EXPLORATIONS IN TURKESTAN

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278 PHYSIOGRAPHY OF CENTRAL-ASIAN DESERTS AND OASES. THIRD EROSION CYCLE. To us the third cycle is most interesting, as it overlaps the second glacial epoch and less time has elapsed to obliterate its records. As a result of its uplift, apparently warped, the river cut down through the alluvial fillings of the second Fig. 455.-Ice-cave of the Zerafshan, Looking from within. Fig. 456.-Terraces of the Zerafshan. cycle and into the old rock bottom to a depth of from 50 feet in the lower to 300 feet in the mid-warp part of the valley with a canyon about as wide as the present and reaching about the same depth. Then the uplift appears to have stopped
PLATE 62. schrund Moraine 4 \ II ier ice I X ·//I//i t f ///////////////// /////I//////// 7-7Ty7-rr-J · ////// ..... z'/////////////////////7///7////7//////,:/7;;,/' THE ZERAFSHAN GLACIER '//^//9_ ________ Cobble Plainf/ I I MA<strong>IN</strong> VALLEY JUST BELOW THE GLACIER G Village of Tro I AT TRO I/ NEAR PACKSHIFF Vertical and horizontal scale 500 00o0 1500 2000 feet I~_L I _ AT KODISHAR ;/, AT PACHURD / //// / ABOUT THREE MILES BELOW PACHURD G AT URMITAN. TWO MILES BELOW VISIST AT MON AT M<strong>IN</strong>DONA d Samarcand Obu Siab Canal 6000ft Rice fields - Flood Plain of cobble stones AT SAAC AT SAMARCAND Rice - _-field \Vertical and horizontal scale o iooo 2000 3000 feet LEGEEND Oo° g 3__ ° Moraine Loess Alluvial conglomerates Limestone === (Unconsolidatec) stys G Slates (The Great Lower Terrace) IS referred to asthe 3rd erosion cycle Twelve Cross sections of the Zerafshan Valley.
Page 1 and 2: EXPLORATIONS IN TURKESTAN EXPEDITIO
Page 3: Ancient Anau and the Oasis-World, a
Page 6 and 7: VI CONTENTS. I'AGE. CHAPTER XV. OAS
Page 8 and 9: VIII CONTENTS. PAGE. CIIAPTER XIX.
Page 10 and 11: X LIST OF ILLUSTRATIONS. TBXT-PIGUR
Page 14 and 15: -r frR K "'I'RAN .A'i'P c'l 67 ~- -
Page 16 and 17: 244 PHYSIOGRAPHY OF CENTRAL-ASIAN D
Page 28 and 29: 2,56 PIIYSIOGRAPHY OF CENTRAL-ASIAN
Page 32 and 33: 26)0 IPIYSIOGRAI'IIY OF CENTRAL-ASI
Page 34 and 35: 262 PIIYSIOGRAPHY OF CENTRAL-ASIAN
Page 38 and 39: 266 PHYSIOGRAPHIY OF CENTRAL-ASIAN
Page 40 and 41: 268 PIIYSIOGRAPHY OF CENTRAL-ASIAN
Page 42 and 43: 270 I'IIYSIOGRAPHIY OF CENTRAL-ASIA
Page 48 and 49: 276 PIIYSIOGRAPIIY OF CENTRAL-ASIAN
Page 53 and 54: DESERTS. 279 short and the base-lev
Page 55 and 56: DESERTS. 28I The Zerafshan River is
Page 57 and 58: DESERTS. 283 The principal river wh
Page 59 and 60: DIESERTS. 285 perhaps tile unconfor
Page 61 and 62: DESERTS. 287 THE FERGANA BASIN. ITS
Page 63 and 64: DESERTS. 289 that low relief was di
Page 65 and 66: DESERTS. 291 THE ARALO-CASPIAN BASI
Page 67 and 68: - DESERTS. 293 are drowned by the p
Page 69 and 70: DESERTS. 295 ward over the Hunger S
Page 71 and 72: DESERTS. 297 Konshin believes to ha
Page 73: '1 PLATE 63 NW -
Page 76 and 77: 300 PIIYSIOGRAPIIY OF CENTRAL-ASIAN
Page 80 and 81: - .-- - _ - -- - 304 PHYSIOGRAPHY O
Page 86 and 87: 3Io PIIYSIOGRAPHIY OF CENTRAL-ASIAN
Page 93 and 94: OASES. 315 tributary delta descendi
Page 95 and 96: ut that would not detract from the
Page 97 and 98: OASES. 319 canal-way to the Djillan
Page 99: PLATE 65. r 0 x c K rv U) 0 c -r I
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322 PHYSIOGRAPHY OF CENTRAL-ASIAN D
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324 PIIYSIOGRAPIHY OF CENTRAL-ASIAN
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PLATE 67. I
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PLATE 69. e cn er NU1 rp 7 or- r- a
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326 PIIYSIOGRAPIY OF CENTRAL-ASIAN
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OASES. 335 type Ia. But the signifi
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OASES. 337 tributary canal, they bu
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CHAPTER XVI.-INTRODUCTION. The rich
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INTRODUCTION. bones, chiefly the di
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346 ANIMAL REMAINS FROM THE EXCAVAT
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PLATE 72. I-'. I-^ . ,, 't t 11; 1.
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_ _ _- 348 ANIMAL REMAINS FROM THE
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3,56 ANIMAL REMAINS FROM THE EXCAVA
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PLATE 74. 4 Poephagus grunniens and
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PLATE 76. IG. . AMedian part of car
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PLATE 78. "I I 5 FIG. 1. 11asioccip
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ORDO PERISSODACTYLA. 385 of the hea
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-- --- --- __ ORDO PERISSODACTYLA.
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ORDO PERISSODACTYLA. - 389 to that
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__ _- ORDO PERISSODACTYLA. 39I RADI
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PLATE 80. ,e f FIG,. 1. Sus critatl
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FIG. 1. Long-horned ox from NeSpal,
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PLATE 84. C) lDq F 3 0 n,, 11 "O pp
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PLATE 85. 000 0 00 ao 0o 0 0 0 0 0
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CHAPTER XIX. THE HORSE OF ANAU IN I
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FOSSIL AND SUBFOSSIL ORSES AND THEI
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CRANIOLOGICAL DIFFERENCES BETWEEN T
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PLATE 87. I 1 .:? i ; : : . . .. i
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PLATE 89. 1 2 F'l(;. 1. Nornma late
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_ _ _ _ _ ~ - 4I2 THE HORSE OF ANAU
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414 THE HORSE OF ANAU IN ITS VARIOU
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--- --- 420 THE HORSE OF ANAU IN IT
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PLATE 91. a It 1u I I s d I r ' I _
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_____ ___ __ 424 THE HORSE OF ANAU
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430 THE IHORSE OF ANAU IN ITS VARIO
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CHAPTER XX.-CONCLUDING REMARKS. We
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CONCLUDING REMARKS. 435 scanty past
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CONCLUDING REMARKS. 437 of inclosur
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CONCLUDING REMARKS. 439 The next pe
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CONCLUDING REMARKS. 441 Mesopotamia
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PART VII. DESCRIPTION OF SOME SKULL
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446 SKULLS FROM ANAU. OTHER SPECIME
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PLATE 93. C I. ; FlI. 1. Imperfect
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CHAPTER XXII. SOME HUMAN REMAINS FO
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HUMAN REMAINS FROM THE NORTH KURGAN
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PLATE 94. a 2 b . , IlG. 1. Right f
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PLATE 96. a b c 1 a -- b ~~Z a 3 D3
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- ~ : _ _ _ 466 HUMAN REMAINS FROM
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468 HUMAN REMAINS FROM THE NORTH KU
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CHAPTER XXIII. THE REMAINS OF PLANT
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REMAINS OF PLANTS FROM THE NORTH KU
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PART X. STONE IMPLEMENTS AND SKELET
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478 LARGER STONE IMPLEMENTS OF THE
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484 SKELETONS EXCAVATED IN NORTH KU
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492 SKELETONS EXCAVATED IN SOUTH KU
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494 SKELETONS EXCAVATED IN SOUTH KU
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II INDEX. PAGE. Boucher de Perthes
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IV INDEX. PAGE. Erosion cycles-Cont
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VI INDEX. PAGE. Horses, fossil, sub
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VIII INDEX. PAGE. Ox, wild (Asiatic
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x INDEX. PAGE. aksh Valley.........
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