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THE DlSCUVEllEUS OF THE CAUCASUS 9<br />

once undertook to prove to me that there are no glaciers at all<br />

in the Himalaya. In the Caucasus there have heen of late<br />

years not a few such<br />

'<br />

specialists,' and their contributions to<br />

Caucasian literature have been considerable. They make the<br />

most of theli- own expeditions — generally failures— above the<br />

snow-level. Those who are more successful they describe as<br />

'<br />

mere tourists.' They see very little and what ; they do see is<br />

frequently out of focus. Their ignorance of movmtain phenomena<br />

and the terms properly applicable to them often renders their<br />

narratives misleading. They constantly boast that their facts<br />

and descriptions are 'scientific,' forgetting that a statement whicli<br />

is neither accurate nor intelligible cannot be made scientific by<br />

any<br />

initials attached to the name of its author.<br />

who misuse the name of Science !<br />

Enough of these pretenders<br />

I have dealt with some of them individually elsewhei-e. I need<br />

not waste my readers' time by pursuing in detail their divagations.<br />

The only errors T shall correct here are those into which<br />

serious students and writers of authority have been led in past<br />

years by the impei'fect material at their disposal and the partial<br />

character of the exploration of the snowy chain. Let us turn<br />

back to some of the statements found in works of authority<br />

current at the date of my first journey. The 1860 edition<br />

of Keitli Johnston's Dictionary of Geography contained these<br />

very remarkable assertions, the first of which was repeated in<br />

1877 :—<br />

'The mountains of the Caucasus are eitlier Hat or cup-shaped; the<br />

existence of glaciers is uncertain.'<br />

The doubt as to glaciers was shared by Agassiz. The erroneous<br />

information as to tlie main features of the geological structure of<br />

the mountains given by Kupffer in 1830 was still current in 1868,<br />

and Sir Roderick Murchison was eager for information on this point.<br />

The existence of erratic blocks had been denied by Abich and his<br />

;<br />

assertion, after he had corrected it himself, was repeated by Tchiliat-<br />

chefF, a Russian traveller of considerable reputation. There was<br />

similar uncertainty as to the existence of mountain lakes or tarns,

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