Journal of Geological Society of India (Online archive from Vol 1 to Vol 78)

Shampa Chakraborty ¹, Sujit K. Chakraborty ¹

Affiliations
1 B-1/202, Nirala Nagar, Lucknow 226020, IN

Abstract

A point bar about 1.83 km long on River Tista shows gravel, ranging in size from pebble to boulders shows horizontal bedded structure forming the dominant sediment type. A largely upper flow regime condition is indicated. Comparison of maps prepared at different times indicates the bar to be stable in location but undergoing only changes in shape.

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