CHAPTER XII.

THE NINETEENTH CENTURY AND AFTER: ASIA AND AUSTRALIA

The beginning of the nineteenth century was signalized by the

initiation of the great trigonometrical survey of India, and the

first half-century was a period of much important geographical and

anthropological work within that empire, but to no great extent beyond

its boundaries, though in 1808 a mission penetrated to the sources of

the Ganges, and Baluchistan and Afghanistan were in some part explored

by officials of the East India Company. But the physical problems of

the heart of the continent were left to a later period--those, for

instance, concerned with the trans-Himalayan region (as viewed from

India), including Tibet, eastward that region so important in the

hydrography of the continent, where the river systems of China and

Burma take their rise, northward the deserts of Mongolia and Turkestan,

westward the nodal mountain-region of the Pamirs, and the area which

long concealed the sources of the Brahmaputra (Tsanpo) and the rivers

of Punjab. In spite of the endeavours of the Tibetans to hold inviolate

the secrets of their land--in great measure successful so far as their

capital, Lhasa, was concerned--the Indian native surveyors, such as

Nain Singh, Krishna, and Ugyen Gyatso, were able to penetrate the

country, and even Lhasa itself; their work covered the period 1863–82.

And the last quarter of the century provides a wonderful record of

continuous exploration in Tibet, as will appear from the mere quotation

of names and dates--P. Bonvalot and Prince Henry of Orléans, 1886–87;

W. W. Rockhill, 1888 and 1891; Hamilton Bower, 1891–92; Dutreuil de

Rhins and F. Grenard, 1893–94; St. George Littledale, 1895; Captains

W. S. Wellby, 1896, and H. H. P. Deasy, 1896, whose work was afterwards

extended by Captain C. G. Rawling and by Sir M. A. Stein; and Sven

Hedin, 1896–98, 1899–1902, 1906–08, whose last journey revealed the

existence, long suspected, of the great mountain system north of the

upper Tsan-po. This list is by no means exhaustive, nor can be that of

the Russians who worked from the opposite direction, from their own

territory; their leader was Nicolai Prjevalsky, who in 1871–73 and in

1876 worked in the Tsaidam region and made the first contribution to

the mapping of the important hydrographical area above referred to, and

in 1879 studied the vast physical changes which have taken place in

Central Asia within historic times, and form one of the most remarkable

geographical problems in the world. He continued his work in 1883–85,

and was followed by Pevtsov and Roborovsky (1889 and 1894), P. K.

Kozlov, Potanin, and many others. The names of Russian scientists, such

as Baron A. Kaulbars and L. Griesbach, are also associated with the

problems of the Aral and Caspian depressions. The former extensions of

human settlement over areas now covered by the Central Asian deserts

has been brought to light in great measure through the researches of

Sven Hedin, and especially of Sir M. A. Stein. The general result of

all these investigations has been to modify profoundly, even during the

present generation, preexisting ideas of the physical geography of the

central region. Nor should we overlook the work of recent travellers

in China proper, a broad canvas on which outlines had been sketched

earlier; but details remained, and still in great part remain, to be

filled in, though Ferdinand Baron von Richthofen, in the course of his

seven journeys in 1868–72, left few districts entirely unvisited.

The problem of the former existence of flourishing communities in areas

now desert, and of the causes of the change, has a partial counterpart

in southern Arabia. The modern period of Arabian exploration began

earlier than that of Central Asia. The journeys of J. Halévy (1869),

E. Glaser (1889), and J. T. Bent (1893) in the south were primarily

archæological in purpose. In other parts of the peninsula the work of

J. L. Burckhardt (1815), Sir R. F. Burton, Captain G. F. Sadlier, W. G.

Palgrave, Charles Doughty, Wilfrid Blunt, C. Huber, Musil, Leachman,

and others, has made it possible to lay down at least the position

of the chief towns and settlements, and the main physical outlines,

with close accuracy, save in the Dahna or great desert of the southern

interior, which remains untrodden.

The detailed exploration of Australia began from Sydney, the earliest

settlement, and was directed along the coast rather than towards the

interior, the penetration of which was difficult. George Bass, after

a short expedition inland, was accompanied by Matthew Flinders in

exploring the coast of New South Wales as far as the George River

and Hat Hill towards the end of the eighteenth century; in 1797–98

Bass Strait was found to separate Tasmania from the mainland, and

that island was circumnavigated. Bass was subsequently lost in

South America; but Flinders extended the work in 1801–03, when,

having sailed from England, he worked from King George Sound at the

south-west of Australia right round the south, east, and north coasts

as far as Arnhem Bay, west of the Gulf of Carpentaria, and would have

accomplished more but for the unseaworthiness of his ship. Flinders

was not only a competent explorer, but also a man of theories: he

took the limestone cliffs of the Great Australian Bight (south coast)

for coral reefs, and when he entered Spencer Gulf he thought of a

northward strait connecting with the Gulf of Carpentaria, and conceived

an Australian archipelago; nor was he wholly disabused until he had

definitely located the heads of both gulfs. A number of important

inlets, such as Port Phillip, Keppel Bay, and Port Bowen, were

thoroughly investigated by him, and he also surveyed the Great Barrier

Reef. And the substitution of the name of Australia for New Holland is

due to a suggestion of his. His unfinished survey of the western shores

was completed by Captain P. P. King in voyages between 1817 and 1822.

The accident of a drought in 1813 drove some of the Sydney settlers

to look for new pastures in the hinterland. The divide between the

short eastward and the long westward drainage systems was surmounted

with difficulty; a road to the point where the town of Bathurst

afterwards grew up was promptly made, and an arresting geographical

problem confronted the investigators when the westward-flowing rivers

Macquarie and Lachlan were found. Lieutenant Oxley, R.N., attempting to

follow the Lachlan in 1815, was presently brought to a halt by great

swamps. He struck south to avoid them, and narrowly missed discovering

the Murrumbidgee river, before he turned back to carry to Sydney the

conviction that the westward drainage generally was lost in swamps

fringing an inland sea. Cunningham found a route from this coast up

to the rich Liverpool Plains, towards the north of New South Wales,

in 1823; but for the most part exploration was temporarily directed

to the south-west, and Hamilton Hume and Hovell in 1824–25 took an

inland route from New South Wales to the south coast on the west side

of Port Phillip. This inlet was not recognized by them; they returned

to report that they had seen the coast-land, and found it good, further

to the east at Western Port; settlers who visited that district on

their recommendation were disappointed, and the development of the

Victoria coast-lands received a set-back in consequence of this error.

Cunningham in 1828 opened the route from the coast at Brisbane to the

downs of the south Queensland hinterland. In the same year a new phase

was entered in the solution of the problem of the far interior, when

Charles Sturt, carrying with him Oxley’s conviction of the existence

of an inland sea, journeyed inland at a season of drought to find

the Macquarie river losing itself on the dry plains, and the Darling

flowing salt. He attributed this fact to an admixture of sea-water, and

set down the interior of the continent as a desert. In the following

year he settled the problem of the drainage of the Murrumbidgee,

Lachlan, and Murray rivers by following them to the mouth of the Murray

in Lake Alexandrina (south coast); and although he now held that the

waters of the Darling were included (as they are) in this system, it

was still doubted whether there was a divide between north and south

flowing waters about the central latitude of New South Wales, where,

in the interior, high ground was known to exist. Sir Thomas Mitchell

settled this question by a great journey in 1836, which, among other

results, immediately threw open to settlement the fertile country

about Port Phillip, hitherto, as we have seen, neglected through the

misunderstanding of Hume and Hovell.

The larger problems of Australian geography were thus early settled,

though there was (as even now there is in some parts) a multitude of

details to be filled in. But the leading questions awaiting solution

by explorers now become economic rather than purely geographical. Thus

we find Dr. Leichhardt’s first expedition (1844), from Moreton Bay

in southern Queensland by the Burdekin, Mitchell, and Roper rivers

to Port Essington, inspired by the conception of an overland route

between Sydney and a northern seaport. He was lost (and the mystery

of his fate was never solved) in 1848 in attempting a crossing of the

continent from east to west, and Kennedy’s expedition in the same year,

in attempting to cross northern Australia, also met with disaster,

where A. C. Gregory succeeded in 1855–56. The penetration of the

interior from the south and the crossing to the north had attracted

travellers before this; Eyre in 1840 had discovered the series of

salt lakes and swamps which he lumped together under the name of Lake

Torrens, while Sturt in 1845 added little to Eyre’s discoveries,

and, after failing to penetrate the Stony Desert to the north, put a

temporary period to explorations in that quarter. Babbage in 1856 and

Parry in the following year obtained more accurate knowledge of the

Lake Torrens region, and Goyder in 1857 reported a great freshwater

lake which was found later to have been conceived out of some shallow

pools and visions of the mirage. J. M. Stuart’s six expeditions

from south to north in 1858–61 added much to exact knowledge; that

of Robert Burke and William Wills in 1860–61, ill-managed as it was

and ending in the death of the leaders, obtained a fame in excess

of its scientific value; but other expeditions sent in search of it

achieved better results, and incidentally made clear the danger of

assessing the worth of some of the inland districts on the report of

one traveller who might have come upon them at an unfavourable season.

Thus J. McKinlay in 1861 brought word of fertile lands which Sturt had

condemned as desert. The many journeys through the interior of Western

Australia--such as those of J. S. Roe (1836), the brothers Gregory,

H. M. Lefroy (1863), Sir J. Forrest (various expeditions in and

after 1869), Warburton (1873), and Ernest Giles (first crossing from

Adelaide to Perth by an inland route, 1875)--though often of extreme

importance from an economic point of view, whether concerned with the

discovery of pastoral lands or of gold or other mineral fields, can

only be referred to here as having gradually opened up the detailed

knowledge of this part of the continent, and as having redeemed it

in part from a reputation for complete inhospitality, until we have

now a trans-continental railway planned to connect the systems of

south and of western Australia. The exploration of the Kimberley and

north-western areas of the state was delayed until the latter half of

the last century.

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