National Institute of Informatics - Digital Silk Road Project
Digital Archive of Toyo Bunko Rare Books

as it can anywhere be seen in the valleys of the Rhine or of the Danube. I might even speak
of 'Berg' and 'Thal-Löss,' but I shall not enter into details on this occasion; for I may have
a much better opportunity of studying this remarkable deposit. At present I will only notice
that commonly we meet with extensive deposits of Loess only in the valleys. Its thickness
varies in places from ten to eighty, and more, feet; a fine yellowish unstratified clay, occasion-
ally with calcareous concretions and plant fragments. In Europe the origin of this extensive
deposits was, and is up to the present date, a disputed question. Naturally, if a geologist is
not so fortunate as to travel beyond the 'Rhine' or 'Donau-thal,' and is accustomed to be
surrounded with the verdant beauty of these valleys, he might propose half a dozen theories,
and as he advances in his experience disprove the probability of one after the other, until his
troubled mind is wearied of prosecuting the object further. Here in the desert countries,
where clouds of fertile dust replace those of beneficial vapour, where the atmosphere is hardly
ever clear and free from sand, nay occasionally saturated with it, the explanation that the Löss
is a subaerial deposit, is almost involuntarily pressed upon one's mind. I do not think that by
this I am advancing a new idea; for,—unless I am very much mistaken,—it was my friend
Baron Richthofen who came to a similar conclusion during his recent sojourn in Southern
China.

Yarkand lies about five miles from the river, far away from the hills, in the midst of a
well cultivated land, intersected by numerous canals of irrigation; a land full of interest for
the agriculturist, but where the geological mind soon involuntarily falls into repose. And
what shall I say of our road from Yarkand to Kashghar? Little of geological interest, I
am afraid.

Leaving Yarkand we passed for the first few miles through cultivated land, which, how-
ever, soon gave away to the usual aspect of the desert, or something very little better. A few
miles south-west of Kokrabad a low ridge runs from south-east to north-west. If we are
allowed to judge from the numerous boulders of red standstone and Gryphæa marl, some of
considerable size and scarcely river-worn, we might consider the ridge as being composed of
cretaceous rocks. But one hardly feels consoled with the idea, that in wading through the
sand he should only cross a once cretaceous basin, and that the whole of this country should
have remained free from encroachment of any of the kainozoic seas. It is very dangerous
to jump to conclusions regarding the nature of a ground untouched by the geological hammer.
The answer to any doubt must for the present remain a desideratum. On the fourth day of
our march approaching Yangihissar, we also crossed a few very low ridges, but these consisted
entirely of gravel and marly clay beds, most of them dipping with a very high angle to south
by east, the strike being nearly due east and west. South of Yangihissar the ridge bent
towards south-west, and there was also a distant low ridge traceable in a north-easterly
direction, the whole having the appearance of representing the shore of some large inland
watershed. From Yangihissar to Kashghar we traversed only low land, as usually more or
less thickly covered with a saline efflorescence, but still to a considerable extent cultivated.
Here in Kashghar the distant heights of the Kuenlün, of the Pamir and Thinshan ranges, are
ready to unfold their treasures, whether we go in a southerly, or westerly, or northerly direc-
tion; geological ground is even nearer to be found in some of the low ridges from twelve to
thirty miles distant, while the Moralbashi forests lying eastward, invite the zoologist and
sportsman. I trust we shall soon be able to see and relate some novelties from our neigh-
bourhood.

Kashghar, 20th December 1873.

Section III.

Note regarding the occurrence of jade in the Karakash valley, on the southern borders of
Turkistan, by Dr. F. Stoliczka, Naturalist attached to the Yarkaud Embassy.

The portion of the Kuenlün range, which extends from Shahidula eastward towards
Kotan, appears to consist entirely of gneiss, syenitic gneiss, and metamorphic rocks, these
being quartzose, micaceous, or hornblendic schists. On the southern declivity of this range,