season a _counter current_ from west to east. But I need not

enlarge upon this topic to such attentive navigators.

The line of no inclination was crossed six times by Duperrey between 1822

and 1825. When I first discovered, near Truxillo, the low temperature of

the cold Peruvian current, it was 12°·8 Réaumur (60°·8 Fahr.). The

temperature observed in the course of twenty years by Mr. Dirckinck von

Holmfeld, in the neighbourhood of Callao, expressed in degrees of Réaumur,

were as follows:--

September 1802 12°·8 (Fahr. 60°·8) } Thermometer in the air.

November " 12°·4 ( " 59°·9) } 13°·3 Réaumur.

December, end of 16°·8 ( " 69°·8) } (61°·92 Fahr.)

January 1825 12°·7 ( " 60°·57)

February " 15°·3 ( " 66°·42)

March " 15°·7 ( " 67°·32)

April " 14°·5 ( " 64°·62)

The temperature of the sea I found to be 22° Réaumur (81°·5 Fah.) north of

Cape Blanco, when on my way from Callao de Lima, at which point the cold

current diverged towards the Gallipagos.

Between the Gulfs of Guayaquil and Panama, north-east of the cold current,

the temperature of the sea during the month of April rose as high as

24°·5, (87°·12 Fahr.). Within the range of the current, Mr. Dirckinck had

carried on his observations in compliance with my instructions, by means

of thermometers that had been compared by Arago. Everywhere in the

current, in December 1824, he found from 16° to 18° (68° to 72°·5 Fahr.);

between Quilca and Callao, in January, 1825, from 18° to 19° (72°·5 to

74°·75 Fahr.); between Chorillos, near Lima (Lat. 12° 39' S.) and

Valparaiso, in August, 1825, from 13°·8 to 10°·5 (63°·05 to 55°·62 Fahr.);

between Chorillos and San Carlos de Chiloe, in June, 1825, from 18°·8 to

9°·2 (74°·3 to 52°·7).

In sailing from the Sandwich Islands to the west coast of America, the

Imperial Expedition will have to choose between the Ports of San Francisco

or Acapulco. The first choice would be of great mineralogical advantage

for those regions of the United States, lying North of the river Gila.[3]

Parallel with the chain of the Rocky Mountains, which, according to

Marcou, contains up to the present day several volcanoes in full activity

in its northern part (Lat. 46° 12' N.), run single, and at certain points

double ranges of coast chains from San Diego to Monterey, from 32° 15' N.

to 46° 45' N. They begin with the coast range specially so-called, which

is a continuation of the high ridge of the Peninsula of Lower or Old

California; after which, farther to the North, there follow in succession,

first the Sierra Nevada di Alta California, between 36° and 38° N. the

lofty Shasty mountains, and the Cascade Range, nearly twenty six miles

distant from the littoral, including many high and active volcanoes, and

extending far beyond Fuca Straits. The following are still in

eruption:--Mount St. Elias (46° 2' N.); Mount Regnier, or Rainier, (46°

46'); and Mount Baker, (48° 48'.) These three active cones would be most

conveniently visited by the geologist of the expedition from San

Francisco, as would likewise the whole Cascade Range. We have as yet no

certain intelligence as to the geology of the entire longitudinal

auriferous valley of the Sacramento River, (where a trachytic crater, in

a state of disintegration, is known as the Butt of Sacramento). Does the

auriferous quartz occur in veins, and are these still _in situ_, or are

they broken up? What description of rock is traversed by these veins? Does

the wash-gold here contain occasionally, as in the Ural Mountains,

fragments of vein-stones with isolated cavities, in which are found

impressions of leaves and membranes, clearly proving that they have not

been rolled, or transported by water, any great distance to the spot they

now occupy? Have these been found, alongside of gold, diamonds, platinum,

osmium, iridium, or mercury?

[Footnote 3: The Gila falls into the Colorado about forty miles above the

embouchure of the latter into the head of the Gulf of California.]

Should the frigate steer for Acapulco, it may be assumed that there exists

an intention to cross the Continent to Mexico and Vera Cruz, from the

volcano of Colima (1877 toises) as it were, along the parallel of the

range of volcanoes, and greatest heights rising in detached groups between

the two seas, about the parallel of 19° N. New astronomical observations

are greatly needed for determining the position of the volcanoes of Colima

and Jorullo (667 toises). The volcano of Colima, with its twin peaks _de

fuego_ and _de nieve_, should be carefully examined, as also the volcano

of Jorullo, with the fragments of granite enclosed in its lava; the Nevado

de Toluca (2372 toises), Popocatepetl (2772 toises), Itztaccihuatl (2456

toises), Cofre de Perote (2098 toises), and the volcano of Tuxtla (18° 28'

N.), on the eastern slope of the Sierra St. Martin, from which a column of

flame shot up with great violence on 2nd March, 1793, a fair specimen of

what the Spaniards term _Malpays_, the Sicilians _Sciarra viva_. The face

of the country is covered over with boulders of lava, at San Nicolas de

los Ranchos, at the foot of Popocatepetl, adjoining the city of Puebla de

los Angeles, after which, on the road from Puebla to Vera Cruz, will be

observed two narrow strips of boulders of cooled basaltic lava, rich in

olivine. Similar examples will be found at Parage de Carros, near

Tochtilacuaja and Loma de Tablas, between Cancas and the Casas de la Hoja.

The mere ascension of volcanic cones is geologically of far less

importance, than the bringing away numerous specimens, carefully selected,

of various trachytic rocks, which, by their oryctognostical composition,

are characteristic of each volcano. I would nevertheless recommend that

the Pico del Fraile of the Toluca volcano (2372 toises) should be

ascended, proper caution being used. From this very sharp peak, I brought

away thin plates of trachyte perforated by lightning, and within the holes

of a melted glassy surface, resembling those brought from Little Ararat.

Both for the miner and geologist, an interesting and useful visit might be

paid to the rich mines of Guanaxuato and the Mines de la Biscaina and

Regla, on the road from Mexico to Real del Monte, so as to observe the

close connection subsisting between the richer silver ores, occurring in

trachytic porphyry without quartz, but with felspar, (glassy felspar?),

and the thoroughly volcanic Cerro del Jakal, abounding in obsidian, and

the Cerro de las Navajas (Razor Range), which remind one of the environs

of Schemnitz, with the sole exception, that the trachytes "_porphyres

meulières_" of Beudant, are wanting here.

As it is highly desirable that considerable time should be devoted to the

volcanoes of Quito, Peru, and Chili, it appears uncertain whether the

course of the frigate, on leaving Acalpulco, will be shaped direct for

Guayaquil, thus reversing the route taken by myself, or whether she will

not touch at some of the central American ports--Realejo or Sonsonate. The

crowded series of volcanoes in Central America, of which no less than

eighteen, conical or dome-shaped, may be considered as still in active

eruption, would yield a rich harvest of facts of all kinds in elucidation

of the theory of volcanic action, such as have never hitherto been

sufficiently taken advantage of. We are still in need of the mineralogical

determination of the rocks, while the form and situation of the mountain

masses have been well described by Squier, Oersted, and other modern

travellers. The greater number, indeed, of the eruptions of scoriæ and

slag were unaccompanied by streams of lava, as, for example, those of

Mount Isalco, abounding in ammonia. But recently eye-witnesses have

furnished us with quite different accounts regarding these eruptions, in

the case of several volcanoes--as the Nindiri (a twin volcano with that

called Massaya), on which Dr. Scherzer has lately shed much light; the

Volcano el Nuevo, erroneously called Volcano de las Pilas, that of

Coseguina, situated on the Great Bay of Fonseca, and that of San Miguel de

Bosotlan, from which there flowed an extensive stream of lava in July

1844. It would be most tempting to pass by land from Mexico southwards to

Oaxaca, and thence to the Isthmus of Guasacualco or Tehuantepec, and

Chiapas, so as to rejoin the frigate at Realejo or Sonsonate. Facts might

be obtained, in such a journey, of great value in determining the

dependence of geological phenomena on each other; but it is to be feared

it would be attended with too much fatigue and loss of time. For similar

reasons, it cannot be proposed that the scientific gentlemen attached to

the Expedition, should leave the frigate for three or four months, when

they reach Central America, in order to cross by rail the Isthmus of

Panama, with the object of examining the Volcancitos of Turbaco and Gabra

Zamba, both active, and thence ascend the Rio Magdalena from Carthagena de

las Indias, as far as Honda, whence they could proceed by Bogotà and

Popayan to Quitó.

It will be also unavoidable to forego the examination of the sedimentary

rocks, rich in fossils, between Honda, Bogotà and Ibagues, the Mastodon

fields (_Campos del Gigante_), and the Salto de Tegumidama on the plateau

of Bogotà, the wax palm (_Ceroxylon Andicola_), and the Azufrales of the

Passo de Quindiu, the volcanoes of Tolima, measured by myself and ascended

by Boussingault, and of Paramo de Ruiz (4° 15' N.), as also the two

volcanoes of Popayan, the Puracé and the much more interesting but now

extinct Sotará. As a middle course, I may suggest a disembarkation, not

exactly at Guayaquil, but on the gold and platinum coast of the Choco,

near San Buenaventura, so as to proceed thence to Popayan, and afterwards

return to the volcanoes of the province of Pasto, which are highly

important, and so on to Quitó, by way of Guachucal, Tulcan, and Villa de

Ibarra, rejoining the frigate only at Guayaquil.

I believe, however, it would be more advisable to select Quitó as the

starting-point, whence to examine the important elevated volcanic region

De los Pastos (between 2° 20' and 0° 56' N.), containing the volcano of

the town of Pasto, the volcanoes of Tuguerres, Chiles and Cumbal, and the

Azufral de Pasto, and not to land at any port of the Choco coast, not even

from the Bahia de Cupica, which for half a century I have recommended in

vain on account of its vicinity to the Rio Naipi, one of the tributaries

of the Atrato. In drawing up a list of names of the volcanoes of the

renowned lofty plateau of Quitó, I may include, Imbaburu, Cotocachi, Rucu,

Pichincha, Antisana, the much-disputed question of the stony walls like

streams of lava, on the east slope of Tana Volcan, and Reventazon de

Ansango; Cotopaxi, with its strange inexplicable quarries of pumice, of

Guapecho and Zumbalica, in the neighbourhood of Llactacunga and San

Felipe, the pumice containing oligoclase, not glassy felspar, deposited in

strata, like any rock _in situ_ for a considerable distance on all sides

of Cotopaxi; Tunguragua (mica slate), studded with garnets, and beds of

granite, which dip under the former, and have themselves been pierced by

the trachytes of Tungurahua at Rio Puela and the Hacienda de Ganace; the

hills of Moya, near the village of Pelilco, cast up in the celebrated

earthquake of 7th February, 1797, and still in a state of activity; the

Chimborazo, which M. Jules Rémy, accompanied by an Englishman named

Princkley, was in the belief they had ascended, on the 3rd of November,

1856, to the very summit, "_mais sans s'en douter_." Poggendorff, (Vol. X.

p. 480), has clearly demonstrated that the boiling point given by Rémy for

the summit, would not give 6544 mètres (little different from my own

trigonometrical admeasurement of 6530 mètres), but fully 7328 mètres. As I

distrust my own half-barometical measurements, I have vainly implored

travellers, these fifty years past, to have a new series of

trigonometrical observations made of the summit of Chimborazo. The merit,

then, of settling this moot point, it also remains for the members of the

_Novara_ Expedition to obtain.

It would be important to examine the Sangay (16,068 feet)--which, like

Stromboli, is in constant activity, yet without any traces of

lava-streams--on account of the grains of quartz discovered by Wisse in

the trachytic boulders ejected by the volcano, which is of such rare

occurrence in the trachytes out of Hungary; and also on account of the

close vicinity of beds of granite and gneiss, which are broken through by

the Sangay trachyte, forming an island, as it were, of not hardly two

miles in breadth. Still more deserving of attention is the extinct volcano

El Altar de los Collanes (Capac Urcù) a sketch of which I presented in

the atlas published in my "Kleine Schriften" (Plate V. p. 461), formerly

higher than Chimborazo, and still (?) 16,380 feet. Not a single specimen

of its trachyte has ever been deposited in a European museum. The Altar

itself is readily accessible from Riobamba Nuevo. In its vicinity may also

be seen mica slate and gneiss, cropping out at the Paramo del Hatillo near

Guamote, and Teocaxas, which are so seldom fallen in with in the highlands

of Quitó. Tradition relates that gold-mines were worked here during the

days of the Incas, in the neighbourhood of volcanic trachytes. From the

Altar the geologist might proceed, by way of San Luis, (Query, whether the

primitive clay-slate found here be of the Silurian formation?) and

Guamote, to Paramo del Assuay (2428 toises), and Cuenca, as far as Atausca

(2° 13' S.), where an immense mass of sulphur, lying in a quartz seam is

worked, forming a bed in the mica slate. Of what rock does the easily

accessible Cayambe Urcù (18,170 feet) consist, crossing the Equator, S.E.

of Otavalo? _En route_ from Quitó to Cayambe, the rich deposits of

obsidian near Quinche should also be inspected, which furnished the large

mirrors to the Incas, and farther to the north of which are the volcanoes

of Los Pastos, which form a separate system by themselves.

For examining the rocks and exploring the volcanoes of Southern Peru and

Bolivia--respecting which see the last edition of Pentland's Maps, not

those published between 1830 and 1848, in which the height of Sorata was

indicated at 3949 toises (25,257 feet), and Illimani at 3753 toises

(24,004), and accordingly both as much more lofty than Chimborazo, which

is 3350 toises (21,426 feet)--the best starting-point would be the port of

Arica, which may be reached, sailing the whole distance against the cold

current, from Guayaquil, after a short stay at Callao de Lima. Of the

volcanoes of Peru and Bolivia only three are now active.

(_a._) The volcano of Arequipa, three miles N.E. of the town of the same

name, which, according to Pentland and Rivero, is situated about 7366 feet

above the level of the sea. The measurements of M. Dolley, of the French

navy, which were published under my superintendence, give the summit of

the volcano as 10,348 feet above the town of Arequipa, so that its total

elevation above the sea would be 17,714 feet. In the table of heights for

Mrs. Somerville's "Physical Geography," Mr. Pentland speaks of the summit

as being 20,320 English feet in height, or 19,065 Paris feet, closely

approximating to the old trigonometrical measurement (19,080 feet) given

by Thaddeus Haenke, a Bohemian, who accompanied the expedition of

Malaspina, in 1769. What a deplorable state for the science of hypsometry

to be in! which the _Novara_ ought to put an end to. Samuel Anzon, a North

American, in 1811, and Dr. Weddell, in 1847, have ascended the volcano of

Arequipa.

(_b._) Sahama (18° 7' S.), according to Pentland's new map of 1848, is 871

feet higher than Chimborazo (which he gives as 20,970 feet), and is still

active. The true heights of Illimani and Sorata, ascertained since 1848,

are, instead of 3949 and 3753 respectively, only 3329 toises (21,266

English feet), and 3307 toises (21,145 English feet).

(_c._) Volcano Gualatieri, in the Bolivian province of Carangas (18° 25'

S.), height 20,604 feet.

The southern group of South American volcanoes, that, of Chili, presents

the largest number of active fire-mountains--only second, indeed, to that

of Central America, there being from eleven to thirteen. In order to

increase the geological exploration of this region which has been so well

prepared by the memorable expedition under Captain Fitzroy, in the ships

_Adventure_ and _Beagle_, the excellent generalizing theories of Mr.

Darwin, and the naval astronomical expedition of Mr. Gilliss, for 1849-51,

the _Novara_ will probably land at Valparaiso. A great desideratum between

Coquimbo and Valparaiso is an exact measurement of--

_A_. The volcano of Aconcagua (32° 39' S.). Its height has been stated, in

1835, by Captain Fitzroy, as 21,767 feet, Pentland's correction assigning

22,431 feet; while Captain Kellet, of the frigate _Herald_, gives it as

21,584 feet. Miers and Darwin are both of opinion that the Aconcagua is

still in activity, which is denied by Pentland and Gilliss. The most

recent measurement of Aconcagua--that by Pissis in 1854 (see Gilliss, Vol.

I. p. 63)--makes the height 20,924 feet. M. Pissis has published, in the

"Anales de la Universidad de Chili," for 1852, the geodetical elements of

his survey, which is based upon eight triangles. Aconcagua being probably

the highest mountain in the New World, a new measurement is eminently

desirable. Neither Dhawalagiri, with his 4930 toises, nor Kintsinjunga,

measured by Colonel Waugh, with his 4406 toises, are any longer considered

the highest mountains in the Himalaya range, but the Deodunga (Mount

Everest), which is 29,003 English feet, equal to 27,212 Paris feet, or

4535 toises.

_B._ The volcano Maipu (34° 17' S., height 16,572 feet), ascended by

Meyen. The trachytic rock on the summit has broken through the Jurassic

strata, in which Leopold von Buch has ascertained, from heights of 9000

feet, the existence of _Exogyra couloni_, _Trigonia costata_, and

_Ammonites biplex_. This volcano has no streams of lava, but only

eruptions of volcanic slags. It would be most desirable that Dr.

Hochstetter should examine this remarkable protrusion of dislocated

strata.

_C._ The volcano Antuco (37° 7' S.), the geology of which was described by

Pöppig, is a lofty basaltic crater, having a trachytic cone rising up in

its centre to an elevation of 8672 feet. It was observed in full activity

by Domeyko in 1845. Gilliss gives an account of an eruption in 1853.

According to Domeyko, a fresh-burning cone was thrown up on the 25th of

November, 1847, which remained in activity for a whole year. Molina

considers the Nevada Descabezado (35° 1' S.), ascended by Domeyko, to be

the highest mountain in Chili; but its height is estimated by Gilliss at

only 12,300 feet. The most southerly volcanoes are the still active

Corcovado (43° 12' S.), 7046 feet; Yanteles (43° 29' S.), 7534 feet; and

the Volcan de San Clemente, opposite the granite formation on the

peninsula of Tres Montes. Still further south, in 51° 41' S., another, the

Volcan de los Gigantes, is laid down on the old maps of South America, by

La Cruz Olmedella, as opposite the archipelago of La Madre de Dios.

Should the _Novara_ return to Europe through the Straits of Maghellanes,

it would be very desirable the members of the Expedition should visit the

locality from which Prince Paul of Würtemberg, after long zoological

travels through North America, has, within the last year, brought back to

Germany a very large collection of specimens.

Altogether, I calculate the number of active volcanoes on the surface of

the earth to be upwards of 225--one-third of which, or 75, are upon the

various continents, and the remainder upon the insular world. The Western

Continent has 53 active volcanoes--of which, North-Western America, north

of the river Gila, has 5; Mexico, 4; Central America, 18; South America

about 26. Viewing the globe as a whole, there presents itself an extensive

oblique region in which volcanoes most abound, stretching from S.E. to

N.W. in the more westerly part of the Pacific, between 75° W. and 125° E.

of Paris, and between 47° S. and 66° N. In this region, the fused elements

of the interior of our earth may be said to be most permanently in

communication with the atmosphere.

The greatest attention should be paid, with the view of improving them,

to the sections and maps of Chili, contained in the work, "Buenos Ayres

and the Provinces of Rio de la Plata," published in 1852 by Sir Woodbine

Parish, and still more so, to that entitled "Map of the Republic of Chili,

compiled from the Surveys of Gilliss, Pissis, Allen, Campbell, and Claude

Gay, between 23° and 44° S., as contained in Gilliss' 'United States

Astronomical Expedition, 1847-52 Washington, 1855.'"

The chief object to be aimed at by the _Novara_, with respect to

scientific enquiry, seems to me to be the formation of a collection in the

Geological Institute of Vienna, in comparison to which all the collections

which at present aspire to be considered rich in volcanic specimens, (such

as those of Berlin, Paris and London), should appear to be insignificant.

In all periods of history, travellers are only the representatives of the

state of knowledge of their own time, and consequently, collections always

present the readiest means of promulgating new discoveries by

oryctognostical examination or chemical analysis. In order to set on foot

a grand Volcanic Museum, it would be necessary to bring home from every

one of the volcanoes visited, not less than 10 or 12, but still better 15

or 18, specimens of the porphyritic trachytes, all carefully selected,

well-shaped, containing crystals not disintegrated, and of sufficient size

to admit of a fresh fracture being made. For such quantities, however,

there cannot be provided on board ship, even with the kindest patronage of

the commanding officer, sufficient space for the accumulations of two

years' arduous efforts in forming a collection. The greatest part,

therefore, should be sent by other conveyance to Trieste, the most secure

channel being through the consuls of the Austrian Empire, or those of

allied powers, or through the medium of British, Dutch or American

mercantile establishments, or by the regular packets.

Duplicates, say four or five specimens, from each volcano, should be taken

on board the _Novara_ in boxes of about 3 feet long. It would be too

disheartening to have any misgivings of the success of this glorious

scheme for getting together a Museum of Volcanic Rocks in Vienna, of all

the regions of the globe, arranged upon a regular geographical system,

each labelled with its own name, so as to promote a general acquaintance

with these branches of knowledge:

1. Europe.

2. Atlantic Islands.

3. Continent of Asia, South Coast of Arabia (Aden), Kamtschatka.

4. Islands of Eastern Asia and India.

5. The Indian Ocean.

6. The Pacific.

7. Continent of South America: Chili, Peru, Bolivia, Quitó and

New Grenada.

8. Central America.

9. Mexico, south of the river Gila.

10. North-Western America, north of the river Gila.

11. West Indies.

Much of this work might be done on board the _Novara_. As to Nos. 3 and 4,

Kamtschatka, the Kurile and Aleutian Islands, the Red Sea, and the West

Indies, it will not be difficult to procure specimens at some future

period.

Our piping times of peace are favourable to the execution of this project,

which should be zealously kept in view throughout the Expedition.

Travelling as I was, during the great wars, I did not dare shrink from the

difficulty of having to carry along with me 44 large boxes, as I did on

the road through Mexico from Acapulco to Vera Cruz, whence they were sent

to Cuba, Philadelphia, and so to Bordeaux. The mechanical labour of having

the collections carefully packed, keeping duplicates distinct, and sending

away geological, botanical, zoological and ethnographical collections, is

itself quite as important as the purely scientific work.

The exhibition of comprehensive volcanic collections brings to light the

strong analogy subsisting between the trachytes belonging to volcanoes,

far distant from one another, while it indicates the existence of great

differences in the mineralogical composition of volcanoes situated very

near each other. My most excellent friend and fellow-traveller in Siberia,

Professor Gustavus Rose, recently subjected the trachytes of the Berlin

Museum, the greater number of which were collected by myself, to careful

crystallographical and chemical investigation. He found oligoclase and

pyroxene on the trachytes of Chimborazo, Popocatepetl, Colima,

Tunguragua, Puracé, Paramo de Ruiz, and the Peak of Teneriffe, which has

recently been accurately examined by Mr. Charles Deville. The trachytes of

Toluca, Orizaba, Gunung Barang, and Burung Agung, on the Island of Java,

Argæus, in Asia Minor, Cuneguilla, south of Sta. Fé de Nuevo-Mexico, the

Sièrra de San Francisco, west of the Rocky Mountains and Pueblo Zuni,

consist of hornblende, oligoclase, and brown mica. The trachytes of

Stromboli and Etna, those of the Siebengebirge (Drachenfels), and of Kara

Hissar in Phrygia, consist of large crystals of glassy felspar, with

numerous smaller crystals of oligoclase, some hornblende and mica.

Oligoclase, having been mistaken for albite, led to the fantastic idea of

a peculiar rock, the _Andesite_, prevailing in the Andes, and even led our

great master, Leopold von Buch, to make some curious distinctions,

(Déscription des Iles Canaries, 1836, pp. 186-87.)

To ascertain the average height above the level of the sea, I propose that

furrows should be cut in the rocks of the different regions along with

inscriptions, which might carry information to unborn ages, as has been

done, on my suggestion, now some 25 years ago, by the Academy of Science

at St. Petersburg, on the Caspian Sea, while Sir James Ross, in his

"Voyage of Discovery in the Southern and Antarctic Regions," 1839-43, Vol.

II. p. 23, regrets not having done so, or, at least, of having only once

adopted this plan.

I would also, with all deference, suggest observations regarding the daily

atmospheric variations or tides, so as to obtain tables of _maxima_ and

_minima_. In order to obtain these, whenever the frigate is at anchor near

any coast, but particularly within the tropics, hourly observations with

the barometer and thermometer (the latter affixed to the barometer, and

also freely suspended in the open air), should be made through several

consecutive days and nights. During the occurrence of an Aurora Borealis

(or Australis), attention should be paid to the perturbations of the

magnetic variation, and the magnetic intensity of the horizontal needle.

Boreal Auroras have been seen in the southern latitudes of the Peruvian

Pacific, as low down as 12° 13' S.; but the occurrence of such phenomena

there is of much less frequent occurrence than that of Austral Auroras in

Scotland. It is important to keep an exact register of the intensity of

blackness in the "coalbags," when the smallest stars surrounding them are

still visible to the naked eye. The daily meteorological observations, as

also those on the temperature of the sea, will probably be made on board

ship, in conformity with the views of Lieutenant Maury, and the method

agreed upon at the last nautical congress.

* * * * *

As I shall have long ceased to be numbered with the living, when the

_Novara_ returns to Trieste, richly freighted with scientific treasures of

all kinds, with fresh information relating to organic and inorganic

nature, to the races of man, their habits and languages, I now pray to

Almighty God that His blessing may rest upon this great and noble

enterprise, to the honour of our common German Fatherland! And

concluding, in this night, these oblique, illegible lines, I remember, not

without emotion, and with very mingled feelings, that joyous period of my

life when, fifty-eight years ago, in the beautiful gardens of Schönbrunn,

preparing myself for a long journey, I was enjoying with grateful mind the

friendly kindness of the venerable Jacquin and Peter Frank.

A. v. HUMBOLDT.

Berlin, in the night of 7th April, 1857.

[Illustration: DEPARTURE.]

I.

Preparations for the Voyage.

Approbation of the Plan to fit out an Austrian Man-of-War for a

Voyage round the World.--Object of the Expedition.--

Appointment of a Scientific Commission.--Preparations.--

Fitting out the Frigate _Novara_ at Pola.--Departure for

Trieste.--Visit of the Archduke Ferdinand Maximilian on board.

In the autumn of 1856, His Majesty the Emperor was graciously pleased to

approve of the proposal for a voyage round the world, as projected by his

Imperial Highness the Archduke Ferdinand Maximilian, the head of the

Austrian navy, and to commission the sailing frigate _Novara_ for that

purpose, a vessel qualified to meet every requisite condition.

The chief object of the Expedition--a circumstance which must not be lost

sight of--was to afford the officers and cadets of the ship an opportunity

of acquiring that practical acquaintance with naval affairs which, added

to the theoretical knowledge previously attained, would render them

thoroughly familiar with nautical routine, and thus materially contribute

to the further development of the Austrian navy.

This branch of the public service, placed since 1848 on an entirely new

basis, has with difficulty worked its way through all those embarrassing

circumstances inseparable from the organization of a new system; but the

honest zeal and energy of the board appointed, supported by favour from

the highest quarters, have succeeded in introducing many improvements, and

in increasing by degrees the numerical strength of the men, thereby laying

a secure foundation for the rising naval force, the importance of which,

at this moment, every reflecting patriot will acknowledge.

The intended Expedition offered, besides the advantages for the service,

another not less important for the State, namely, the recognition of the

Austrian flag in remote quarters of the globe, to which it had never

hitherto penetrated; and by thus opening new channels for the outlet of

our natural products and manufactured goods, to promote the industrial,

commercial, and maritime interests of the empire.

In order to satisfy the scientific requirements of the age, the

illustrious head of the navy issued orders, that the officers on board

should in every way assist in the researches to be made, connected with

navigation and geography; and was, moreover, pleased to invite the

Imperial Academy of Sciences to nominate two members, he himself naming a

third, to accompany the Expedition for the purpose of observing and

investigating phenomena pertaining to the different branches of physical

science, as well as collecting rare specimens and interesting objects of

natural history. To this commission were ultimately attached a botanist, a

practical zoologist, an artist, and a flower-gardener.

The Academy had, for the guidance of these gentlemen, drawn up

instructions which, with a multitude of other papers containing useful

hints and interesting queries, received from the Imp. Geographical,

Geological, and Medical Societies, as well as from numerous foreign and

native scientific men, formed a most valuable collection of materials for

the purposes of the Expedition.[4]

[Footnote 4: Of these instructions, "The physical and geognostical

remarks," with which the Nestor of natural science honoured the voyagers

of the _Novara_, being of a more general interest, are published at the

end of this volume, together with the facsimile of an autograph letter of

Baron von Humboldt to the commander of the Expedition.]

Foremost amongst these _savans_ stood Alexander von Humboldt, that

illustrious man, who up to the last moment of his existence was alive with

youthful enthusiasm for every scientific enterprise. In England great

interest in the success of the Expedition was evinced by Sir Roderic

Murchison, Sir W. Hooker, Sir Charles Lyell, General Sabine, Admiral

Smyth, Admiral Fitzroy, Professor Robert Owen, Professor Philips,

Professor Bell, Professor W. A. Ramsay, Professor Goodsir, of Edinburgh,

W. J. Hamilton, Esq., Charles Darwin, Esq., L. Horner, Esq., James Yates,

Esq., B. Davis, Esq., &c., &c. From the United States of North America, we

received most valuable communications from Commander M. F. Maury, National

Observatory, Washington, D. C.--Captain Rodgers, and others.

Letters of introduction were received from Germany, and particularly from

England, to influential parties and societies in a variety of places

abroad, amongst which were many warm and friendly recommendations from the

English Government and Admiralty, as well as the Directors of the then

East India Company, to various administrative authorities in the British

Colonies.

[Illustration: GUN-ROOM OF THE _NOVARA_.]

The frigate _Novara_ was laid up in the arsenal of Pola, where all

requisite steps were taken to complete her outfit, and prepare her

thoroughly for the voyage. The ventilation of the lower deck was improved,

and the number of cabins increased in proportion to the number of

individuals for whom accommodation was to be provided.

The gun-room was, by command of the Archduke, converted into a

reading-room, and provided with a well-selected library as well as with

all the charts and maps necessary for the information of the officers, who

here made their calculations and executed their drawings.

The store-rooms for the sails and tackle were enlarged, so as to hold a

double quantity.

A distilling apparatus, the same as patented by M. Rocher, of Nantes, was

fixed on the gun-deck, and being placed in connection with the ship's

coppers, it was found that, during the few hours each day that the latter

were used for cooking, enough sea-water was distilled to supply the entire

ship's company with excellent water to drink. This distilled water, after

having been kept in iron tanks for a month, was found pleasant to the

taste, and agreed very well with the health. The excellent health enjoyed

by all the crew throughout the voyage must, in a great measure, be

ascribed to the circumstance, that scarcely any other but this distilled

sea-water was used, so that the men were enabled entirely to forego

drinking river or spring-water, which in the tropics are frequently found

injurious.

The use of such an apparatus permits a great diminution in the store of

water usually carried by a vessel. The space gained by this diminished

bulk of water, enabled us to take on board a larger cargo of coal and

provisions, such as preserved beef and compressed vegetables. The sailors

were not, however, particularly fond of the preserved beef, because in

cooking it loses a great part of its flavour (though the broth is strong

and good); nor does it seem as an article of diet to have had a

particularly beneficial influence on the health, for the sanitary

condition of the crew was equally satisfactory, and the number of

scorbutic patients not materially increased when, towards the end of the

voyage, the fresh stores were exhausted, and only salt and pickled rations

were issued.

Compressed dried vegetables were of great benefit to the health of our

men, and cannot be sufficiently recommended. The so-called _melange

d'équipage_ of Chollet, as well as _sauer kraut_, potatoes, and other

vegetables, have an excellent taste, improve the soups when mixed with

them, and are easily preserved, provided they be protected from the effect

of damp. Hence it might be advisable to keep them enclosed in

well-soldered tin boxes. The price of these vegetables is so moderate,

that it is surprising they are not more generally employed.

The long-continued satisfactory state of health of the crew must also

partly be sought for in the constant use of shower-baths. For this

purpose, apertures, three-quarters of an inch in diameter, were bored in

the planks of both the deck and forecastle, under which a perforated disc

could be screwed, and above which a pail of water was placed. By these

simple means every one was enabled to enjoy the luxury of a bath; when,

however, the desire for that refreshment became general, so that the

arrangement above-mentioned was insufficient, a hand fire-engine was made

use of, so as to accommodate as many at once as might present

themselves--a process which found great favour with the jolly tars, as

affording abundant opportunities for fun and merriment.

[Illustration: VERTICAL SECTION OF THE FRIGATE "NOVARA."]

The frigate _Novara_ had been placed on the stocks in the arsenal of

Venice in the month of February, 1845, and was launched in April, 1850.

She was pierced for 42 guns, but during the voyage carried only thirty

30-pounders,[5] and four of smaller calibre.

[Footnote 5: The 30-pounder marine guns answer very nearly to the English

32-pounders.]

The principal dimensions of the frigate (Vienna measurement) are:--

Length between perpendiculars 165 feet 5-1/2 inches.[6]

Length of water line 156 " 5 "

Greatest breadth 44 " 11-1/2 "

Greatest breadth on water line 43 " 2 "

Depth of hold 19 " 3/4 "

Draught of water aft 18 " 9 "

Draught of water fore 17 " 5-2/3 "

[Footnote 6: 96-423/1000 Austrian feet = 100 English.]

The superficial area of the ship, or the load-water line, amounted to

5685.35 square feet; quantity of water displaced 2107 Austrian, or 2630

English tons. The superficial area of the principal sails amounted to

18,291 square feet.

The frigate proved herself to be an excellent sailer, as, of the various

vessels which, throughout the voyage, sailed in company with us, only

three clippers outstripped her.

The question may here be asked, why, in the present state of navigation, a

sailing-vessel was preferred to a steamer for this voyage? The principal

consideration which decided this selection was the greater disposable area

which a sailing-vessel offers in comparison with a steamer of the same

dimensions, in which coal and machinery occupy so large a space. On the

present occasion, it will be perceived that what was specially wanted was

room for as great a number of officers, cadets, and men as possible, who

were, as has been stated, to make this voyage for improvement in nautical

affairs. Plenty of space was also required for the numerous instruments

and bulky collections of objects of natural history; while in most parts

of the ocean which we were to traverse, the winds blow so regularly, that,

with very rare exceptions, sails form the best motive power. The expense

of fuel requisite for a steamer, and the trouble of replacing it during

the voyage, are thus saved; whilst, finally, the space occupied by the men

employed in the management of the machinery, and that required for the

stowage of special stores, would be withdrawn from more important objects.

After the frigate had been properly fitted up in the arsenal of Pola, she

sailed on the 15th March, 1857, for Trieste, where she cast anchor on the

17th in the Bay of Muggia. H.I.M.'s corvette _Caroline_, likewise fitted

out at Pola for a voyage to the coast of South America and Western

Africa, followed in her wake, and it was now seen that the frigate was a

better sailer than the corvette, a circumstance so much the more

satisfactory, that the latter had hitherto been considered the swiftest

ship in our navy.

The unfavourable state of the weather interfered so much with the works

which were to be finished at Trieste, that the embarkation of provisions,

swinging the compasses, &c., &c., could only be proceeded with very

slowly.

At last, the members of the Commission arrived, and the vessel only waited

for sailing orders.

Before leaving on so interesting an enterprise, with which the most

pleasing recollections of our lives will ever be associated, we had the

gratification of being honoured by a visit on board from the Archduke

Ferdinand Maximilian. The commander of the Expedition introduced the

officers and scientific gentlemen to his Imperial Highness, who addressed

them in affecting terms, and concluded his remarks by expressing a hope

that the frigate _Novara_ would, with God's help, return happily from her

mission to her own honour and that of the country.

The narrative of the voyage is now presented, and, probably, the results

of the various scientific investigations will very shortly be offered to a

discerning public, leaving it to them to judge how far we have succeeded

in realizing the hopes of the illustrious Prince. But if we have not

satisfied all the expectations entertained, it certainly was not from

insufficiency of means; for everything was complete in that respect, and

we owe it chiefly to the circumspection and kind care of the

Commander-in-chief of our navy, that this enterprise had been so wisely

planned, and its details brought in so short a time to such a degree of

perfection that, during the whole voyage, it was not found necessary to

make the slightest alteration in the original arrangements and

regulations.

[Illustration: GEODETICAL AND ASTRONOMICAL INSTRUMENTS.]

[Illustration: LOOK-OUT MAN.]

II.

From Trieste to Gibraltar.

Departure.--Fair Voyage down the Adriatic.--A Man lost and found

again.--Passage through the Straits of Messina.--The Steamer

_Sta. Lucia_ returns to Trieste.--Regulations and Instructions

for further Proceedings.--A Day on Board the _Novara_.--

Sunrise.--Cleaning the Ship.--Mental and physical occupation.--

Moonlight at sea.

The departure of the frigate was fixed for the 30th April, 1857, and

H.I.M.'s corvette _Caroline_, Captain Kohen, was ordered to accompany her

as far as the coast of South America. H.I.M's steamer, _Sta. Lucia_,

Captain von Littrow, received orders to tow both ships as far as the

extremity of the Straits of Messina to avoid loss of time, such as

frequently arises in the Adriatic during the spring, from calms and

unfavourable winds.

With the dawn of the day fixed for the departure of the ships, all was

bustle on board; craft of all kinds hovered around, and relatives and

friends had assembled in great numbers to take leave. The verdant and

thickly-wooded slopes of the promenade to St. Andrea, near the shore, were

thronged with spectators, and the fair and lovely picture of our native

coast developed itself once more before our eyes, clad in all its charms

of spring, as if to wish us a hearty farewell, an auspicious voyage, and a

happy return!

At 8 o'clock A.M. we weighed anchor, and the steamer _Sta. Lucia_

approached the _Novara_ for the purpose of towing her from the Bay of

Muggia into the roads of Trieste. She had all her colours displayed, and

saluted the city of Trieste, Austria's chief and most important emporium,

with 21 guns. The salute was answered from the castle, whilst the band on

board struck up Haydn's beautiful hymn: "God preserve the Emperor!" The

frigate moved out of the road-stead, accompanied by a great number of

boats, and followed by the best wishes of the numerous crowds assembled on

shore, and of all true patriots, who looked upon this Expedition as a

cheering evidence that a new and energetic spirit of enterprise had arisen

in their native country.

[Illustration: PLATE I.--TRACK FROM TRIESTE TO MADEIRA.]

The corvette _Caroline_, which was waiting outside the roads, was attached

to the frigate, and soon Trieste appeared like a dim cloud on the distant

horizon. The outlines of the Carinthian Alps became fainter, and the

excitement of the parting scene was calmed by that busy activity required

from every one embarking on a long voyage, if he desires to attain any

degree of comfort, however little, in the cramped and limited space of a

crowded ship.

A perfect calm, a smooth sea, and a but-slightly-clouded sky,

prognosticated fair weather, and promised leisure to complete those

arrangements which had been left undone. The steamer _Sta. Lucia_

performed her task of towing the two vessels most satisfactorily, and,

favoured by the prevailing currents of wind and water, we made five miles

an hour, and came, on the day of departure, in sight of the promontory of

Pola.

The passage down the Adriatic was on the whole most pleasant, with the

exception of some showers of rain near the heights of Isola Grossa; which,

however, on this occasion saluted us only with a slight puff of wind. The

ship moved so gently and quietly on her way, that those occupying the

lower cabins could scarcely have fancied themselves at sea, had they not

been made aware of it by other impressions.

On the 1st of May, the crew became highly excited by a man being missed,

when the morning watch was called. Some thought he had, from fear of a

slight punishment hanging over him, jumped overboard, but as nothing of

the kind had been observed by the watch on deck, every corner was

searched, but without success, upon which the man was given over as lost.

When, however, the dinner hour arrived, and the tables and benches were

being removed from the lower deck, how great was the surprise, when the

culprit was discovered crouching among them! A peal of laughter roused the

poor fellow, who this time was let off with the fright and the punishment

of being made an object of ridicule by his comrades.

On the 3rd of May, being clear of the Adriatic, the steamer _Sta. Lucia_

was at midnight despatched to Corfu to complete her store of coal, whilst

we sailed for Cape Spartivento, on the Calabrian coast, which had been

assigned as our _rendezvous_. On the 5th, we sighted this the most

southerly promontory of Italy, when, in consequence of a fresh breeze, the

sea began to make itself rather disagreeably felt. The novices on board

became somewhat alarmed. A feeble voice was even heard, which endeavoured

to prove from this phenomenon that man is a creature made for _terra

firma_, and not for the watery element; but this excellent idea came

rather late; mankind are obliged to submit to existing circumstances, and

this thought alone held out some hope, that a longer stay on board would

prove the best cure for the evil. Such indeed was the case; though pale

faces, want of appetite, and even worse effects, were produced, whenever

the ship made a heavier roll than usual. But these slight inconveniences

of sea life became rarer and rarer, till at last they appeared only in

really stiff gales. On the 7th the steamer _Sta. Lucia_ returned and took

us again in tow.

The weather during our passage through the charming straits of Messina

was delightful. The colossal Etna exhibited in all its glory its

snow-capped summit, gilded by the rays of the rising sun, and Messina

shone with all the attractions of its splendid situation. The coast of

this part of Italy is mostly bare and rugged, the broken outlines of the

mountains imparting to the landscape that characteristic peculiarity which

makes so deep an impression on the mind. We passed the famous Charybdis,

in which a multitude of dolphins were disporting themselves. The

neighbouring coast formed a brilliant panorama, and we kept so close in

shore as to be able to distinguish the movements of the people. The

appearance of our three goodly ships seemed to have attracted the

attention of the inhabitants, for they stood in groups in the streets and

squares of Reggio and Villa San Giovanni, saluting us by waving their

handkerchiefs. When towards the evening we had passed the straits, we

could descry the Neapolitan coast as far as Monte Bulgario, in the Bay of

Policastro, and distinguish the imposing Stromboli, with its volume of

smoke, far on the Western horizon.

The following morning found us in sight of the small island of Alicudi,

situated on the north of Sicily. The estimable captain of the _Lucia_ came

on board to take leave, on his return to Trieste. The steamer, being

relieved of her burden, made her way briskly towards her destination; and,

before an hour had elapsed, we could perceive nothing but a small streak

of smoke in the haze of the horizon.

With light breezes, we came, on the following day, in sight of the island

of Ustica. Sea-gulls (_Thalassidroma pelagica_) enlivened the scene, as

they, from time to time, flew after the garbage thrown from the ship, or

sought for sea-nettles and other small inhabitants of the sea's surface.

These birds much resemble our land swallows, and their movements are so

graceful, that one cannot but admire them, especially when they lightly

touch the agitated water with their little webbed feet, and directly, as

if repelled, withdraw. The muscular power of these feathered creatures is

truly wonderful; they follow the ship for entire days continually on the

wing, ever on the watch to snatch at the little food which the sea seems

but scantily to supply to them.

[Illustration: "PALINURUS".]

Whilst we were passing down the Mediterranean, a great deal of time was

employed in drawing up regulations, and in digesting all those

instructions which had reached the Commander of the Expedition from all

sides, and by which we were to be guided in our future proceedings.

The scientific gentlemen were the first who received certain rules for

their guidance; for, life on board a ship, and especially of a man-of-war,

is so entirely different from that on shore,--the etiquette and usages

practised appear, to those unused to the sea, so vexatious and annoying,

that it was absolutely necessary to inform them of the regulations which

are essential in order to keep so singular an organization as that of a

ship at sea in working order. Erelong every one perceived, that the

matutinal annoyance of holystoning the decks, the daily cleaning of

everything on board, &c., are measures of importance, which contribute

materially to the preservation of the health of the crew, and that a

strict observance of discipline is absolutely necessary to exercise their

powers, and thus to fit them for all eventualities.

For the better accommodation of the naturalists, a place on the lower

gun-deck was fitted up for those operations which, on account of the

limited space and noxious exhalations, could not well be performed in the

cabins.

We had a large quantity of alcohol on board, destined for the preservation

of interesting objects of natural history. In order to prevent any

calamity by fire arising therefrom, the whole quantity was put in a large

iron tank placed in the hold, and covered over with sand. It will,

however, be seen in the sequel, that even this precaution proved

insufficient to protect the ship from the ignition of this

highly-combustible substance.

The meteorological observations, and those connected with the physical

geography of the sea, were entrusted to four officers, who, like those

attached to the watches, had alternately to be at their posts, and had, at

prescribed hours, to observe the barometer, thermometer, and psychrometer,

as well as the temperature of the surface of the sea, the state of the sky

and the ocean, and to note down the obtained results. One of the junior

officers was intrusted with the nautical observations on shipboard, as

well as the astronomical and magnetical on shore.

The midshipmen were at the same time trained by study and practice, so as

to enable them to assist the officers in their duties. Besides the men on

the look-out, one of the midshipmen was employed on the same service. In

stormy nights, when the wind is howling, and rain or snow falling, this

post is certainly not very pleasant, but is, as may readily be imagined,

most important.

Life in the limited space of a ship, completely cut off from the external

world, is so peculiar and interesting to those unacquainted with the sea,

that we will endeavour to describe a day passed on board the _Novara_,

from the instant when at daybreak the bustle and activity begin, till the

late hour when night reminds one of repose, those sweet moments which

carry the voyager to his distant home on the wings of a dream.

As the sonorous bell strikes the fifth hour of the morning, the crew are

called on deck by the boatswain's whistle, the hammocks are slung up and

stowed away, and the work begins.

This is the busiest time of the day, and for the mere spectator the most

uncomfortable. On all sides scouring, rubbing, sweeping are going on,

floods of water are streaming along the decks, and he who is not as yet

familiar with these cleaning processes, runs some risk of a ducking as

soon as he makes his appearance outside his cabin. These morning ablutions

are, however, indispensable evils on board ship, for cleanliness is a

condition essential to the preservation of health, and even the quantity

of humidity which penetrates the timber, and renders the air damp, appears

to be less injurious than the omission of these daily scourings.

When the cleaning of the various parts of the ship is finished, the

idlers, and such of the officers as are off duty, appear on deck, whither

people come to enjoy the fresh air, and to greet the opening day. It may,

however, be permitted to observe, that a sunrise at sea, notwithstanding

its various charms, is by far less imposing than the same scene on a lofty

mountain, where the veil of night seems to vanish as if by magic, and

luxuriant nature lies at our feet like a smiling infant awaking from a

lovely dream. That wild majesty of scenery, that overpowering grandeur of

gigantic mountain forms, such as one sees in the Swiss or Tyrolese Alps,

is wanting at sea, where the rising sun pours his beams only over a

boundless world of water.

The sailors breakfast at 7, the officers at 8, and the Commander at 9. At

the latter hour the bugle sounds the order to "clear the ship," when the

cleaning of arms, guns, and all other articles of metal connected with the

ship's armoury, begins. During this process the band plays cheerful airs,

so that the work is done whilst keeping time with the music, which serves

to lighten the labour. This duty requires to be completed within

forty-five minutes, and terminates with an inspection of the men and their

arms.

This being over, officers and midshipmen off duty assemble together with

the naturalists in the reading-room. Most of the books in the library

referred to those countries likely to be visited by the Expedition, so

that every one might previously obtain useful information relative to

their physical, historical, and social conditions.

The naturalists employ the greater part of the day in their cabins, noting

down their observations, and preparing for those to be made in the course

of the voyage. The crew are kept in activity by being drilled and

otherwise occupied.

The men dine at 12; the dinner of the officers is served up at 3, and that

of the Commodore at half-past 3 o'clock P.M. The remainder of the

afternoon is spent in prosecuting the labours begun in the morning. Thus

steals on the evening, when a general assemblage takes place on deck, for

air and exercise.

[Illustration: SEAMEN OFF DUTY.]

The occurrences of the day, the sunset, the curious formation of the

clouds, or the bewitching beauty of a brilliant tropical sky at night,

form interesting topics for lively discussion. It is, however, rather

daring to institute a comparison between the splendour of the sky in the

tropics and that of our higher latitudes. For, most men become more or

less unjust towards the beauties of a new and foreign natural scenery, in

consequence of their not being able to divest themselves of former

impressions produced in them by phenomena of a similar nature. What

impressions are, for instance, deeper in young and old, and excite more

delightful recollections than the starry sky of home? And can it be

disputed that the association of ideas has a most powerful effect upon

the impressions made by those phenomena of nature which are so peculiarly

attractive and so deeply fixed in the human mind?

The conversation generally becomes more lively on those evenings when the

moon, placid friend of the sailor, appears on the distant horizon,

shedding her silvery beams over the unbroken expanse of water. The

influence which she exercises on the state of the weather, even the

prejudices and superstitions connected with our satellite, offer subjects

of interesting debate; involuntarily the mariner looks with grateful

feelings towards that heavenly luminary, the mild soothing light of which

diminishes the number of his anxious nights, protects him in present,

warns him of remote dangers, and influences so powerfully that vast

element on which he passes the greater part of his life. Indeed he who has

ever spent a dark and stormy night on the ocean, when the ship, lashed by

the fury of the waves, and borne resistlessly along, stands in constant

peril of coming in violent collision with a vessel similarly

circumstanced, or of being dashed to pieces on some iron-bound coast of

rugged rock, easily comprehends and will excuse the sailor who ascribes to

the moonlight somewhat of a supernatural and mysterious power.

In this manner, and notwithstanding the continued sameness, days and

months glide away like hours, until we again cast anchor, and only the

work accomplished gives an idea of the length of time which has been

passed at sea.

Sunday alone breaks the monotony of life on board, when, after the diurnal

cleaning of the ship, and the inspection of the crew, the officers, and

all the men who are not on duty, assemble for divine service on the lower

gun-deck, where the chaplain says mass on a temporary altar, whilst the

ship's band performs sacred music. In the afternoon the men off duty amuse

themselves for a couple of hours with the "_tombola_," a game much liked

by our sailors. Between 6 and 7 P.M. the band plays on deck, whilst the

sailors are cutting grotesque figures to the music. The singular capers by

which all evince their happiness; the good-humoured awkwardness with which

each clings to the brawny arm of his companion; the mock graceful air

those who enact the gentler sex assume in the dance, and, finally, the

affected attitude with which the cavaliers bow to their partners as if

they really were of the gentler sex--all this is most ludicrous and

amusing. The playing the national dance "Monferina" always elicits a

particularly hearty reception. There is a peculiar charm in national

melodies, even though they awaken no political reminiscences like the

Marseillaise, or the Rakoczy; they electrify alike the educated and the

men of the people; a thousand pleasing recollections suddenly crowd into

the memory, and when the well-known tunes strike the ear, the heart seems

to live again in bygone times! As if touched by magic, the sailor from the

Adriatic, as soon as the Monferina is struck up, seizes his neighbour by

the arm with a noisy shout and hurls him about in wild hilarity; his

thoughts seem as if flying towards his distant home, where, in the country

inn, with a buxom lass on his shoulder, he has waltzed away many a happy

hour. The whole village, with all its familiar faces, seems to revive in

his memory during the playing of the melody,--now he fills his glass; now

he clinks it merrily with that of his companion; now he presses his

sweetheart more closely to his side: Lo! suddenly a shrill whistle pierces

the air, the music ceases, the call is heard "to fall in," and the yet

dance-stricken sailor, suddenly, as if awakening from a sweet reverie, is

once more standing on the deck of the _Novara_!

The frigate, in the Mediterranean also, maintained her superiority as a

sailer. The corvette _Caroline_ was able to keep the prescribed distance

from the _Novara_ only by the latter reefing some of her sails. As some

magnetic observations were to be made at Gibraltar, and, as we had to

ascertain the results of the various chronometers on board, on the 12th of

May we signalled the corvette to take her own time and rejoin us at

Gibraltar, as we were anxious to avoid unnecessary detention.

The acquisitions of the naturalists had, as yet, been very scanty: to

their great annoyance they could not even obtain any of the tortoises,

which, from time to time, approached the ship, though they were repeatedly

fired at, and on one occasion a boat was launched, in the hope of catching

some of them. The specimens which we saw were from fifteen to twenty

inches in diameter; they mostly floated quietly on the surface, and seemed

sleeping or basking themselves in the sun.

The night of the 16th May was exceedingly boisterous, and almost tangible

darkness prevailed; thunder, lightning, and occasionally strong easterly

squalls, raged furiously, and only subsided towards the morning, when it

cleared up with fresh southerly breezes. Not being far from Cape de Gatt,

on the Spanish coast, prudence required us to change course, and, during

the continuance of stormy weather, to keep at a respectful distance from

the shore. Here a merchantman, apparently an American, bore down so close

upon us, that, in the darkness, an unpleasant collision seemed

unavoidable. However, we tacked about, and thus, fortunately avoiding our

dangerous neighbour, safely proceeded on our course.

It is truly astonishing how often merchantmen, entirely forgetful of their

own safety, from want of caution, or presumption, or it would occasionally

seem, sheerly from acting upon peculiar and abnormal principles of

navigation, wantonly expose ship, men, and cargo to many dangers, which

might easily be avoided, particularly in cases where no tacking is

required, and only a slight touch of the rudder would suffice to prevent a

collision, which is always attended with danger to the smaller ship. In

this respect the North Americans are very unpleasant neighbours on account

of their national vanity, and the Dutch for their phlegmatic temperament

and the indifference they evince on such occasions.

On the 18th of May, the small rocky island of Alboran, in the narrow part

of the sea between Africa and Spain, was observed; being flat and without

vegetation, it is scarcely perceptible, and the land-fall during the night

should be carefully avoided. The erection of a lighthouse on this island

would certainly be regarded as a great boon by all who navigate the

Mediterranean.

On the 19th of May, the sea suddenly assumed a peculiar orange colour; a

dust-like covering was observed on the surface of the water, and at some

depth white points might be seen, mingling with each other in the wake of

the ship. Clouds of this orange-like matter appeared spread upon the sea,

which thereby lost its usual transparency. On closer examination this

phenomenon appeared to arise from a mass consisting of myriads of minute

animalculæ, which had a yellow opaque kernel, the gelatinous covering of

which was transparent and colourless. A quantity of sea-water impregnated

with this matter, having been brought into a dark room, gave out a light,

and when agitated, such brightness proceeded from it, as justified the

anticipation that, during the night, the whole sea would be illuminated.

Accordingly the wake of the ship was illuminated by a wonderful stream of

light, in the depths of which larger masses of luminous matter could be

discerned, whilst on the surface there was a sparkling and glittering, as

if all the stars of the firmament were reflected in the water.

This phosphorescence of the sea, for the explanation of which we are

chiefly indebted to Professor Ehrenberg, proceeds for the most part from

the emanations of light from molluscæ of the genus _Medusa_, and other

living phosphoric animalculæ; sometimes, however, as for instance in

Venice, it arises from the putrescent fibres of decayed molluscæ, and

other organisms in a state of decomposition.

On the evening of the 20th the splendid Ceuta Light was seen, which, even

at a distance of twenty miles, looks as if it were quite near. This

lighthouse is of the utmost importance to ships emerging into the Atlantic

from the Mediterranean, as the current is exceedingly powerful, and during

the night is apt imperceptibly to carry a vessel out of her course. On the

morning of the 21st, the ship lay in a calm before the rock of Gibraltar.

Barren, gray, and gloomy rose now before our sight this rocky,

gun-studded, colossal sentinel of that vigilantly-prudent, energetic, and

jealous Power, which is so constantly seeking to extend her rule wherever

her own interests are concerned, or where she thinks it advisable to make

herself respected by other nations.

A light breeze sprang up, and at half-past 3 P.M. the anchorage, eleven

and a half fathoms in depth, was reached. The frigate now lay in front of

the Alameda or public gardens of Gibraltar, situated near the town gate,

called the Ragged Staff. This anchorage is tolerably safe at this season,

but in autumn and winter, as well as generally in strong easterly winds,

it is not to be recommended, it being preferable to haul further in

towards the place where the merchant-vessels usually lie. We saluted the

English flag on the fortress with twenty-one guns, which were immediately

answered from the ramparts. There were no English men-of-war in the Roads,

except the sloop _Curlew_, Capt. Horton. The following morning our

consort, the _Caroline_, anchored in our vicinity.

The first day of the arrival of a man-of-war in harbour is attended with

much inconvenience, particularly if she carries the flag of the

Commodore, or it happens that the mail packets are arriving or departing,

or that there are many ships of war in the Roads. The latter was not now

the case, but so many visitors, letters, and newspapers arrived at once,

that neither the one nor the other could be thoroughly enjoyed.

The local authorities, the governor, Sir James Fergusson, at their head,

were extremely obliging and attentive; Mr. Falkland, an officer of the

Engineers, was placed at our disposal; a specially-reserved site was

assigned us for astronomical and magnetical observations; huts were

erected by the workmen of the arsenal for the protection of the

instruments, and in short everything, calculated to promote scientific

labours, was provided. The Chancellor of the Austrian Consulate, Mr. John

Frembly, himself a geologist, proved likewise to be of great service to

our scientific men: and it was considered a fortunate omen to have found,

at this our first anchorage, so much sympathy with the objects of the

Expedition.

[Illustration: VIEW OF GIBRALTAR FROM SEAWARD.]

[Illustration: ROCK OF GIBRALTAR.]

III.

Gibraltar.

STAY FROM THE 20TH TO THE 30TH MAY, 1857.

Political Significance of the Rock.--Courtesy of the British

Authorities.--Fortifications.--Signal Stations.--The only

place in Europe frequented by Monkeys.--Calcareous Caves.--

Chief Entrances into the Town.--Shutting the Town Gates.--

Public Establishments.--Inhabitants.--Elliott's Gardens.--The

Isthmus, or Neutral Ground.--Algeziras.--Ceuta.--Commerce and

Navigation.--Excellent regulation in the English Navy relative

to Officers' Outfit.--Small-pox appears on Board the

_Caroline_.--Departure from Gibraltar.--A Fata Morgana.--The

_Novara_ passes the Straits.--Take leave of Europe.--Voyage to

Madeira.--Floating Bottles to ascertain the Currents.--Arrival

in the Roads of Funchal.

This remarkable promontory, which in our days has obtained so much

political importance, the Calpe of the ancients, constituted of old, with

the opposite Abyla,[7] the so-called pillars of Hercules, celebrated, at

the same time, as the boundary of the then-known world. It derives its

name from the corrupted Arabic _Gebel_ (mountain) and _Tarik_, the name of

a Moorish conqueror, who had pitched his camp here (A.D. 711). Like a

colossal giant, guarding the portal of Europe, and converted, by the

energy and ingenuity of the British, into an almost impregnable outpost,

this precipitous rock has, as regards the Mediterranean, the same high

strategic importance for that great maritime people, as Heligoland for the

German Ocean, Aden for the Red Sea, Ceylon and Singapore for the Indian

Archipelago, Hongkong for the Chinese waters, or the Cape and St. Helena

for the Atlantic Ocean.

[Footnote 7: The present Apes Hill.]

Gibraltar was already strongly fortified, when it belonged to the

Andalusian kingdom, but its grandest fortifications date from the treaty

of Utrecht (1713), when it became an appanage of the British crown.

Stupendous and incomparable are the works which since that period have

been executed on it, though the calcareous formation of the locality and

its numerous caves may have considerably facilitated their construction.

The English authorities, who so kindly assisted in the scientific

researches, obligingly furnished each individual of the frigate's staff

with a written permission to inspect the fortifications as often as they

pleased, and thereby afforded them the particular gratification of being

able to view and admire these vast structures in all their details.

Excellent and well-kept roads lead to the principal fortifications, which

only begin at an elevation of several hundred feet above the town. The

galleries, hewn in the solid rock, forming a kind of casemates, are of

such breadth and height that they may be conveniently traversed by a man

on horseback with his hat on. They have been constructed at an immense

expense of labour and money, and are designated by various names, as

"Upper gallery," "Lower gallery," "Queen's gallery," "St. George's Hall,"

and so on. Their extent is estimated at an English mile, but is probably

much greater. Besides these galleries, passages run for miles in the

interior of the rock, affording the garrison a thoroughly-protected

connection with all points that may chance to be threatened.

The grandest and most imposing of these marvellous excavations are the

"Queen's gallery" and "St. George's Hall." According to carved

inscriptions, most of them were begun and completed between the years 1783

and 1789. At the period of our visit, there were mounted on the different

fortifications 707 guns, about one hundred of which peeped out of the

smaller embrasures. Since that date, however, the number is said to have

been increased so as to amount now to about 1500.

During the stay of the _Novara_, it fortunately happened that the birthday

of Queen Victoria was celebrated, and thus an opportunity was offered of

seeing the fiery mountain in full activity. Though the occasion was

peaceable, yet the imposing spectacle gave a tolerable idea of the

elements of destruction which Gibraltar could put in action if really

attacked. The governor of the fortress, surrounded by a brilliant staff,

in which the Spanish governor of Algeziras and his officers played but a

sorry part, reviewed the garrison, consisting of infantry, cavalry, and

artillery, to the number of from 5000 to 6000 men; and whilst the troops

defiled in slow and quick step, lightnings and thunders issued from all

the crevices and embrasures of the artificially-perforated rock; huge

volumes of dense smoke followed, and a rolling subterraneous rumbling gave

the mountain exactly the character of a volcano suddenly burst into

action. The echo of these salvoes of rejoicing must have been heard, not

only in the adjacent parts of Spain, but also on the more remote coast of

Africa; and he who was ignorant of the real cause, might have supposed it

a grand rehearsal of that fearful tragedy which the English seem

determined to perform in the event of an attack. The supposition, however,

that the guns of Gibraltar are able entirely to command the Straits is

erroneous, for these, at their narrowest part, are 12-1/2 miles wide, and

not even the Armstrong guns, with which the fortress has lately been

furnished, have so extensive a range. The English are, however, able to

command the Straits by a fleet, which would find in the Bay of Gibraltar a

sufficiently safe and roomy anchorage.

From the fortifications, a narrow and rather steep path leads to the

telegraph station, at an elevation of 1300 feet above the level of the

sea. Steamers and men-of-war, as soon as visible, are signalled from this

point by means of immense balls and flags. It would be very difficult to

signal merchantmen in the same way, as, during a prevailing westerly wind,

multitudes of ships often appear to the eastward of the rock, anxiously

waiting for a favourable easterly breeze to carry them through the

Straits; in the same way the westerly horizon is sometimes crowded with

ships, prevented by contrary winds from entering the Mediterranean.

We found at the station an Aneroid-barometer, and a thermometer. The

advantages for navigation and physical science of extensive meteorological

observations, regularly made, are so evident, that it is astonishing to

see how often opportunities are neglected for making them, such as are

offered here.

There was no opportunity for seeing any of those families of monkeys, the

occasional appearance of which on the Rock of Gibraltar has given rise to

tales found in books of travel of the existence of a submarine

communication, through which this single representative of the genus in

Europe has found its way to this rock from Africa. Sometimes, however,

during easterly winds, single individuals are observed on the highest

peaks on the eastern side of the rock, where it is completely

inaccessible; probably the remnants of that species (_Inuus ecaudatus_),

which at some former time, either by chance, or human agency, have found

their way hither from the Moorish coast.

The calcareous caves are very remarkable. That on the western side, called

St. Michael's, situated at a height of 800 feet, is the most important. It

contains beautiful stalactite formations, and seems to be of considerable

extent; it has, however, not been closely examined hitherto, as only a

small part is conveniently accessible. St. Martin's Cave, on the

south-east, likewise about 800 feet above the level of the sea, is

smaller, but its stalactites are of a purer whiteness. A third was

discovered a few years since on the eastern side of the rock at a height

of only 80 feet, the lower portion of which consists of accumulations of

sand and recent shells. There have also been found bones and teeth of

large herbivorous animals.

[Illustration: ROCK CAVERN IN GIBRALTAR.]

The characteristic vegetation of the mountain is Spanish broom (_Spartium

junceum_), the yellow blossom of which strikes the eye pleasingly at a

great distance. There is also one species of cactus, and one of the dwarf

palm (_Opuntia vulgaris_, and _Chamærops humilis_), which grows in great

abundance, and forms, on the south face of the rock, almost the only

vegetation, whilst, on account of difference of temperature, it is

altogether absent on the remaining sides.

Gibraltar has little to attract strangers to settle; barracks, military

store-houses, and fortifications, render the appearance of the place

peculiarly monotonous, the more so that there are no elegant buildings, or

fine shops, on the rock. There was nothing observed, however, to confirm

the statement, in a celebrated geographical work, copied by all later

compilers, that "most of the houses are painted black, to soften the glare

of the sun, and prevent an attacking enemy having a distinct view of the

place." The town, which is built in terraces on the side of the rock, is

accessible only from three points. The greatest portion of the traffic

passes through the so-called Old Mole at the north end, whilst the

entrances on the south are generally used by men-of-war sailors only. All

are opened at 5 in the morning, and, according to the season, shut between

7 and 8 in the evening, precisely twenty-five minutes after the first

signal-gun. This closing of the gate is attended with ceremonies verging

on the comic. A broad-shouldered corporal, carrying in his hand a heavy

bunch of immense keys, marches, visibly impressed with the importance of

his mission, in measured steps, accompanied by a number of red jackets

with fixed bayonets, towards the massive town-gate; the bridge is then,

with much ado, drawn up, and the horribly-creaking gate, with great

exertion, closed, bolted, and finally locked. After "gun fire" no one can

leave the town by the Old Mole; at 10 P.M., however, and at midnight, a

little postern is opened, through which those jolly stragglers, who have

forgotten in merry company the measure of time, may slip out to return to

their floating abodes. From this hour till morning all communication with

the harbour is arrested, and the utter impossibility (except in

extraordinary cases) of leaving the town _after_ this hour, has given rise

amongst the people to the saying, "There is only _one_ thing more

difficult than to get _out_ of the town after midnight, and that is to get

_in_."

There are in the city two Anglican churches, one Wesleyan, one

Presbyterian, two Catholic chapels, and two synagogues. The garrison

library, where likewise a great number of journals and magazines are kept,

possesses 22,000 volumes, amongst them several very rare and costly works,

especially of ancient Spanish literature. It was founded in 1793 by

Captain Drinkwater, and has been hitherto kept up by private subscriptions

and the profits arising from a printing-establishment attached to it.

Gibraltar owes to the energy and public spirit of the governor, Sir James

Fergusson, the foundation of several important establishments and

undertakings. Since the beginning of his administration in 1856, the

number of public schools has been considerably increased, the town

supplied with gas, and well-arranged public baths established.

The city does not possess a single well or spring; the water used is

obtained from tanks, in which the rain is collected. The quantity of rain

that fell during the twelve months of 1855 amounted to 78 inches; in 1856,

it is said to have been only 24 inches. Nevertheless, there is at no time

any scarcity of water. The Government have lately caused the erection of

a distilling apparatus for making sea-water fit for domestic purposes,

which, however, hitherto has not been used.

The population of Gibraltar, including the garrison of 6000 men, amounts

to about 20,000 souls, consisting of Spaniards, English, Italians (mostly

Genoese), Portuguese, Moors, Turks, Greeks, and Jews; indeed, a mixture of

races, customs, and manners such as scarcely can be found at any other

place in Europe. The native residents call Gibraltar briefly _the rock_,

and themselves, with a kind of pseudo-patriotism, _rock people_, though by

the officers of the garrison and navy generally complimented with the name

of "rock-scorpions."

The permanent settling of foreigners, in consequence of its being a

fortress, requires a number of formalities, which have the effect of

limiting the population; and even the English portion must be considered

migratory, as it consists chiefly of military and government officers,

who, after the lapse of certain intervals, exchange in regular order.

The only really beautiful walk in the place is Elliott's Gardens, situated

at the south end of the town, laid out in a grand style, but disfigured by

a tasteless bronze statue of General Elliott (afterwards Lord Heathfield),

the heroic defender of Gibraltar in 1782. In the evenings, when one of the

military bands is performing, the grounds are thronged by visitors on

foot, horseback, and in carriages, whilst loving couples, of all races and

grades, ramble in happy union through the shady avenues.

Near the gardens, towards the south, is a second quarter of the city,

which mostly consists of government buildings. On the lowest terrace,

which juts furthest into the sea, stands the lighthouse, on the celebrated

"Europa Point."

[Illustration: SOUTH GATE, GIBRALTAR.]

Narrative of the Circumnavigation of the Globe by the Austrian Frigate Novara, Volume I (Commodore B. Von Wullerstorf-Urbair,) Undertaken by Order of the Imperial Government in the Years 1857, 1858, & 1859, Under the Immediate Auspices of His I. and R. Highness the Archduke Ferdinand Maximilian, Commander-In-Chief of the Austrian Navy. · 第 9 / 15 章