CONTENTS. XIII 
SECOND VOLUME. 
Part V. PHYSIOGRAPHY OF CENTRAL-ASIAN DESERTS AND OASES. R. WELLES PUMPELLY. 
PAGE 
See MN EL ORR Ces, fos fe Val Cue wf ubnpey a Sine Sto oe baa es cies a en me cee tgs ee tae 243-298 
PERM URORPE SA LNASITL AS ATL OF PATI WWTIOIE oo org rnc licks Sere Gicee a itn ihe oie ais a ra RIEL orc 243-250 
ase essential chatacters Of & desert Dass. ds cil se ee ois oc Me, at, thu AD Setneralaa: bi. a 243-244 
The three agencies of erosion and transportation, ice, water, and wind; and the five 
deposition zones, glacial, alluvial, lacustrian, flying sands, and loess arising 
Cherelrany cece ec ee he seid Sha cies eho a. 3s has hat wes Bench bic Anaad 244-246 
The interlapping of deposition zones effected by climatic oscillations.................. 247 
The cyclical development of an ideal desert Basin .y.<< i065 acs ye ein ending sie ane nawacees 247-250 
Be PXESDIN CR EMVO@USIN F IRICEN PTR od Sse tld alana ett 095) 12 ans ass. ad wba Spain bhcn eo Gelnnig os 251-259 
Corea LO Attit Ceres CVey PRN coe ean Se en aiete ape are dies Minas, s cane ate wie N, + acne wig A wd wa klar 251 
BRON DES LT Bae RR ie le A a Pe Oko eee en ae 251-258 
Tentative reconstruction of Quaternary sequence of events................0200.2000. 259 
Pema WhO Wa ce RAIN te a di cae oaralatG Sais ale Woes daly atv. eleseyy ov iat’ 259-264 
PCSEEANN Ere PONISI Rasa GE id ys Spf S ge Nd en 5 os» 91) 6A ache Bes TV, Fale on 8 Rees 259-261 
Glaciology and evidences of mountain movement... «2.2.2... 652 cneseecn cree cedtenaes 261-264 
A tentative reconstruction of events in the Alai Valley... . 2.2.0... 0500. s cece e een ees 264 
SO eae aD ed Ne Fe ae re er es Wa 8 ra Fes Zoi Hate SA Glope eae 4 eA eed wien caine ES 265-274 
ep ee eure SON BI EAL BAZIN ON alien ile gals nol spe ed ohess tage oy Wid os wossaeie Be wien Se 265-269 
Cie RT es CEN ESISMO SVB cc aa eal oc ayauwminiale ania a sla,a'e Hiaienwid p omtierdaces & ai, < 270-274 
Tentative reconstruction of erosion cycles in Karategin and Hissar................... 274 
OMT Ce UR CAN ING Fe ee cee fins mild yi) 2h DS Gua even ge sanamar ica updsSebnease Gears ae apelnes 275-282 
Ore MEMS es WSS MTSE CUINAL VAIOW. o05 <5 65 one via aici ad no, aptaPnis nMelesnioan Hida. btses ncrlis beelhs 3 276 
eM Reem OS Ble Wr eo 7. in Sates NR Len Ga. > al steuav Scud ka. stun Sure be Oho 257 
eae NG Mer eee ae sii o.oo Cie a van Cini > oie x sug aasba Sua puel Rbia a Sanh Oe, aumloe oe i 
NN RN tN eA ee Re ake Bs SC oie 25h nak OLE ANG Ov Fie Gei69 Hpw WALA de win eie ais 277 
TES TTS Fe EIS SR 2) ee ee ee ea Pee een re eee 278-279 
OVERS PISCE MAIC IR RCL O oh oes Oe AN vc Gon im ore Cink WS, A bha ite poms xtnaiido Aad pice ohm nam, Ria aamla ce 279-282 
ESE SPEER RE CU 6 Sg ieee SA OER SE a ee ee a ar er ae 282-286 
ee IPL Ot, DOTAUNIMT EL SIPMULES eT Oe tenons sx e'e ale cits ase as 6 ha wh a ania eons HF HAE eR eas 282-283 
The uptilted piedmonts of northwestern Tarim as a key to the past.................. 283-286 
Be OTE ES SE LOC CCRT, LO) ORCL CLG ooo. oi in acvon le Seite dow 98, pans casos tun, min Budell Rm «8 gin ars 286 
dentative reconstruction o& the prst int Tarim... 5 «© sey wiv. 3.0, dais Wi toe a eee as © Waele ew e's 286 
SEaeRE OT Pics AIS oe et e's Gola kr vaio Sina als @eed boop 8°07 2 Od, Wo Al aypine wh otis 0 Slatmpi eels WA leit Oe SM 287-290 
DS eR RIN UELINGE By te ce eet wie ni aa eg, anak sb. in id am mele are wiaitiv nh Galore aap Sass 287 
Alar erosion eycles based on the, Taldie profiles. 5c eiac 0 dec cisveien ode Sawa Raw's ops bes 287 
RVR e rE: LOO) L1A0Y CoAaeh sis 5 a gaat tae sieht tists Soin AI Ws ee inlay wide ve w eee 4k oe 287-289 
PsP CMMMOPIOTOItOUs OF CHE PiIAIOs tain, be ci eres em Oi eae awe os Pky ys aah oS 289 
Presentasciliation i the dendsition: 2Ones 4. Gear co ties shades cele won nk SB Brei ewe Snes 290 
Reconstruction of past events of the Fergana Basin...........-.--0cee cece esc eesces 290 
PIAS RIGA SS piAth AST: cutie -eiccipiae sin aes «apne Oe eer Ge see 64 Sas ve Salo v eon bees 291-298 
Complications and functional peculiarities arising from shape and size................ 291-292 
The lacustrian zone (Aralo-Caspian Sea expansions).............0. cece eee e cece ees 292-294 
Recent developments in the alluvial and the flying-sands zones.................00055 294-295 
ieecent cuanges.in the course of thie Oxuss 64 oc ane ie wire gos leh ens mss a8 ie ee 295-297 
Tentative reconstruction of the past in the Aralo-Caspian Basin..................... 298 
UTA PTH ROG VEO ASHS eee nee he eave te stent ake: Ce relts Neg Spa Re eee PE AI AIICEG cotter shetebane“e eb) Suskorly “ot @ 299-337 
ie ones Ge a PeOIOPICal PrODlelt, 7s oss or ese oe ieee elle elves Be tin Fide hws ERR Ea ee 299-307 
Man as a geologic factor of excavation, transportation and deposition, and a director of 
mlltivial depositiong, |. 2sciawie ne see doce ss iectew en Wee 9 wie's vinld’s vx Agents 299-301 
