国立情報学研究所 - ディジタル・シルクロード・プロジェクト
『東洋文庫所蔵』貴重書デジタルアーカイブ

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カラー New!IIIFカラー高解像度 白黒高解像度 PDF   日本語 English
0261 Southern Tibet : vol.6
南チベット : vol.6
Southern Tibet : vol.6 / 261 ページ(カラー画像)

New!引用情報

doi: 10.20676/00000263
引用形式選択: Chicago | APA | Harvard | IEEE

OCR読み取り結果

 

 

The localities of the plants collected have been arranged chronologically in the following enumeration wherein notes on the physical conditions , geographical position, height above sea-level , date of collecting and other information are given.

1894.

Litllc

Kara-kul, July i 8 94.

Little moraine lake, hardly v, km. from north to south, at the N. N. W. foot of Mus-tagh-ata, Eastern Pamir; at its southern shore enters the brook of Sarik-kol in several delta arms flowing across swampy meadows. Towards the south-eastern shore runs a mountain ridge called Kara-kir which to the north and along the northern shore is connected with old moraine ridges of gravel and sand, here and there interrupted by grassy ground and meadows. Erratic blocks are often seen. Along the western shore a mountain ridge is situated , though narrow meadows have space enough at its base. Here also the ground is often swampy. There are many springs at the shores and in the swamps. Moss is rather common on the moraines and mountain slopes. At several places there are small lagoons along the shores.

At the northern shore a little brook issues from the lake and joins the river Ike-bel-su. Along its banks are swampy meadows and small pools formed from springs.

N. W. of Little Kara-kul are the two lakelets Lower and Upper Basik-kul. To the latter three valleys come down from the S. W. One of them is called Kara jilga, and has a little brook partly fed by springs.

Little Kara-kul has an absolute altitude of 3720 m. Upper Basik-kul is at 3727 m. The lower part of the valley of Kara-jilga is a few meters higher. Swampy ground with grass is comparatively common in the last-mentioned valley and between it and Basik-kul.

The Korumde-glacier, July 27 th i 894.

This glacier issues from the névés of Mus-tagh-ata, and its snout points to the north, in the direction of the river Ike-bel-su.

The snout of this glacier is on both sides, more especially the left or western one, surrounded by moraines, consisting of gravel, blocks of all sizes, and sand. In the depressions between the moraines and at protected places there is some vegetation. The absolute altitude is 4367 m.