IIIF Color HighRes
National Institute of Informatics - Digital Silk Road Project
| |||||||||
|
| IIIF Color HighRes |
| Explorations in Turkestan : Expedition of 1904 : vol.2 |
 |
 |
 |
 |
 |
 |
|
|
 |
|
|
|
|
|
|
|
|
Citation Information
II
INDEX.
PAGE.
Boucher de Perthes 403
Boulogne 414
Bovina, of Anau I and II 359-369
tables of comparisons 359, 362, 366
comparative heights 369
Briesen 348, 426
Broca 401, 451
. Bruniquel 404
Bubales arnee Kerr 359, fi.
bainii 359
pakeindicus Falconer 361
occipitalis Falconer 363
Budenz 351
Bumüller, J. 451, 454
Bural-bas-tau, peneplain 277
described by Davis 287, f f .
Bushed 416
Cmsar 430, 431
Camel 378
of Anau II 383-384
Camelus .342-383
alutensis 384
bactrianus 384
knoblochi . 384
Canidm 345, 354
Vulpes montana Pearson 345
Canis. 341, 342, 345-354
familiaris matris optimæ Jeitteles..348, ff.
430, 435, 438, 439, 441
hodophylax 346
inostranzewi 347, 348, ff., 353, ff., 435
lupus Linnmus 346-347
molossus 350
pallipes Sykes 346, 347, 352, ff.
palustris 350
poutiatini .. 347, 348, 349, 350, 353, ff., 435
Cuon alpinus Pallas 347
Canning-town 374
Capra 342
hireus riitimeyeri Duerst 378, 380-381
cegagrus 380
cretensis 381
Cardamone 395, 418, 420, 421
422, 423, 424, 427, 430
Carice system of underground water supply. . 302
Caspian Sea 245,292
Caucasus 438, 439
Cavern springs 324
Caverne . 392
Cavicornia of Anau I and II 359-382
Cedar 273
Cervus moral Ogilby 382
Charjui 297
Cherry, wild 273
China, Mai Valley route from Bactra to ... 307-3Io Chinese records of desiccation and dune ex-
pansion in Tarim 286
Chinese Turkestan, preservation of ruins in 306
Chosroes II . 362
Christians, early Nestorians of the Zerafshan 314
Chust 289
Cindré 392, 402, 419, 429
Clercq 352
Climate, diurnal extremes on the Pamir .... 253
relation between climate and landlocked
seas 245
in an ideal desert basin 247-248
See Aridity.
Climatic cycles, ideal 247-248
in the Aralo-Caspian Sea expansions. 292-294
PAGE.
Climatic cycles-Continued.
recorded by the interlapping of deposi-
tion zones 247
Climatic change recorded-
by recent changes in the glaciers of Pamir 258 by the Zerafshan glacier and its tribu-
taries 279-280
in a recent oscillation of the alluvial zone
in Tarim 283-284
in the late expansion of flying sands in
Tarim 286
in recent oscillations of the deposition
zones of Aralo-Caspia 294-295
in the present oscillation of the deposi-
tion zones in Fergana 290
in a recent decrease of surface drainage
in the Kopet Dagh 322-324
in the periodic invasion and burial of dunes on the margin of the
Anau delta 327-328
in the unconformities of the growth of
Anau delta 329-330
in the superposition of deposition zones
at Mery 336
Conglomerate, uptilted piedmonts of, in Fer-
gana 289, ff.
in Western Tarim basin 282, ff.
Conner, F 440
Couvres 419, 429
Culture deposits (kurgans):
accumulation of . 299-300
distribution of 301
relation between erosion and burial of . . 303-305
preservation of 305, 307
grading into irrigation deposits 329
how they are recognized 328
Culture, uninterrupted growth made possible
in high valley oases 313
Curchy 392, 419, 429
Cuvier 404
Damburachi 268
Dara-ut Kurgan 309*
Dargum canal 281, 283*
David, Abbé 363
Davis, W. M 254, 277, 285, z87, 292, 293
Débris of human occupation discussed geo-
logically 299-301, 303-307
Deer 382
Deflated silts and residual dunes 285*
Deflation and secular disintegration of the
Pamir 253
surface boulders of moraines planed off by 257
of silt plains in Tarim 283, ff.
of the Pamir 252*, 253*
Deformations, see Uptilted piedmonts; Warpings. Deformations of the Hissar Valley evidenced by a fault-scarp and capturing
of the Kizil Su 270, fi.
Delta oases 301, ff.
of Anau . 320, fi.
of Mery 330-333
Deposition zones, origin and arrangement of
the five 244-246
interlapping of, caused by climatic os-
cillation 247
in an ideal desert basin 247-250
recent oscillations of the alluvial in
Tarim 284-286
recent oscillations of the alluvial in
Fergana 290
|
|
|
|
|
|
|
|
|
Copyright (C) 2003-2019 National Institute of Informatics and The Toyo Bunko. All Rights Reserved.