144. GREEK WHITE MARBLE.—_The Marmo Greco, of Italian artists, is of

snow─white colour, in fine granulations_; and somewhat harder, and

consequently capable of higher polish, than most other white marbles. It

is found near the river Coralus, in Phrygia.

_ITALIAN MARBLES._—145. PARIAN MARBLE _is of snow─white colour,

inclining to yellowish white_. It is obtained from quarries in the

island of Paros, is finely granular, and, when polished, has somewhat of

a waxy appearance. Parian marble hardens by exposure to the air, and is

one of the most permanent kinds that is known. Varro and Pliny each

state that it was named _lychnites_, by the ancients, from a Greek word

signifying a lamp, because it was generally hewn in quarries by the

light of lamps. The finest Grecian sculpture that has been preserved to

the present time is of Parian marble. The principal statues of it now

extant are the Medicean Venus, the Diana Venatrix, and Venus leaving the

Bath. It is also Parian marble on which the celebrated tables at Oxford

are inscribed.

146. CARRARA MARBLE, the purest of all the kinds with which we are

acquainted, is to this day obtained from quarries near the town of

Carrara. _It is of brilliant white colour, has a granular texture; and,

when broken, sparkles like sugar._ This marble, which is almost the only

one in use by modern sculptors, was also quarried and wrought by the

ancients.

It is susceptible of a high polish, and is applicable to every species

of sculpture, except when, as is too often the case, dark veins intrude,

and spoil the beauty of the work. In the centre of the blocks a

beautiful kind of rock crystals, called _Carrara diamonds_, are

sometimes found.

During the late war with France, the exportation of statuary marble from

the countries under the dominion of Buonaparte was prohibited; and, at

one time, it became so scarce in England as to be sold at the rate of

more than seven guineas per cubic foot. The block of marble for the

statue of his late Majesty in the great Council Chamber at Guildhall,

London, was stated by the public prints to have cost twelve hundred

guineas.

147. LUNI MARBLE _is a snow─white, compact, and finely granular

variety_, which was obtained by the ancients from quarries on the coast

of Tuscany. It was preferred by the Grecian sculptors, both to the

Parian and Pentelic marbles; and it is usually supposed that the

Belvidere Apollo, as well as the Antinous of the Capitol, was wrought

out of this marble. There is now found at Luni a white marble,

variegated with red spots and dots.

148. GREEN ANTIQUE MARBLE, or VERDE ANTIQUE _of the Italians, is a

mixture of white marble and green serpentine_ (132). This is believed to

have been obtained from some part of Italy, but the quarries are not now

known.

149. SIENNA MARBLE _is of close texture, and yellowish colour, disposed

in large irregular spots, surrounded with veins of bluish red, passing

sometimes into purple_. It is not uncommon in the vicinity of Sienna,

and is in great request, throughout Europe, for chimney─pieces and

ornamental furniture.

150. BROCATELLO MARBLE is somewhat like the last; but is also

irregularly marked with various shades of red, and, in some parts, with

white.

151. MANDELATO MARBLE _is of light red colour, with yellowish white

spots_. It is found at Lugezzana, in the Veronese. Another variety,

bearing the same name, occurs at Preosa.

152. VERDE DI PRATO MARBLE _is a green marble, marked with darker green

spots_, which is found near the town of Prato in Tuscany.

153. LAGO MAGGIORE MARBLE _is a beautiful kind, white, with black spots

and dots_. It has been employed for decorating the interior of many

churches in the Milanese.

154. BRETONICO MARBLE.—This beautiful marble, which is found near the

village of Bretonico, in the Veronese, _is varied with yellow, grey, and

rose colour_.

_FRENCH MARBLES._—155. Many valuable kinds of marble are obtained from

different parts of the French territory.

156. CAMPAN MARBLE.—Three kinds of marble are known by this name, all of

them procured from immense quarries at Campan, near Bagnere, in the

Pyrenees. The first, called _Green Campan_, is of pale sea─green colour,

and exhibits, on its surface, lines of much deeper green, forming a kind

of net─work. The second, called _Isabel Campan_, is of delicate rose

colour, with undulating green veins. The third variety, the _Red

Campan_, is of deep red colour, with veins of still deeper red. The

green variegations in this stone are formed by a talcy mineral,

intermixed with the lime─stone.—The Campan marble is well adapted for

slabs, tables, chimney─pieces, and other ornamental purposes in the

interior of buildings; but, if exposed to the weather, the talcose

substances perish, and leave hollow spaces which render its surface

rough and uneven.

157. GRIOTTE MARBLE _is of a deep brown colour, with blood─red oval

spots, formed by shells_. Its name has been obtained from its brownish

colour, being similar to that of the cherries that are called by the

French _griotte_. This marble has, of late, been much used in the

decoration of public monuments, and in splendid furniture, in France.

Some of the ornaments of the Triumphal Arch of the Carousel are made of

it. The department of Herault is the part of France from which it is

obtained. It sometimes contains large white veins, which destroy the

harmony of the other tints.

158. MARQUESE MARBLE.—This, which is obtained from quarries, near the

village of Marquese, between Calais and Boulogne, is marked with

_different shades and variegations of white and brown_. Of this marble

Buonaparte commenced a magnificent column on the heights near the sea,

at Boulogne, to commemorate his victories; but, since his dethronement,

the erection of this structure has been discontinued.

159. SARENCOLIN MARBLE _is distinguished by exhibiting large zones, and

angular spots of yellow or blood─red colour_. It is found at Sarencolin,

in the High Pyrenees.

160. ST. BEAUME, or LANGUEDOC MARBLE, _is of light red colour, marked

with white and grey zones, formed by madrepores_. The eight columns

which adorn the Triumphal Arch, in the Carousel at Paris, are of this

marble. It is obtained from quarries at St. Beaume, in the department of

Aude.

161. BRECCIA MARBLE OF THE PYRENEES.—One kind of this marble contains

black, grey, and red, middle─sized spots in a brownish red ground. It

admits of a good polish. Another kind has an orange─yellow─coloured

ground, containing small fragments of snow─white colour. Both these are

found in the Pyrenees.

_SPANISH MARBLES._—162. Few countries are more productive of marble than

Spain; and in few countries are the public monuments and buildings more

profusely decorated with marble. The vault of the theatre of Toledo is

supported by 350 marble columns; and an ancient mosque at Cordova is

ornamented with 1200 columns, most of which are of Spanish marble. The

palace and church of the Escurial, and many of the churches in Madrid,

are decorated with marbles of the most beautiful description.

163. WHITE SPANISH MARBLE.—Near Cordova; at Filabres, three leagues from

Almeria, in Grenada; and in some other parts of Spain, white marble is

obtained, which is susceptible of a good polish, and is well adapted to

the general purposes of sculpture.

164. SEVILLE MARBLE _is a beautiful red variety, with shining red and

white spots and veins_. In the vicinity of TORTOSA is found a kind of

marble which has a _violet ground, spotted with bright yellow_; and near

GRENADA a marble of _green colour_, which somewhat resembles the

celebrated verde antique (149).

165. SPANISH BRECCIA.—There are several beautiful varieties of breccia

in Spain. At Riela, in Arragon, there is one, composed of angular

portions or fragments of black marble, embedded in a reddish yellow

base. The breccia marble of Old Castile is of bright red colour, dotted

with yellow and black, and encloses fragments of pale yellow, brick─red,

deep brown, and blackish grey colour.

_GERMAN MARBLES._—166. Germany abounds in marbles, and affords many

kinds which are remarkable both for beauty and singularity. Of these the

kind best known is

167. LUMACHELLI MARBLE.—_This exhibits beautiful iridescent colours,

which are sometimes prismatic internally, but more commonly of various

shades of red or orange_; whence it has also obtained the name of _fire

marble_. Few kinds of marble are more generally admired than this. It

has a dark ground, and is marked throughout with the appearance of small

whitish shells, which, in certain parts, refract the most beautiful and

brilliant colours. This marble is cut into the tops and bottoms of

snuff─boxes, and several other ornamental articles. It is found in veins

at Bleyberg, in Carinthia.

168. Many beautiful kinds of marble are obtained from the island of

SICILY, particularly one called _Sicilian jasper_, which is red, with

stripes like ribbons, white, red, and sometimes green. SWITZERLAND

abounds in marbles; PORTUGAL, SWEDEN, and NORWAY afford few. In the

RUSSIAN EMPIRE many have been noticed, particularly among the Uralian

mountains. The late Empress Catharine caused an immense palace to be

built for her favourite Orloff, which is entirely coated, both inside

and outside, with marble. She built the church of Isaac with marbles of

different kinds, on a vast space, near the statue of Peter the Great, in

Petersburgh. We are at present very imperfectly acquainted with the

marbles of ASIA. Dr. Shaw mentions a red marble obtained from Mount

Sinai; and Mr. Morier, in his journey through Persia, speaks of a

beautiful translucent kind which he calls _marble of Tabriz_, and the

colours of which are light green, with veins sometimes of red, sometimes

of blue. He says it is cut into large slabs, some of which he describes

to have measured nine feet in length, and five feet in breadth.—No

account has hitherto been published of the marbles of AFRICA.—In the

United States of AMERICA many kinds of marble have been discovered, some

of which have been wrought, and polished; but very imperfect

descriptions have yet been given of them.

169. Few countries produce a greater variety of excellent marbles than

the BRITISH ISLANDS. Although these marbles are seldom noticed much

beyond the limits of the districts in which they occur, many of them are

admirably adapted for ornamental purposes; particularly for slabs and

chimney─pieces. It is much to be regretted that we should send to

foreign countries for stones which, in many instances at least, could

certainly be as well supplied from our own. The following is an

enumeration of a few of the most important kinds.

_ENGLISH MARBLES._—170. PETWORTH MARBLE, when cut into slabs, is equal,

both in beauty and quality, to many of the marbles imported from the

Continent. The Earl of Egremont has, at Petworth, several chimney─pieces

formed of it. Much of this marble was used in the cathedral church of

Canterbury. The pillars, monuments, vaults, pavement, and other parts of

that venerable structure, have been formed of it. The archbishop’s chair

is an entire piece of Petworth marble. This marble is found in greatest

perfection upon an estate of the Earl of Egremont, at Kirdford. It lies

at the distance of from ten to twenty feet under the surface of the

ground, and in flakes or strata nine or ten inches in thickness.

Petworth marble is also an excellent stone for walls; and, for paving,

it cannot be excelled. When burned, it also constitutes a valuable

manure, superior, as some farmers imagine, even to chalk.

171. PURBECK MARBLE is obtained from the island of Purbeck, in

Dorsetshire. _It is of dark colour, and contains numerous small round

shells_, which, when it is cut and polished, mark it with roundish

variegations of brown, dark green, and grey. This marble was formerly

more used than it is at present. Several of the small columns, and many

of the monuments, in the churches of Dorsetshire, and the adjacent

counties, are formed of it. But it is not so durable as many other

kinds. Wherever it is long exposed to the weather, the surface cracks,

splits off, and becomes defaced.

172. BABBICOMBE MARBLE is one of the most beautiful kinds that is found

in any country. _It varies in colour, from light brown to deep red_; and

large slabs of it have been obtained that are elegantly and diversely

marked, some in streaks, others in spots, and others in different

coloured shades.

This kind is quarried at Babbicombe, in Torbay, Devonshire, and is

extensively manufactured into chimney─pieces in the West of England. An

attempt was lately made to introduce it in London; but, from its not

being the production of a foreign country, this has failed of success.

173. DERBYSHIRE MARBLE.—There are, in Derbyshire, several kinds of

marble, most of which contain an abundance of fossil shells, and other

remains of marine animals. At Wetton, near Ashbourne, a beautiful kind

is obtained, of greyish black colour, which contains a vast number of

whitish and very minute shells. This has the name of _bird’s eye

marble_. Near Monyash a beautiful variety is found, of a cheerful

colour, inclining to brown red, and full of large marine figures in all

directions; these, when the marble is cut, appear white, and afford a

pleasing contrast.

174. KENDAL MARBLE.—Some varieties of black, grey, and brown marble, are

wrought near Kendal, in Westmoreland. These somewhat resemble the

Derbyshire marbles; and, like them, are manufactured into

chimney─pieces, and ornamental slabs for houses. Several of the slabs

are found to contain corallines, and the remains of other marine

animals, which vary their appearance in a very pleasing manner.

The MONA MARBLE is a species of serpentine intermixed with white

limestone: it has been already described (132).

_SCOTTISH MARBLES._—Scotland affords many valuable and beautiful

varieties of marble.

175. TIRIE MARBLE.—Few of the British kinds of marble have been more

admired than that obtained from Tirie, one of the Western Islands of

Scotland. _It is of a reddish, sometimes a delicate rose─coloured tint,

and sometimes white; and is always intermixed with other minerals which

add to its beauty._ The most common of these is of black colour, and

called hornblende; the others are pale green sahlite, blackish brown

mica (123), and green chlorite. In some varieties the hornblende is more

abundant than the marble.

176. ASSYNT MARBLE.—At Assynt, in Sutherland, _a white marble_ has been

discovered, which is perfectly solid and pure, and entirely free from

blemishes or stains. Blocks or slabs of it may be cut of almost any size

that can be required. This marble acquires a smooth surface, but remains

of a dead hue; whence, of course, its uses as an ornamental marble are

much circumscribed.

177. ISLE OF SKY MARBLE.—There is found in the Isle of Sky a marble of

pure white colour, which appears capable of yielding large and valuable

blocks. Its fracture is granular and splintery, and its texture fine. It

is harder, heavier, and more compact than the marble of Carrara (146);

and is apparently well fitted for all the purposes of sculpture. But it

has the defect of being very unequally hard. While some parts of the

stone are nearly as easy to work as that of Carrara, other parts are so

hard as to add a charge of near fifty per cent. to the cost of the

working.

178. SUTHERLAND MARBLE.—Some beautiful specimens of marble of dark brown

colour, veined with whitish, light red, or light brown, have lately been

brought from the county of Sutherland. These appear of close texture,

are susceptible of a beautiful polish, and are capable of being wrought

into extremely beautiful slabs for chimney─pieces and other ornamental

purposes.

179. GLEN TILT MARBLE _is of white or grey colour, and veined or spotted

with yellow or green; some specimens are nearly white_. The granulations

are peculiarly large; and, in its aspect and composition, the Glen Tilt

has great general resemblance to the Pentelic marble (143). This marble

has of late attracted the notice of the Duke of Athol, through the

suggestion of Dr. Macculloch; and chimney─pieces of it have since been

made. It is obtained from a valley of the same name in the county of

Perth.

180. BLAIRGOWRIE MARBLE.—A few miles from Blairgowrie, in Perthshire,

there is an excellent granulated broad─bedded marble, _of sugar─loaf

texture, and as white as the finest statuary marble_. It may be easily

raised in blocks and in slabs of great size, perfectly free from

blemishes. This marble is supposed to be well adapted for ornamental

architecture, but its large sparry texture renders it unfit for the

sculptor.

181. GLENAVON MARBLE _is of white colour, with large granular

concretions_, somewhat like spangles, and as large as the scales of

fishes. This is a valuable kind; but its situation in the forest of

Glenavon, on the property of the Duke of Gordon, is remote and difficult

of access.

182. BALLICHULISH MARBLE.—On the north side of the ferry of

Ballichulish, in Lochaber, there is a rock of marble, of beautiful

_ash─grey colour_, and of a fine, regular, and uniform grain, which is

capable of being wrought into blocks or slabs of any size, and is

susceptible of a fine polish. This marble is finely sprinkled throughout

with grains and specks of pyrites (236), and with grains and specks of a

beautiful lead ore, which to the eye appears to be rich in silver. If

used for ornamental purposes, it would be a bright and beautiful

metallic marble.

183. BLAIRMACHYLDACH MARBLE.—In the bed of a river, at the farm of

Blairmachyldach, about three miles south of Fort William, is a singular

marble, consisting of _a black ground, flowered with white_. It is of

fine close grain, but not very hard. The flowering in it is light, and

beautiful, like fine needle─work, or rather resembling the frosty

fret─work upon glass windows, in a winter morning.

The cutting and polishing of marble appear to have been performed by the

ancients nearly in the same manner as it is with us. In polishing, the

first substance employed is a sharp, coarse─grained sand. Afterwards a

finer sand is used, then emery (58) in different degrees of fineness.

These are followed by a red powder called tripoli (119): and the last

polish is given with putty.

184. _BLACK MARBLE is a species of limestone, of uniform black colour,

and easily distinguishable, by an excessively disagreeable smell, which

is emitted on rubbing two pieces of it together, or striking it with a

hammer._

Few minerals are susceptible of a more beautiful polish than this. It is

consequently much used for chimney─pieces, small columns, vases, and

other ornamental work. There are two quarries of black marble near

Bakewell, in Derbyshire: and it is manufactured to a considerable extent

by Messrs. Brown and Co. at Derby, who have fixed up in their ware─rooms

a large slab of it as a looking─glass.

By the ancients it was much prized. Marcus Scaurus is said to have

ornamented his palace with columns of black marble, each thirty─eight

feet high; and many of the monuments of ancient Persepolis were executed

in it. M. D’Avejan, Bishop of Alais, used a kind of black marble for

paving the apartments of his palace; but the friction and heat rendered

it so fetid that his successors were compelled to substitute another

species of stone in its place.—The pavements, however, of many churches,

and of the porticos of several galleries, on the Continent, are of black

marble.

185. _CALCAREOUS ALABASTER is a species of limestone of somewhat whitish

or yellowish colour, translucent, and internally splendent or shining._

_It is nearly a pure carbonat of lime; and occurs in masses, hanging,

like immense icicles, from the roofs of lime─stone caverns, and also

coating the sides of such caverns._

The formation of this substance is deserving of notice. The water which

oozes through the crevices of limestone rocks, becomes strongly

impregnated with minute particles of lime. This water, when it has

reached the roof or side of a cavern, is generally suspended, for a

considerable time, before a drop of sufficient size to fall by its own

weight is formed. In the interval which thus elapses, some of the

particles of lime are separated from the water, owing to the escape of

the carbonic acid (26), and adhere to the roof. In this manner

successive particles are separated, and are attached to each other,

until what is called a _stalactite_, having somewhat the appearance of

an icicle, is formed. These stalactites are sometimes solid, having a

lamellar structure; sometimes of a fibrous texture, radiating from the

centre to the circumference, as may be observed when they are broken;

and sometimes hollow. If the water collects and drops too rapidly to

allow time for the formation of a stalactite, it falls upon the floor,

and there forms an irregular lump of alabaster, which has the name of

_stalagmite_. In some caverns, the separation of the calcareous matter

takes place both at the roof and on the floor; and, in course of time,

the substance upon each increasing, they meet, and form pillars,

sometimes of great magnitude.

Caverns of this kind occur in almost every country. Those of Derbyshire

are well known; but the most celebrated stalactitic cave in the world is

that of Antiparos, in the Grecian Archipelago.

The kind of limestone formed in the above manner is what the ancients

generally denominated _alabaster_. It was employed by them for the same

purposes as marble, was cut into tables, columns, vases, and sometimes

even into statues. They also used it in the manufacture of vases or

boxes for containing unguents. It is supposed to have been a vessel

formed of this stone that is mentioned in the Gospel of St. Matthew,

where it is said there came unto our Saviour “a woman having an

alabaster box of precious ointment.” In the National Museum at Paris

there is a colossal figure of an Egyptian deity, which is cut in a kind

of alabaster brought from the mountains between the Nile and the Red

Sea.

186. _TUFA, or INCRUSTING CARBONAT OF LIME, is a calcareous substance

deposited by such water as is impregnated with lime._

_It clothes, with a stony coat, the smaller branches of trees, leaves,

moss, plants, and other substances; and thus preserves them from decay,

by protecting them from the action of the atmosphere._

Most of the substances termed by the common people _petrifactions_

belong to this kind of lime. They are, however, merely covered with, and

by no means converted into stone.

The dropping well at Knaresborough, in Yorkshire, is particularly

celebrated for them. An overhanging rock, several yards in depth, has

been gradually formed of the calcareous matter which the water holds in

solution; and, from this rock, it incessantly drops into the basin

below. The persons who have the care of the place constantly keep these

petrified articles for sale. Even old wigs and hair brooms are subjected

to the powers of the water, to furnish subjects for attraction to the

visitors. There are other springs of this description in Oxfordshire and

Somersetshire, and particularly at Matlock, in Derbyshire. We are

informed that at Dalton, on the south side of Mendip, the workmen not

unfrequently discover large pieces of oak enveloped in blocks of stone

which are four or five tons in weight.

Blocks of tufa are, in some countries, cut and used for building stones;

and this substance, when burned, becomes an excellent lime. Pieces of it

are sometimes hollowed, and used as filtering stones.

In the British Museum there is a human skull completely incrusted with

stone, which was found in the river Tiber.

The warm baths of Hungary are often so thickly coated at the sides and

bottom with tufa, that, during certain intervals, it actually fills up

the tubes and canals through which they are supplied. The _fur in

teakettles_ is a somewhat similar deposit from water in boiling.

187. _PORTLAND STONE, BATH STONE, KETTON STONE, are different kinds of

limestone; and, of a texture so hard and compact as to be used in

building._

Useful Knowledge: Volume 1. Minerals Or, a familiar account of the various productions of nature · 第 8 / 21 段