The study of Quaternary sediments of Manjra River,Near Chousala, Dist. Beed P. B. Zamarkar* A.D. Fuladi** Assistant Professor, Department of Geology, S.S.E.S.A’s Science College, Congress Nagar, Nagpur, M.S., India. Email:
[email protected] Corresponding Author: A. D. Fuladi ABSTRACT The study is based on Quaternary sediments of Manjra River, Near Chousala, District Beed. The field work is carried out near Chausala. The main objective of the field work was to observe the lithology, depositional features of sediments. Deccan trap is observed at the base of the soil and Quaternary sediments. During the fieldwork samples were collected and brought to the laboratory for investigations. The laboratory study includes, pH, sieve analysis, clay mineral analysis, and Granulometric study. The study reveals that the nature of sediments suggests the flow regime is turbulent and it is a mixture of different size sediments. But at places it shows that the flow regime is much turbulent and suddenly changed to stagnancy and represented by fine sediments. The overall observation reveals that sediments are river transported. Keywords: Quaternary sediments, Manjara River, clay minerals. I INTRODUCTION The various studies on geographical, lithological and structural mapping of a limited area and Quaternary sediments have been carried out from the upper and lower Godavari sediments by a handful of workers. This prompted the author to take up the similar studies in Manjara River. Hence, the area near Chausala was selected for the present studies. Sediment supplies from continental sources to adjoining rivers are gently influenced by climatic and tectonic variables at various spatio – temporal scales (Milliman and Meade, 1983; Vaithyanathan, et.