II INDEX. 
PAGE. 
Boucher de-Perthesi.. 2 cnn sinter rns 403 
Boulogne. (282 tune cut aon tice ae ee eee 414 
Bovitia, of Anau andclleaeersr ete cere 359-369 
tables of comparisons...........359, 362, 366 
comparative heights......... 369 
Briesen..5.cnays teeny aesds cess ene ean meres 348, 426 
Broa a.gsis syn oan eee ee he sneer Rilo 401, 451 
Bruniqiue] Poca seis eee eee eee 404 
Bubalis.atnée Kerri. see ee eee B50n ui 
DONTE SSO eee 359 
paleindicus Falconer... ..........+--: 361 
OCcepiialis Valconeta ae teen ieee 363 
Budettzi:} 20. ar ee oe eer ets 351 
Pepuboeh bl Corgis Mey San sero mG Ciuice om opomene 451, 454 
Bural-bas-tatrspeneplaia.. 2.7 te ene 5) 
described by Davis.t.7.. ese 287, ff. 
Bushéd,..c hace eee ete ciate aren aetna, 416 
Cobar 35.3. seine ote eke ere eee ee ete 430, 431 
Camel, Sew kas niealor sche oa ee ee eae ee 378 
Of Amar LGictctsus were o> Cree 383-384 
Camelusicvon Gaia cae Cee eee ae ee 342-383 
CIUENISES oe arom rat per tena ra ae 384 
DACELANUS.. eionir teases oi ce. o, teste tee 384 
Rnobloche. s aerstecn eo ete coe ieee tee tel 384 
Canidae: 5 AR ae cae ee ee aces 345, 354 
Vulpes montana Pearson.............. 345 
CONT Se Soh ar eae a aero Ne ree 341, 342, 345-354 
familiaris matris optime Jeitteles. . 348, ff. 
430, 435, 438, 439, 441 
hodo phylaxis: sea eee ee 346 
inostranzewt...... 247" 348, 1.353. ao 
lupus Tignes on eee ee 346-347 
MOLOSSUS: Beas lets she te ee le 350 
pallipes Sykes........... 346,347,352, fe 
PALUSULUSS ieee erica oe sted ee 350 
poutratint . . 347, 348, 349, 350, 353, ff, 435 
Cuon alpinus Pallas. 220; 3)... te-ee 347 
Camhing-town F20% te ieee ee ee 374 
COPIA) Sore eee cate ae eee ee ee 342 
hircus riitumeyert Duerst......... 378, 380-381 
CPE PRE eh iris CE Cs Se oe ye 380 
CYELENSUS <n eens. seh A ee ee ee 381 
Cardamone= ste Le eee 395, 418, 420, 421 
422, 423, 424, 427, 430 
Carice system of underground water supply.. 302 
Caspian ‘Sain 7p. aneiacden ae aes ee 245, 292 
Caucasus iyacise evan ore eee eiel Pees eaters 438, 439 
Cavern Springs de ru ae oie eer 324 
Caverné 22. 05 haoue ess rate ea eee 392 
Cavicormia of Anan land Tia eee 359-382 
Cedars. 20.h6 3 soe ia elena eter ete 273 
Cervus maral Ogibyin..aeo eee eee 382 
Char tu fs Tae ha'dl ee Meriepo: rela ae eee 297 
Cherry wild son «tga eee eee 273 
China, Alai Valley route from Bactra to. ..307—310 
Chinese records of desiccation and dune ex- 
pansion in “Larinmn. Si.ea cee 286 
Chinese Turkestan, preservation of ruinsin.. 306 
Chosroes" TL ipa. ec crete ea ee ee 362 
Christians, early Nestorians of the Zerafshan 314 
Chust. cic. cee cae cea hain eee een aie 289 
Cindré:c is. ca ae ea eee 392, 402, 419, 429 
Clereg Meh d ste eRe eee eee 352 
Climate, diurnal extremes on the Pamir.... 253 
relation between climate and landlocked 
SCASiin shan pee eee 245 
in an ideal desert basin.............. 247-248 
See Aridity. 
Climatic cycles, ideal...... ie Met Bs ac 247-248 
in the Aralo-Caspian Sea expansions. . 292-294 



PAGE. 
Climatic cycies—Continued, 
recorded by the interlapping of deposi- 
tioh zones... el... eee nee 247 
Climatic change recorded— 
by recent changes in the glaciersof Pamir 258 
by the Zerafshan glacier and its tribu- 
taries ©.) 0 79 ey ee eee 279-280 
in a recent oscillation of the alluvial zone 
in Tarim... eee 283-284 
in the late expansion of flying sands in 
Tarim. \ cues ete eee 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 Daghs 29." .428" 322-324 
in the periodic invasion and burial of 
dunes on the margin of the 
‘Anat deltas... 7252) 2 ene 327-328 
in the unconformities of the growth of 
Anau deltatcns....ca0 ree 329-330 
in the superposition of deposition zones 
at Merv 20y.0c154. 2) soe 336 
Conglomerate, uptilted piedmonts of, in Fer- 
Pama.) Siri eee 289, ff. 
in Western Tarim basin... 4.4.7. .0)se 282, ff. 
Conner, Fo. cca) J +.2. ge ee 440 
Convres. QUA aigne Bead alent en ce 419, 429 
Culture deposits (kurgans) : 
accumulation’ Of {icice 2. vee eee 299-300 
distribution OF... ...o ce. cae eee 301 
relation between erosion and burial of. . 303-305 
preservation) of 27 ca. seu oie ee 305, 307 
grading into irrigation deposits........ 329 
how they are recognized.............. 328 
Culture, uninterrupted growth made possible 
in high valley oases.......... aes 
Garb ced +h, Me IE. SA oe oe 392, 419, 429 
Quvier o..0. 2 6 anal sr ee ee 404 
Damburachi.!.te% ohio Rie een 268 
Dara-ut Kurgan... ..¢. 0.55 06 cee ee eee 309* 
Dargum canal... cu ose es sa eee 281, 283* 
David, ABBE ...00i.8ac ec ete che sie ee ee 363 
Davis; Wie Mo ate anna 254, 277, 285, 287, 292, 293 
Débris of human occupation discussed geo- 
logicallyscky seHer re 299-301, 303-307 
Deer nnats 2 ix 25 ee cue oe ee ee 382 
Deflated silts and residual dunes........... 285* 
Deflation and secular disintegration of the 
Pamireneetatt aoe. 253 
surface boulders of moraines planedoffby 257 
of silt¢plains in’ Tarim! liye eee 283, 
ofthe Pamitiec: 0. Aone ee ee 252%, 253* 
Deformations, see Uptilted piedmonts; Warpings. 
Deformations of the Hissar Valley evidenced 
by a fault-scarp and capturing 
of the Kazi Siren eee 270% 
Delta oases .ci'c0n8 See keke Cae eee 301, ff 
Of. Amat 2.0 %cls dilcekaieg ) Sa ie nel tee 320, ff 
Of Mervin cians we oe Ak taceiate weet che ieee 330-333 
Deposition zones, origin and arrangement of 
the) fivew che. « soa taeda 244-246 
interlapping of, caused by climatic os- 
cillation) :34 Agate rie eee ee 247 
in an-ideal.desert basin®..cass- ce 247-250 
recent oscillations of the alluvial in 
Tarim > eo pe ane eee 284-286 
recent oscillations of the alluvial in 
Fergana 35.202 220. ee, See 290 

