1V INDEX. 
PAGE. 
Erosion cycles—Continued. 
the Aralo-Caspian) Basin’ ao ane 298 
the Anau. Sa... 2s ewan ee eee te ee 322 
growth and oscillations of the Anau delta 
during the various nic.n 1s = 330 
HskimoS acs: scbik bre cro crenata 459, 460, 461 
Euphrates, cick eicAeed Boa pee eee 437 
Evolution of a continent.,..sstme trent 243 
desert: basin sui akknge ht 22k eerie 247-250 
EX 00f; POLY 25.6 en wae ern eee a 414 
Faiza bad - ic smpeeteeie omen ceeley Orns Raters 272 
Fault-scarp in the loess plain of Hissar.270, 272*, 274 
Fergana, abandoned oases of............. 317-320 
Fergana Basin, physiography of.......... 287-290 
Fischer, Hos fin sss sWrw ck 2 ee ee 452 
Kish traps of the Kazil Sus. eee eee 271% 
Flower, Wi. Harkins hess eet area 459 
Horsyth Ma jore|ia Corwen 386, 394, 402, 405 
Fowyents Aut cok ke cee ielee ee eae 403, 419, 429 
Fox fromsAnauts so <p oe atten eae 345 
table of measutements of 7.2. 7:,.2 5... 345 
tabular comparison of, with Eurasiatic 
FOXES sateen 346 
Fraas, Odckoiss «nse ee a ere One e 403, 416 
Frank, T......386, 388, 401, 406, 408, 412, 417, 429 
Fuegians..vastihon suena 457, 459, 460, 461 
Gaillard? <3. 3t.20 copes 0s Ais abn one eee B73 
Galeha.. ¢ sis saserece creas oie ee aes errs 265 
See Tadjik. 
Galcha: dialecticowapioscs> =e sone ee ke 312 
Galchas. . . 2097, 2707, 314", 315%, 316* 
Galcha Beg with his hunting eagle’ ei g cee 266* 
Garm 2's. sadn ale coe ee Se ress 269 
Gaudry,; Alber tiie sa setae ats cena ene 433 
Gazella subgutturosa Gueldenstedt......... 382, 435 
Genghis Khatsi.sia sls 2s yassceeee eae 332 
Gera .octs diohen ley oottene Ae mPa ee x eee na 414 
Gervais) Patil aos 05 <n cyoeaie 3 were easrerainee ete 345 
Ghiaur Kala, rapid deflation of the ruins 
during a sandstorm.......... 303 
physiographic shaft-explorations in. . . 333-337 
Glacial petiddisse% 65522. eee coon eens 250 
climate and conditions on the Pamir 
during thesceaaesae toe 256-257 
four epochs on the Pamir during the. . 254-257 
in the Alar Valley s.c coy seen 261, ff. 
in the: Zerafshan: «<\.;n se. 2--eee ee Pig heke sf 
correlated with the late ‘‘ Aralo-Caspian 
Dea. si te A ae eee eae 294, 298 
Glacial zones of ice mantles. ..i.66..0.4..- 245 
acceleration of each erosion cycle...... 248 
obstructions to stream erosion, preser- 
vation of ancient topography 
on Pamir hint eee eee 254 
clays deposited in Lake Kara Kul...... 2555 Is 
troughs in the Trans-Alai Mountains. 263 
alluviation of the Zerafshan gorge during 
the second and third erosion 
cyclesie:ni 5). ce anes 277-279, 281 
origin ‘of loéss=- era ee ee ee 281-282 
Glaciation of the gorges of the fourth erosion 
cycles, sites wan cee 279, ff., 282* 
Glacier ice-mantles of the Pamir during the 
first and second epochs...... 254-255 
ice of second epoch preserved under lake 
sediments of Kara Kul.°..... 256* 
Glacier of the Zerafshan, differential uplift 
and‘advancerole-sbeen. ee 280*, 281* 
of the Tokus Kungei."), .ntGoesnwewe « Pop eee 


PAGE. 
Glacier—Continued. 
Varkatelnita se 9 byes tees ote selene 282* 
of the Karaca tem iem sce cena ee 255* 
northeast ofmKiara Kail eines ee rere 257* 
Glacier-thrusted allttviuim: 5. 7.2 ase elena 279* 
Glaciers, coalescing fans or piedmont glaciers 
of the second epoch.......... 255 
of the Pamir, pectiliarities of ....-... 22 258 
differential uplift and expansion of..... S754: 
Glory 2s Ae ee eee 272 
Goatof Anat TL; soa dart ee ree 380-381 
table of dimensions and comparisons. . 381 
Cretan <, save scic 5 ae ORIU eee eee 380 
GObtRA a eden meen ers ee eee 244, 249, 282, 398 
Grass, settling ground of dust from the Kizil 
Kn 22 Hee oA ae ee og fst 
in the: Alay Valley <> ce Soe. curso eres 260 
during the glacial period.............. 298 
brackish water, and wire-,............ 252 
areas shrinking in Fergana............ 290 
Gtisonsis. ainsi Saree ere piste eee 415 
Gross Czernosek........ 367, 381, 411, 419, 425, 426 
Grotte dw Pontil 4... .2-5 7a. eee ee 375 
Gruim-Grshimatloz .. Se. 2. ape eee eee 402, 429 
Guanchass 2707.25: ee cee orotate 456 
Gulbrandsdals iki cs oe: ote ee 415 
Gulcha foie 20s ip ae ce ace ee oa 289 
Gulcha River :o2 5. 0.2204 ebee ae eee 289 
Gyaours River vanishing: ....°...c.. eee B28 
Ha wee. cide som « Sng Sn eae ee ene ee 269 
Hallstadts..¢.. S252. seas decease green ee 410 
Hensel Or ..0 5 250s op ep bw eter ee ee 421 
Hepbtirn 24 05..t ye cea ee eiceire eee 451 
Heschelermocncci bree 392, 393, 394, 416, 426 
Hickory s00. vv 5 ee etek eects ae 273 
High valley oases... .... 4.60 sos oe 301, ffs 
of the Zeraishan suc. acc sme eee 311-313 
Hindu-Kisie ovis eats ere einen tere 251 
Hep partots. a. tdci wil aera 395, 397, 422, 424 
Hissar, ancient route frome. aac. cre eres 310 
Gitadel Of 024 Ue ee a 316, ff., 320* 
{NOUNEAITIS ©...) toe eee ee 272, 2746 
Hissar Valley, preservation ofkurgansinthe. 306 
physiograpity, Ola, whe as eee 270-274 
Hodja Mussaii Ashar}... i050>503 <1: eee 314 
Hommel F 5 ige he ee eee 351 
Homo Primigentus ne oe ses odaie sg cine 454 
Hordeum distichum, chaff of, in pottery of 
J Gat- 5 la! Arena crareten RA inspira nr 472 
Horse of Anau, Equus caballus pumpellir 
Diterst’s Si, skaters cee arene 387-397 
tables of measurements comparing with 
other subfossil equids, pre- 
molars and molars... 387 
dental indices. 5 2 heat 388 
JAWS F506 fo 2 Fees eo ee 390 
indices of metacarpus tertius.......... 391 
Scapiilacsites clots cage: tetas trans 391 
humerus, radius, and metacarpi....... 392 
fenivr aid tibia h ata sa, yenlace oo 393 
metatarsi and phalanx Iand II........ 394 
phalasux IT], astragn lis. 2 ooh cas anee 395 
type and-relations of cic. caucuses ee 396 
meta tarsus tertulus a sacs es aware ea ec 396 
height of withers sian sheers tee 396, 397 
characteristics of Anau horse summar- 
TZOO a teh ee ete teens 397 
Horse of the Quaternary period of Europe.. 402 
prehistoric, Giese. vive es = heen cee 1 4038 
the neolithieiager tween. ee aneriate 403 
