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This paper records my geological and geomorphological observations enroute from Urumuchito Aksu. Leaving Urumuchi on August Ist, we passed through the graben trough of Davan,followed the course of Bayan Ho to Toksun in the Turfan Basin. Glaci-fluvial deposits were seen in the valley of Bayanho at 980m. above the sea. Toksun city has an elevation read from
This paper records my geological and geomorphological observations enroute from Urumuchito Aksu. Leaving Urumuchi on August Ist, we passed through the graben trough of Davan, followed the course of Bayan Ho to Toksun in the Turfan Basin. Glaci-fluvial deposits were seen in the valley of Bayanho at 980m. above the sea. Toksun city has an elevation read from