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Explorations in Turkestan : Expedition of 1904 : vol.2 |
INDEX.
PAGE.
Deposition zones-Continued. Drainage, 'recent decrease in surface 322-324
the lacustrian in Aralo-Caspia 292-294 Duerst, Prof. J. U 449
recent developments in the alluvial and description of animal remains from exca-.
flying sands of Aralo-Caspia.. 294, 295 vations at Anau 341-442
kurgans in the 303-307 Dugès, A 405, 406, 408
the building of a tilting delta on 321 Dunes, dune-sand, etc., see Sands.
under the control of man. 324-326 Dushambeh 270, 459
interbedding of the alluvial and flying Dust, cyclonic storms of 244
sands at Anau 327 precipitated as loess 244
the Murg-ab delta and man's control of the settling ground of 245
alluviation 330, 331, 332, 333, ff. absence of dust deposits on Pamir 253
Deposits from ice, water, and wind 244-247
See Deposition zones. Eeman Tepe 318
of man (culture débris) 299, ff. Egypt 302, 334, 440
irrigation deposits 324-327 Eichbaum 416
of man, water, and wind at Anau 328-329 Elisée Reclus 295, 296
of man, water, and wind at Mery 334, ff. Elm, black 273
of the Zerafshan River (glacial origin of Equus asinus 403, 416, 417, 424
loess) 281-282 caballus 390, 395
of ancient dune-sand interbedded with Exmoor pony 416, 421, 422
the Anau delta clays 327-328 caballus donlesticus 360
in the Aralo-Caspian Basin, variations caballus fossilis 402
in amount of 292 caballus fossilis Rütimeyer, the ances-
Desert-interior of Pliocene Asia 243 tor of the oriental and occiden-
of Gobi (uptilted borders of) 243 tal races 431
the Northern Pamir an extreme 251 caballus fossilis robustus scu germani-
of Great Kara Kul 251-252 eus Nehring 428
deflation of Kara Kul 253 caballus germanicus 398
preservation of ancient topography on caballus germanicus seu robustus 399
Pamir 254 caballus Linnæus 384
valley of Eastern Karategin 266 caballus nehringi 398, 399, 420
Kizil Kum 271 the forest type .430, 431
Tarim 282, ff. caballus pumpellii 397, 398, 412, 413, 417
transgression of the Kara Kuni 293-294 418, 419, 422, 423, 424, 4z6, 429, 430
Deserts, physiography of 243-298 the type of the desert 431
Desert basin as an organic whole 243-25o caballus robustus Nehring, the type of
essential character of a 243, ff. the steppes 431
three agencies of erosion and five deposi- hagenbeckii 398
tion zones in a 244-246 hemnionus....387, 388, 389, 392, 393, 395, 396
interlapping of deposition zones in a.... 247 hemionus (var. kiang) 387, 390, 391
the cyclical development of an ideal... 247-250 mauritanicus 402
Desiccation (see Climatic) of Tarim basin . .. 286 namadicus 428
Devenzano 418, 427, 43o onager 387, 388, 390, 391, 394, 396
Diest 352 parvus 401
Displacement, orogenic evolutions in the piscinensis 428
desert basin 249 plicidens Owen 428
Distributaries, unstability of the Murg-ab, przewalskii 387, 388, 390-398, 40!
and their effect upon man... 331-333 411-415, 419-426, 428, 429, 431
Djigettai 390,391 quaggoides 402,428
Djillan-ooti Darya 318-320 quaggoides a ffinis Woldrich 428
Dog, ancient Egyptian 352 robustus 401, 417
Assyrian and Babylonian 352 sivalensis. 428
Australian 348, ff. spela?us 402, 428
brought from Inner Asia to Europe... 354, 43o stenonis 395, 396, 402, 417, 418
dingo 348, ff., 435 420, 421, 422, 423, 428
of Anau II 348-354 stenonis affinis Woldrich 428
relationship of 35o taniopus 416
tables of comparison with dogs of Erke Tepe 334
Eurasia and Africa 348, 349, 353 Erosion, the agencies of 244
subfossil 353 man as a geologic factor in 299
of Bohemia, pariah 349, fi. in the obliteration of kurgans 303-307
shepherd 349, ff. Erosion cycles of an ideal desert basin 247-250
turbary 439 the Pamir 259
264
Domestic animals, census of, in Turkestan the Alai Valley
in 1903 433 general discussion of the duration and
relative percentage of, in Cultures I and magnitude of 267-268
II at Anau 438 Karategin and Hissar 274
Don River 292, 297 the Zerafshan Valley 277-2822
Dongola 388 Tarim
Dongus-tau 288 the Alai Mountains 287
Dordogne 403 • the Fergana Basin 290
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