| 0030 |
[Figure]
1 |
アナウの堀のある古墳の断面Section of the Trenched Tumulus at Anau.
|
| 0030 |
[Photo]
2 |
アナウ古墳の堀The Trench in the Anau Tumulus.
|
| 0030 |
[Photo]
3 |
アナウ古墳内の大槌The Maul in the Anau Tumulus.
|
| 0031 |
[Photo]
PL. 1 |
アナウ古墳から出土した装飾のある焼き物 平地から約10フィートの高さにある堀の底の内側から撮影 1903年DECORATED POTTERY FROM THE ANAU TUMULUS. TAKEN FROM THE SIDES AT BOTTOM OF TRENCH ABOUT 10 FEET ABOVE LEVEL OF PLAIN, 1903.
|
| 0033 |
[Photo]
4 |
アナウ古墳にある小さなマッフル形の物体の断面Section through a small Muffle-shaped bject in the Anau Tumulus.
|
| 0034 |
[Photo]
5 |
アナウ古墳の土壁の残骸Remains of Earthen Wall in the Anau Tumulus.
|
| 0035 |
[Photo]
6 |
ギヤウル・カラにある占領の残骸が堆積した高原Plateau of Accumulated Debris of Occupation in Ghiaur Kala.
|
| 0036 |
[Photo]
7 |
Paikent 砂に埋没した都市Paikent, a Sand-buried City.
|
| 0037 |
[Photo]
8 |
中世サマルカンドのモスクA mosque of Mediæval Samarkand.
|
| 0038 |
[Photo]
9 |
古代サマルカンドのCulture ~ationsにおける貯水システムWater Pool System in the Culture ~ations of Ancient Samarkand.
|
| 0050 |
[Figure]
10 |
ボスポラス海峡を横断する高地の略図 コンスタンチノープル北部のロバート・カレッジから東向きSketch of the Uplands across the Bosporus, looking eastward from near Robert College, north of Constantinople.
|
| 0050 |
[Figure]
11 |
黒海側の出口から見たボスポラス海峡の鳥瞰図Bird's-eye Diagram of Bosporus at its exit from the Black Sea.
|
| 0051 |
[Figure]
12 |
岬（Headland）と海角（Foreland）のスケッチ サムスン西部 黒海南岸 西向きSketch of Headland and Foreland, west of Samsun, south coast of Black Sea, looking west.
|
| 0051 |
[Figure]
13 |
トレビゾンド東部の高い海岸線の側面 黒海南岸 東向きProfile of Elevated Shorelines east of Trebizonde, south coast of Black Sea, looking East.
|
| 0052 |
[Figure]
14 |
トレビゾンド付近の砂利の出現を描いた図Diagram to illustrate the occurrence of gravels near Trebizonde.
|
| 0053 |
[Figure]
15 |
バク南西地方の略地図Sketch Map of te District southwest of Baku.
|
| 0054 |
[Photo]
16 |
カスピ海の古い海岸線 バク近郊An old Caspian Shoreline, near Baku.
|
| 0055 |
[Figure]
17 |
3マイルにわたる尾根の断面 バクの北西6マイル 北向きThree-mile section of Ridge, six miles northeast of Baku, looking north.
|
| 0055 |
[Photo]
18 |
ビビエイバトの油井 バクの南2マイル 北向きThe Oil-Wells of Bibi-Eibat, two miles south of Baku, looking south.
|
| 0056 |
[Photo]
19 |
Zuyk近郊の尾根にあるトンボロ（陸繋砂洲、Cobble Spit） バクの北東7マイル 北向き；最前面は亀裂の入ったアラロ－カスピアン地層（Aralo-Caspian Strata）A Cobble Spit on a ridge near Zuyk, seven miles northeast of Baku, looking north; fissured Aralo-Caspian Strata in the foreground.
|
| 0058 |
[Figure]
20 |
クラズノボーツク周囲の地区の略地図と区域Rough sketch Map and Sections of the District about Krasnovodsk.
|
| 0059 |
[Photo]
21 |
バルカン山脈にあるカスピ海の隆起した海岸線 中央アジア鉄道のジェベル駅近郊An Elevated Caspian Shoreline in the Balkhan Mountains, near Jebel Station, Central Asiatic Railway.
|
| 0066 |
[Photo]
22 |
コペトダク山脈の麓にある切り開かれた段丘 キジル-アルバト南部 南向き 左側にある山の水平な石灰岩層は、中央にある段丘の粘土層の下を通るように突然湾曲しているDissected Terraces at the base of the Kopet Dagh, south of the Kizil-Arvat, looking southwest. The horizontal limestones of the Mountain on the left are suddenly bent down so as to pass under the clays of the Terraces in the middle distance.
|
| 0067 |
[Photo]
23 |
バハルデン近郊の砂丘 南向きSand-hills near Bakharden, looking south.
|
| 0068 |
[Photo]
24 |
バハルデン近郊のバルハン 南向きA Barkhan near Bakharden, looking south.
|
| 0069 |
[Photo]
25 |
キジル－アルバト近郊にあるトルコマンKibitkasの村A Village of Turkoman Kibitkas, near Kizil-Arvat.
|
| 0070 |
[Figure]
26 |
コペトダクの地質学的概略図 アシハバードの南西Geological Outline Map of the Kopet Dagh, southwest of Askhabad.
|
| 0073 |
[Figure]
27 |
セラニ渓谷の段丘 北西向きTerraces in the Serani Valley, looking northwest.
|
| 0075 |
[Figure]
28 |
ナマリの段丘の側面2マイル 東向きTwo-mile profile Terraces at Namali, looking east.
|
| 0075 |
[Figure]
29 |
シンクリナル渓谷の断面2マイル ナマリの南東Two-mile section of Synclinal Valley, southeast of Namali.
|
| 0076 |
[Figure]
30 |
Duruigar渓谷の段丘の側面2マイル 東向きTwo-mile profile of Terraces in the Duruigar Valley, looking east.
|
| 0077 |
[Figure]
31 |
段丘開発計画Scheme of Terrace Development.
|
| 0080 |
[Photo]
32 |
ギヤウル・カラの中央の塚 60～80フィートの高さ オールド・メルブ 北向きThe Central Mound of Ghaiur Kala, from 60 to 80 feet high, in Old Merv, looking north.
|
| 0081 |
[Photo]
33 |
チャルジュイ南部の砂丘 北西向きSand Dunes south of Charjui, looking northwest.
|
| 0083 |
[Figure]
34 |
鉄道の切り通しの図 ジザク南部Diagram of Railroad Cut, south of Jizak.
|
| 0086 |
[Figure]
35 |
黄砂の流れの図 カラブラク近郊 南向きDiagram of Loess Drifts, near Kara-bulak, looking south.
|
| 0089 |
[Photo]
36 |
カンバルアリ（Kambar-Ali） クガルト（Kugart）のミンバシ（Min-Bashi）Kambar-Ali, the Min-Bashi of Kugart.
|
| 0090 |
[Photo]
37 |
クガルト（Kugart）のミンバシ（Min-Bashi）とその召使いThe Min-Bashi of Kugart and his Men.
|
| 0091 |
[Photo]
38 |
Kuve-Gen-Shigai-ef 彼の年若い妻と子供たち そして我々のボス、Ma'raimKuve-Gen-Shigai-ef, his Younger Wife and Children, and our Head Man, Ma'raim.
|
| 0092 |
[Photo]
39 |
Kuve-Gen-Shigai-efとその召使い数人 ソンクルのアクタシュでKuve-Gen-Shigai-ef and some of his Men at Akh Tash, Son Kul.
|
| 0097 |
[Figure]
40 |
扁平なBural-bas-tau 南東向きThe Flat-Topped Bural-bas-tau, looking Southeast.
|
| 0097 |
[Figure]
41 |
扁平なBural-bas-tau 南向きThe Flat-Topped Bural-bas-tau, looking South.
|
| 0099 |
[Figure]
42 |
アレクサンダー山脈の遠くの側面 西向きDistant Profile of the Alexander Range, looking west.
|
| 0099 |
[Figure]
43 |
山脈の略地図 イシククルの南西Rough sketch Map of the Ranges southwest of Issik Kul.
|
| 0100 |
[Figure]
44 |
山脈CからDの典型的な断面 図43 東向きIdeal Section from Range C to D, Figure 43, looking east.
|
| 0101 |
[Photo]
45 |
Vyernyiとセミパラチンスクを結ぶ駅馬車街道にある駅のTarentassA Tarentass at a Station on the Post-road between Vyernyi and Semipalatinsk.
|
| 0101 |
[Figure]
46 |
Dsungarianアラタウの概略 南向きRough outline of the Dsungarian Ala-tau, looking south.
|
| 0102 |
[Figure]
47 |
Abukumof駅近郊の山脈の略図 南向きRough Sketch of a Range near Abukumof Station looking south.
|
| 0103 |
[Photo]
48 |
Sergiopol北部のうねるステップ（大草原） セミパラチンスクThe Rolling Steppe north of Sergiopol, Semipalatinsk.
|
| 0108 |
[Photo]
49 |
Kok-tal山脈のKum-ashu峠から見たChalai山脈 北向き；暗い突出部（dark spur)の背後にある巨大な古い氷堆積が左に進む Chalai山脈の山頂は雲でぼやけているThe Chalai Range from Kum-ashu Pass in the Kok-tal Range, looking north; a large old Moraine advances to the left, behind the dark spur. The crest of the Chalai Range is dimmed by clouds.
|
| 0109 |
[Figure]
50 |
トゥルク渓谷の氷堆積 西向きMoraine in the Tuluk Valley, looking west.
|
| 0110 |
[Photo]
51 |
Chalai山脈の古い氷堆積内にある若い氷堆積 北向きA young Moraine within the Old Moraine in the Chalai Range, looking north.
|
| 0112 |
[Photo]
52 |
クンゲイ・アラタウのSutto-bulak峠の下の雪原 南西向き；背景にあるのは圏谷Snowfield below Sutto-bulak Pass in the Kungei Ala-tau, looking southwest; a Cirque in the background.
|
| 0114 |
[Figure]
53 |
平均的な渓谷の先端にある圏谷の側面Profile of a Cirque at the Head of a normal Valley.
|
| 0114 |
[Figure]
54 |
Kalkagar-tauの圏谷Cirque in the Kalkagar-tau.
|
| 0115 |
[Figure]
55 |
Kalkagar-tauの圏谷Cirques in the Kalkagar-tau
|
| 0115 |
[Figure]
56 |
Sutto-bulak峠近郊の圏谷 クンゲイ・アラタウCirque near Sutto-bulak Pass, Kungei Ala-tau.
|
| 0116 |
[Figure]
57 |
ナリン地層の全体的な断面 東向きGeneral Cross-section of the Narin Formation, looking east.
|
| 0117 |
[Figure]
58 |
ナリン地層の小規模な単斜 東向きA small Monocline in the Narin Formation, looking east.
|
| 0117 |
[Figure]
59 |
Ulu-tuz峡谷を貫く3マイルの断面 東向きThree-mile section through Ulu-tuz Gorge, looking east.
|
| 0118 |
[Photo]
60 |
Alabuga渓谷 北向き ナリン地層の切り開かれた背斜の尾根の向こうにChaar Tash山脈の東端が見える；ypseousの花が背斜の尾根にある峡谷の壁面を水平方向に白く染めている 最前面にあるのはキルギスの墓The Alabuga Valley, looking north. The east end of the Chaar Tash Range is seen over the dissected anticlinal ridge of the Narin formation; gypseous efflorescence whitens the transverse gorge walls in the anticlinal ridge. Kirghiz Tombs in the foreground.
|
| 0119 |
[Figure]
61 |
ナリン地層の北側の縁を横切る4マイルの断面 東向きFour-mile section across the northern border of the Narin formation, looking east.
|
| 0120 |
[Figure]
62 |
Kach-kar盆地を横切る15マイルの断面 東向きFifteen-mile section across the Kach-kar Basin, looking east.
|
| 0122 |
[Photo]
63 |
（西）クガルト（Kugart）の段丘 北東向きTerraces of the (western) Kugart, looking northeast.
|
| 0123 |
[Figure]
64 |
（西）クガルト（Kugart）渓谷を横切る3マイルの断面 北東向きThree-mile section across the (western) Kugart Valley, looking northeast.
|
| 0123 |
[Photo]
65 |
（西）クガルト（Kugart）の峡谷 タラン・バザールの上 東向きGorge of the (western) Kugart, above Taran Bazaar, looking east.
|
| 0124 |
[Figure]
66 |
（西）クガルト（Kugart）渓谷にある峡谷の1マイルの断面 北東向きOne-mile section of Gorge in the (western) Kugart Valley, looking northeast.
|
| 0124 |
[Photo]
67 |
キルギス橋近郊にある（東）クガルト（Kugart）の上部の段丘 南西向き 背景は、傾いた古い礫岩の切り開かれた丘と突出部（spurs）Upper Terrace of the (eastern) Kugart, near the Kirghiz Bridge, looking southwest. Dissected hills and spurs of tilted older conglomerates in the background.
|
| 0125 |
[Photo]
68 |
（東）クガルト（Kugart）の段丘にある砂利の断崖 南向き 中央には礫岩の突出部（spurs）；後方にはフェルガナ山脈Gravel Bluff in the Terraces of the (eastern) Kugart, looking south. Spurs of conglomerate in the middle distance; the Fergana Range in the background.
|
| 0126 |
[Figure]
69 |
（東）クガルト（Kugart）渓谷の地滑りの10マイルの断面 北東向き 現在の川谷は砂利層が浸食されて水平になっており、これより古くて幅の広い、浸食されて傾斜した礫岩層が渓谷をふさいでいるTen-mile section of a Landslide in the (eastern) Kugart Valley, looking northeast. The present river valley is eroded in horizontal gravels that occupy an older and much wider valley eroded in tilted conglomerates.
|
| 0126 |
[Figure]
70 |
Alabuga渓谷にある段丘の2マイルの断面 東向きTwo-mile section of Terraces in Alabuga Valley, looking east.
|
| 0127 |
[Figure]
71 |
Alabuga川とナリン川の接合部にある段丘の3マイルの断面 東向きThree-mile section of Terraces at the junction of the Alabuga and Narin Rivers, looking east.
|
| 0128 |
[Figure]
72 |
段丘の典型的な断面Ideal section of Terraces.
|
| 0132 |
[Photo]
73 |
イシククルの東端にある平原の沈水した渓谷 北東向きA Drowned Valley in the Plain at the east end of Issik Kul, looking northeast.
|
| 0133 |
[Figure]
74 |
イシククル湖の北西の端(A) 中央(B) 北東の端の汀線 2ベルスタのロシア地図が18ベルスタ～1インチに縮小したShorelines of Issik Kul at the northwest end (A), the middle (B), and the northeast end (C) of the lake, reduced to 18 versts to an inch from the 2-verst Russian map.
|
| 0134 |
[Figure]
75 |
渓谷、隆起した海岸、そして現在のイシククルの汀線の関係図Diagram of the relation of a Valley, the raised Beaches, and the present Shoreline of Issik Kul.
|
| 0135 |
[Figure]
76 |
ある花崗岩の岬上のイシククルの汀線の概略 西向きProfile of the Issik Kul shorelines on a granitic headland, looking west.
|
| 0136 |
[Figure]
77 |
周りを囲まれた湖での傾斜効果；右側に隆起Effect of tilting on an inclosed lake; uplift on the right.
|
| 0136 |
[Figure]
78 |
周りを囲まれた湖での傾斜効果；左側に隆起Effect of tilting on an inclosed lake; uplift on the left.
|
| 0138 |
[Figure]
79 |
ソンクル湖近郊のストーン・サークル サークル間の距離はフィートで図の右に表示されているStone Circles near Lake Son Kul. The distance in feet between the circles is indicated in figures on the right.
|
| 0140 |
[Photo]
80 |
イシククルの東端の平原にあるCarvecストーン 南向きA Carvec Stone on the plain at the east end of Issik Kul, looking south.
|
| 0147 |
[Figure]
81 |
フェルガナのスケルトン（Skeleton）地図A Skeleton Map of Fergana.
|
| 0148 |
[Figure]
82 |
パミール地図 スヴェン・ヘディンの地図から取るMap of the Pamir, taken from Sven Hedin's Map.
|
| 0149 |
[Photo]
83 |
アライ渓谷に向かうキルギス・キャラバンA Kirghiz Caravan on its way to the Alai Valley.
|
| 0149 |
[Photo]
84 |
タルディック渓谷のポプラの木A Poplar Tree in the Taldic Valley.
|
| 0150 |
[Photo]
85 |
Ak-Busa-Gaの大平原への入り口でタルディック渓谷を見上げるLooking up the Taldic Valley at the Entrance to the Broad Plain of Ak-Busa-Ga.
|
| 0151 |
[Photo]
86 |
Ak-Busa-GaAk-Busa-Ga.
|
| 0151 |
[Photo]
87 |
アライ渓谷の向こう のトランス-アライ山脈を望む Sari Tash北部の頂上から撮影Looking across the Alai Valley to the Trans-Alai Mountains. Taken from a peak north of Sari Tash.
|
| 0152 |
[Photo]
88 |
アライ渓谷のキルギスThe Kirghiz in the Alai Valley.
|
| 0154 |
[Photo]
89 |
Uy Bulak峠からカラクルを見下ろすLooking down the Kara Kul from Uy Bulak pass.
|
| 0155 |
[Photo]
90 |
圧縮された花崗岩の巨礫Deflated bowlder of granite.
|
| 0155 |
[Photo]
91 |
圧縮された花崗岩の巨礫 東向きのくぼんだ側 午前10:30に撮影Deflated bowlder of granite, hollowed side facing east. Taken at 10.30 a.m.
|
| 0155 |
[Photo]
92 |
斜面に囲まれた結晶質石灰岩の塊A talus-shrouded mass of crystalline limestone.
|
| 0155 |
[Photo]
93 |
気温の変化により亀裂が入った氷河期の結晶質石灰岩の巨礫A glacial bowlder crystalline limestone cracking from the changes of temperature.
|
| 0156 |
[Photo]
94 |
一般的な風化した巨礫 周りに散らばっている軽量の破片はもともとは塊だったCommon type of weathered bowlders. The light fragments strewn about it are parts of the former mass.
|
| 0157 |
[Photo]
95 |
氷堆積にあるkettle-hole湖はKurumdi Massからアライ渓谷にかけて横に広がっている トランス-アライ山脈は雲間にそびえているA kettle-hole Lake on the Moraine extending from the Kurumdi Mass transversely into the Alai Valley. The Trans-Alai Mountains rising into the clouds.
|
| 0158 |
[Figure]
96 |
氷堆積を横断するアライ渓谷の断面Section of Alai Valley Transverse Moraine.
|
| 0158 |
[Figure]
97 |
“2つ谷がある”渓谷の典型的な断面Ideal section of a "twice-troughed" valley.
|
| 0159 |
[Figure]
98 |
Bor Dabaのキジル－アルト渓谷を横断する断面 北向きSection across Kizil-Art Valley at Bor Daba, looking north.
|
| 0160 |
[Figure]
99 |
キジル－アルト渓谷の氷堆積と段丘の概略Profile to show moraines and terraces of the Kizil-Art Valley.
|
| 0164 |
[Photo]
100 |
カラクルの北部半島 図の右半分の下部にある白い物は塩、恐らくCaSO4The Northern Peninsula of Kara Kul. The white of the lower portion of the right half of the illustration is salt, probably CaSO4.
|
| 0165 |
[Figure]
101 |
カラクル盆地の東西の断面An east-west section of the Kara Kul Basin.
|
| 0165 |
[Figure]
102 |
湖の上およそ100フィートの小丘の断崖でむき出しのカラクル堆積物の断面Section of Kara Kul sediments exposed in Hillock Bluff about 100 feet above Lake.
|
| 0166 |
[Photo]
103 |
カラクル盆地の氷堆積 これより古い氷堆積上で北西向き 右側の遠くには上に重なった氷堆積が見えるMoraine of the Kara Kul Basin, looking northwest on the Older Moraine. An overriding Moraine seen in the distance on the right.
|
| 0167 |
[Photo]
104 |
上に重なった氷堆積により押し上げられた堆積物Sediment pushed up by an overriding Moraine.
|
| 0167 |
[Photo]
105 |
上に重なった氷堆積により押し上げられた堆積物Sediment pushed up by an overriding Moraine.
|
| 0167 |
[Photo]
106 |
湖の100フィート以上の高さで、氷体積の上に凝固しながら成長した硫酸カルシウムConcretionary growths of Calcium Sulphate on Moraine more than 100 feet above Lake.
|
| 0168 |
[Photo]
107 |
カラジルガ氷堆積の前からキジルクル・ステップ（大草原）まで北を見るLooking north from the front of the Kara Jilga Moraine to the Kizil Kul Steppe.
|
| 0169 |
[Photo]
108 |
キジル－アルトのやや西に向いており、キジルクル・ステップ（大草原）に接合する渓谷The valley heading a little west of Kizil-Art and joining the Kizil Kul Steppe.
|
| 0170 |
[Photo]
109 |
北部半島の西側にある沈水した渓谷 トランス-アライ山脈方面に北向きDrowned Valleys on the west side of the North Peninsula. Looking north to the Trans-Alai range.
|
| 0173 |
[Figure]
110 |
Sari Tash渓谷の北側に面する断面Section looking north up the Sari Tash Valley.
|
| 0174 |
[Photo]
111 |
Katin-Art峠のおよそ5ベルスタ下から見たSari Tash渓谷の西側The eastern side of the Sari Tash Valley from about 5 versts below Katin-Art Pass.
|
| 0174 |
[Photo]
112 |
下盤Aの断片 Taldic峠のすぐ下から見下ろしたものRemnants of Floor A, as seen looking down from just below Taldic Pass.
|
| 0175 |
[Photo]
113 |
Taldic渓谷の段丘 下盤BからTaldic渓谷を見上げたもの グルチャ上部およそ63ベルスタ 下盤Aは右側の上部にあるTaldic Valley Terraces, looking up the Taldic Valley from Floor B, about 63 versts above Gulcha. Floor A is high up on the right.
|
| 0175 |
[Photo]
114 |
Taldic渓谷の段丘 下盤CからTaldic渓谷を見上げたもの グルチャ上部およそ46ベルスタTaldic Valley Terraces, looking up the Taldic Valley from Floor C, about 46 versts above Gulcha.
|
| 0176 |
[Figure]
115 |
Ak-Busa-Ga草原と流水溝の地図Map of the Ak-Busa-Ga grass plain and stream channels.
|
| 0177 |
[Figure]
PL. A |
OSHからカラクルにかけての渓谷の段丘と氷堆積の概略PROFILE OF VALLEY TERRACES AND MORAINES FROM OSH TO KARA KUL.
|
| 0180 |
[Figure]
116 |
Langar Gulliesの傾斜が二重に変化したことを示す断面Section to show double change of slope in Langar Gullies.
|
| 0180 |
[Figure]
117 |
途中の断面 Langarの北20ベルスタ 西から15°南を向く 傾斜の荒れ地が、より最近の荒れ地の下に傾斜しているSection en route, 20 versts north of Langar, looking 15°south of west. The tilted waste inclines under the later waste.
|
| 0182 |
[Figure]
118 |
説明図 例えば草原にある荒れ地の展望の相対的な古さを測定するExplanatory diagram for example in determining relative antiquity of horizons of the waste on the plains.
|
| 0183 |
[Photo]
119 |
アライ山頂南部の鋭い山頂 Katin-Art峠から西に数ベルスタの頂上から撮影The sharp peaks south of Alai Crest. Taken from a peak some versts east of Katin-Art Pass.
|
| 0190 |
[Figure]
120 |
中央トルキスタンの略地図Sketch map of Central Turkestan.
|
| 0191 |
[Figure]
121 |
略地図 図120の位置を示すSketch map, showing location of Figure 120.
|
| 0193 |
[Photo]
122 |
Shor Kul西部のSugun渓谷にある石灰岩のひだ 西向きFolds in the Limestone in the Sugun Valley west of Shor Kul, looking west.
|
| 0194 |
[Photo]
123 |
カシュガル西部 Kan Su近郊の桃色砂岩の下半分にある波紋Ripple-marks on the lower half of the pink sandstone near Kan Su, west of Kashgar.
|
| 0202 |
[Figure]
124 |
イシククルの南西からカシュガル盆地にかけての天山山脈の断面 過高感=7 陰影なしの概略が実際の規模で描かれている 地層に付けられた番号はp.162図Iを参照Cross-section of the Tian Shan Plateau from Issik Kul southwest to the Kashgar Basin. Vertical exaggeration= 7. The unshaded profile is drawn on the true scale. The numbers attached to formations refer to Table I, p. 162.
|
| 0203 |
[Photo]
125 |
Yak_Tash盆地の光景 天山山脈の北部にある 北西向き 最前面の盆地底は、多数の池がある平らな氷堆積で覆われている；その向こうには頂上が平坦な山々と氷河の渓谷があるScene in the Yak_Tash_Basin, in the northern part of the Tian Shan plateau, looking northwest. In the foreground the basin-floor is covered with a flat moraine holding numerous ponds; beyond are smooth-topped mountains cut by glacial valleys.
|
| 0205 |
[Photo]
126 |
カシュガル市西部のカシュガル盆地の端にある第三層の光景 ここの地層は、観測者の背後にある盆地から北西に傾いている 左手には古い勾配の平原が一部見えているが、恐らく氷河期初期にできたことを表しているView of the Tertiary strata on the edge of the Kashgar Basin west of Kashgar City. The layers here dip northwest away from the basin, which lies behind he observer. On the left several portions of an old grade plain probably represent the work of an early glacial epoch.
|
| 0206 |
[Photo]
127 |
クジルオイ盆地の南側に急な断層があり、その前には滑らかなシルトが堆積しているFault scarp on the southern side of the Kuzzil Oi Basin, with a smooth deposit of silt lying in front of it.
|
| 0207 |
[Figure]
128 |
クジルオイ盆地とミンヨル盆地の流域Drainage of the Kuzzil Oi and Min Yol basins.
|
| 0209 |
[Photo]
129 |
Ispairan峡谷の下位部 ここからアライ山脈からフェルガナ盆地まで北方向にかけて流れの幅が広がっている 渓谷は砂利でいっぱいで、流れが段丘を横切っているGorge of the Ispairan in its lower portion, where it begins to widen as it flows northward from the Alai Mountains to the Fergana Basin. The valley is filled with gravel, in which the stream has cut terraces.
|
| 0210 |
[Photo]
130 |
Kichikアライ西部の石灰岩の峡谷、アライ山脈の北側でIspairan川に出会う 峡谷の上部は、恐らく氷河によって広げられており、底部にある細長いシルトは氷河期後に削り取られたことを示す 中心の渓谷は、写真が撮られた側から見ると、明らかに氷河によって作られたもので、横側の渓谷は主流と関係があるに違いないLimestone Gorge of the Western Kichik Alai, where it enters the Ispairan River on the north side of the Alai Mountains. Probably the upper portion of the gorge was widened by a glacier, and the narrow slit at the bottom represents post-glacial cutting. The main valley, from the side of which the photograph was taken, is clearly of glacial origin, and the side valley must have borne a hanging relation to that of the master stream.
|
| 0217 |
[Figure]
131 |
Khoja IshkenまたはKok Su渓谷の縦断面Longitudinal section of the Khoja Ishken or Kok Su Valley.
|
| 0218 |
[Photo]
132 |
Khoja Ishkenで最も新しい峡谷、メインの氷河渓谷の底に切り込んでいる メインの氷河渓谷の急勾配の側面がはっきりと右側に見えるYoungest Gorge of the Khoja Ishken, cut in the Bottom of the Main Glacial Valley. The over-steepened sides of the latter show clearly on the right.
|
| 0219 |
[Photo]
133 |
大理石の巨礫、ならびに第4Khoja Ishken氷河と関係のある峡谷の始点Marble Bowlders, and beginning of the Gorge associated with the fourth Khoja Ishken Glacier.
|
| 0220 |
[Figure]
134 |
Khoja Ishken渓谷の断面 3つの峡谷の形状と相対的な大きさを示す 計測ではなく、観測から割り出した、円は氷堆積を示す 薄い斜線の部分は、渓谷のそれぞれの部分が凍りで覆われていた頃以来、浸食された量を示すCross-sections of the Khoja Ishken Valley, to show the shape and relative size of the three gorges. Drawn from the observation, without measurement . The circles indicate moraines. The lightly shaded portions indicate the amount of erosion since the respective parts of the valley were filled with ice.
|
| 0220 |
[Figure]
135 |
Khoja Ishken渓谷の3つの峡谷の断面 渓谷の拡大と浸食の量を示す 個々のケースは流水と浸食の力に関係している 実際の大きさは参照していないCross-sections of the three gorges of the Khoja Ishken Valley, to show the amount of widening and erosion of the valley in each case relative to the power of the stream and of erosion without reference to the actual size.
|
| 0221 |
[Figure]
136 |
略地図はMudirum氷堆積の位置を示しているSketch map showing the location of the Mudirum Moraines.
|
| 0224 |
[Figure]
137 |
Kan Su渓谷の断面 標高11,000フィートCross-section of the Kan Su Valley at an elevation of 11, 000 feet.
|
| 0226 |
[Figure]
138 |
タカ渓谷の氷堆積の平面図Plan of the Moraines of the Taka Valley.
|
| 0227 |
[Figure]
139 |
タカ渓谷の断面 北向きCross-section of the Taka Valley, looking north.
|
| 0233 |
[Photo]
140 |
Bokharaの西の境界からKuzzil Suを見下ろした眺望 砂利で埋まった渓谷が見える この渓谷は再発掘された 最前面には4つの段丘が左手に見えるView down the Kuzzil Su on the eastern border of Bokhara, showing a gravel-filled valley which has been re-excavated. In the foreground four terraces can be seen on the left.
|
| 0234 |
[Photo]
141 |
天山山脈のChadir Kul近郊にある別のKuzzil Suの段丘と蛇行した川 標高11,000フィート これら段丘には、砂利や赤い第3紀石灰石などの層があるTerraces and Meanders of another Kuzzil Su near Chadir Kul, on the Tian Shan Plateau, at an elevation of 11, 000 feet. These terraces are cut partly in gravel and partly in red Tertiary limestone.
|
| 0235 |
[Photo]
142 |
Kan Suの段丘の壁面 カシュガル西部 傾斜した中生代の層の上には水平な砂利の層がある 左手は北側で、石炭の層が、右手は朱色の定盤がある この2つの間には、やや不整合なAが見られるTerrace wall of the Kan Su, west of Kashgar, showing horizontal gravel above tilted Mesozoic strata. On the left or north side are the coal measures; on the right are the vermilion-red beds. Between the two can be detected a slight unconformity, A.
|
| 0236 |
[Photo]
143 |
天山山脈のKok Kiya段丘 標高11,500フィート 最前面の中央にある流水は石灰岩で遮られ、単なる狭い峡谷になっている その間の砂利は、側面がひな壇状の広大な氾濫原を削っているTerraces of the Kok Kiya, on the Tian Shan Plateau, at an elevation of 11, 500 feet. In the foreground and in the middle distance the stream has been caught upon limestone and has cut merely a narrow gorge, while in the gravel between it has excavated a broad flood-plain with terraced sides.
|
| 0237 |
[Figure]
144 |
Ispairan渓谷の断面 削り取られる時期と堆積する時期が連続していたことを示すCross-section of the Ispairan Valley, showing successive periods of cutting and filling.
|
| 0239 |
[Photo]
145 |
Shor Kul 南向きShor Kul, looking south.
|
| 0242 |
[Figure]
146 |
Dungsugotの湖から山に至るShor Kul平原の南北の断面North and south section of the plain of Shor Kul from the lake to the mountains at Dungsugot.
|
| 0242 |
[Figure]
147 |
Dungsugotでシルトに入り込む渓谷の断面 解説は図146を参照Cross-section of a Valley cut in the silt at Dungsugot. For explanation see fig. 146.
|
| 0243 |
[Photo]
148 |
Dungsugotにある砂利で覆われた湖成堆積物 前の図と同じ特徴を示している 解説は図146を参照The gravel-covered lacustrine deposits at Dungsugot, illustrations the same features as the preceding diagrams. For explanation see fig. 146.
|
| 0248 |
[Figure]
PL. 4 |
イラン地図Map of Iran
|
| 0260 |
[Photo]
149 |
タバスの風車Windmills at Tabas.
|
| 0261 |
[Figure]
150 |
ペルシャの風車の横断面Horizontal section of a Persian windmill.
|
| 0261 |
[Photo]
151 |
ザヒダン近郊のMil-i-Kasimabadの廃墟 これら泥壁は少なくとも500年前のものである 南北の方向だけが今でも残っているRuins at the Mil-i-Kasimabad, near Zahidan. These mud walls are at least five hundred years old. Only those in a north-and-south direction remain standing.
|
| 0263 |
[Figure]
152 |
イランのダブル・ベイスン（double basin）の略地図Sketch map of the double basin of Iran.
|
| 0268 |
[Photo]
153 |
昔のKuchanの廃墟The ruins of Old Kuchan.
|
| 0270 |
[Figure]
154~1 |
Pul-i-KhatunのHeri Rudに沿った南北の断面 白亜紀の石灰岩North and south section along the Heri Rud at Pul-i-Khatun. Cretaceous limestone.
|
| 0270 |
[Figure]
154~2 |
Pul-i-KhatunのHeri Rudに沿った南北の断面 第3紀褐色石灰岩North and south section along the Heri Rud at Pul-i-Khatun. Tertiary brown limestone.
|
| 0270 |
[Figure]
154~3 |
Pul-i-KhatunのHeri Rudに沿った南北の断面 第3紀褐色砂岩North and south section along the Heri Rud at Pul-i-Khatun. Tertiary brown sandstone.
|
| 0270 |
[Figure]
154~4 |
Pul-i-KhatunのHeri Rudに沿った南北の断面 第3紀薄粘土石灰岩North and south section along the Heri Rud at Pul-i-Khatun. Tertiary thin clayey limestone.
|
| 0270 |
[Figure]
154~5 |
Pul-i-KhatunのHeri Rudに沿った南北の断面 第3紀軟質砂岩North and south section along the Heri Rud at Pul-i-Khatun. Tertiary soft sandstone.
|
| 0270 |
[Figure]
154~6 |
Pul-i-KhatunのHeri Rudに沿った南北の断面 第3紀不純黄色石灰岩North and south section along the Heri Rud at Pul-i-Khatun. Tertiary impure yellow limestone.
|
| 0270 |
[Figure]
154~7 |
Pul-i-KhatunのHeri Rudに沿った南北の断面 第3紀赤褐色砂岩North and south section along the Heri Rud at Pul-i-Khatun. Tertiary reddish-brown sandstone.
|
| 0270 |
[Figure]
154~8 |
Pul-i-KhatunのHeri Rudに沿った南北の断面 第3紀白色石灰岩North and south section along the Heri Rud at Pul-i-Khatun. Tertiary white limestone.
|
| 0271 |
[Figure]
155~a |
Khitayi近郊の断面 Zorabad盆地の南の境界にある 頁岩Section near Khitayi, on the southern border of the Zorabad basin. Shale.
|
| 0271 |
[Figure]
155~b |
Khitayi近郊の断面 Zorabad盆地の南の境界にある 砂岩と礫岩Section near Khitayi, on the southern border of the Zorabad basin. Sandstone and conglomerate.
|
| 0271 |
[Figure]
155~c |
Khitayi近郊の断面 Zorabad盆地の南の境界にある 湖成粘土Section near Khitayi, on the southern border of the Zorabad basin. Lacustrine clay.
|
| 0271 |
[Figure]
155~d |
Khitayi近郊の断面 Zorabad盆地の南の境界にある 新しい砂利Section near Khitayi, on the southern border of the Zorabad basin. Recent gravel.
|
| 0287 |
[Figure]
156 |
アナウ川に沿った南北の断面 アナウ断層地塊を横切る ダッシュは段丘を示すNorth and south section along the Anau Brook, across the Anau fault block. Dash lines indicate terraces.
|
| 0292 |
[Photo]
157 |
Khatayi近郊のHeri Rudの段丘 川を横切ってアフガニスタンまでの北東の眺望Terraces of the Heri Rud, near Khatayi. View northeast across the river into Afghanistan.
|
| 0293 |
[Figure]
159 |
Kogneh湖とジャム盆地の略地図Sketch-map of Kogneh Lake and the Jam Basin.
|
| 0298 |
[Photo]
159 |
Binalud Kuh山脈のややひな壇状の渓谷 Turbat-i-Haideriの北30マイル 1904年3月3日A slightly terraced Valley in the Mountains of Binalud Kuh, 30 miles north of Turbat-i-Haideri, March 3, 1904.
|
| 0299 |
[Figure]
160 |
Chahak盆地にあるハジ・フセイン・ベグの渓谷の段丘Terraces in the Valley of Haji Hussein Beg in the Chahak Basin.
|
| 0300 |
[Photo]
161 |
Bajistanの街 東向き 最前面の中央では、田畑は耕作用に段丘となっている すぐ最前面にはシルトと砂利の河成段丘があるThe Town of Bajistan, looking east. In the Middle Foreground the Fields are Terraced for Cultivation. In the immediate foreground lies a fluviatile terrace cut in silt and gravel.
|
| 0301 |
[Figure]
162 |
Bajistan盆地の北東の角にある段丘Terraces at the Northeastern Corner of the Bajistan Basin.
|
| 0310 |
[Photo]
164 |
シスタン北東の典型的な砂利砂漠の一部A Typical Portion of the Gravel Desert northeast of Sistan.
|
| 0311 |
[Photo]
165 |
Sayidあるいは“花”を棹にするアシのいかだ シスタン湿地の縁A Raft of Reeds poled by a Sayid, or "Fowler," on the Edge of the Swamp of Sistan.
|
| 0312 |
[Photo]
166 |
シスタン湖の一部 最前面はアシ原；背後には湖成平原An Arm of the Lake of Sistan. In the foreground are beds of reeds; in the background, the lacustrine plain.
|
| 0314 |
[Photo]
167 |
シスタンのヘルムンド三角州の運河 運河は雑草の橋の上で別の運河を横切っているCanals in the Delta of the Helmund at Sistan. One canal crosses the other upon a bridge of weeds.
|
| 0317 |
[Figure]
PL. 5 |
シスタン湖の北西岸に沿った様々な位置から見た湖の堆積物の断面Sections of Lake Deposits from Various Locations along the Northwestern Shore of the Lake of Sistan.
|
| 0320 |
[Figure]
168 |
Kuh-i-Khojaメサの典型的な断面 濃い斜線の部分=溶岩；薄い斜線の部分=ピンク・シルト；斜線のない部分=緑粘土Ideal cross-section of the Mesa of Kuh-i-Khoja. Heavily shaded portions= lava ; lightly shaded portions = pink silt; unshaded portions = green clay.
|
| 0323 |
[Figure]
PL. 6 |
シスタンの地図Map of Sistan
|
| 0330 |
[Figure]
169 |
シスタン湖の北西岸の湖段丘と断崖の典型的な断面Ideal Cross-section of the Lake Terraces and Bluffs of the Northwest Shore of the Lake of Sistan.
|
| 0332 |
[Photo]
170 |
Seh-Kuheh近郊の湖成断崖と最近の砂丘 北東の眺望Lacustrine Bluffs and Recent Sand-dunes near Seh-Kuheh. View to the northeast.
|
| 0333 |
[Photo]
171 |
Sabazkimの過去の海岸と湖成断崖 断崖の底部では砂丘が堆積しているAbandoned Beach and Lacustrine Bluffs at Sabazkim. At the base of the bluffs sand-dunes are accumulating.
|
| 0334 |
[Photo]
172 |
Sabazkimの昔の湖岸 西向き 湖は岸の右側にあり、潟湖は左側にあるOld Lake Beach at Sabazkim, looking West. The lake stood on the right of the beach and a lagoon on the left.
|
| 0334 |
[Figure]
173 |
Sabazkimの古い湖成岸の典型的な断面Ideal cross-section of the old Lacustrine Beach at Sabazkim.
|
| 0335 |
[Figure]
174 |
Sabazkim湾の古代の海岸の特徴を記した略地図Sketch Map of the Ancient Shore features in the Bay Sabazkim.
|