National Institute of Informatics - Digital Silk Road Project
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Explorations in Turkestan 1903 : vol.1 |
VI
CONTENTS.
Page.
The Tian Shan Mountains—Continued.
Weather, climate, and vegetation in the Tian Shan
Development of the Tian Shan Mountains
The Bural bas-tau
The Koktal Range and the Son Kul Basin
The ranges near Issik Kul
The ranges and steppes of Semiryetshensk and Semipalatinsk
Origin of the existing ranges of the Tian Shan
The bearing of the Tian Shan ranges on the theory of horsts
Glacial records in the Tian Shan
Moraines near Son Kul
Moraines in the Tersloei Ala-tau
Moraines in the Kungei Ala-tau
Subdivision of the Glacial period
Glacial erosion in the higher ranges
The Narin Tertiary Basin...
The period of deposition
The period of deformation and erosion
The rivers and valleys of the Tian Shan
Rivers of the Issik Kul district
The Kugart terraces
The terraces of the Narin Basin
Origin of the terraces
The Issik Kul Basin
The early basin deposits
The piedmont slopes and valleys
The recent changes of Issik Kul
Relations of the river Chu to Issik Kul
Notes on archeology
Conclusion
List of references
PHYSIOGRAPHIC.OBSERVATIONS BETWEEN THE SYR DARYA AND LAKE
KARA KUL, ON THE PAMIR, IN 1903.
Description of the route
Detailed observations
In the Alai Valley
In the Kizil-Art Valley
Moraines
On the Pamir
Ancient shorelines and sediments of the Great Kara Kul Basin
Observations on the glacial geology of the Great Kara Kul Basin
The Kara J•ilga moraine
Observations in the region of Kizil Kul
Fluctuations of lake level and glacial advances explained by climatic changes
Glacial epochs
Form of the great Alai Valley
The valley itself
Side tributaries
Explanation of conditions
Observations in the Taldic Valley
Observations on the southern;border of the Fergana lowland plains
Attempt at correlation of recent geology of the mountains and plains
Miscellaneous observations on the lowland, plains.
Conclusion
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I05
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I06 I09 III
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117 I18
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