Adjective:

पोलिश, गाळाचा,

alluvial मराठी अर्थाचे उदाहरण:

तापी आणि पूर्णा नदीचा भाग हा गाळाचा प्रदेश आहे.

মোহाना येथे जबरदस्त गाळाचा भाग आहे आणि म्हणूनच पाण्याची खोली उथळ आहे.

परंतु यामुळे त्यामधील समुद्राने तयार झालेला गाळाचा भाग हलका असल्याने दबण्याऐवजी उंचावला गेला, जसजसे भारतीय उपखंड अजून आत येत गेले तसतसे हा भाग अजून उंचावला व हिमालयाची निर्मिती झाली.

alluvial's Usage Examples:

It forms sheets across alluvial plains and can occur as discontinuous lines of nodular kankar or as indurated layers in stratigraphic profiles.

An alluvial fan is a fan-shaped deposit formed where a fast flowing stream flattens.

Predominately residual clay and/or silt loam soil or small to large cobble-dominated alluvial deposits.

The topography of Libon is generally characterized as plain to undulating; extensive alluvial floodplain on its eastern flank, gently rolling to sloping uplands and steep mountains on its central western parts.

At altitudes of 10–30 meters above sea level, older alluvial accretions show up as horizontal layers of brown clay, and the higher areas are dominated by red-brown laterite.

In addition the removal of the dam and accumulated alluvial sediment would be complex especially given the downstream communities and environment.

When the alluvial plain is narrow or short parallel to depositional flow, the fan shape is ultimately affected.

They are found on level and slightly sloping alluvial plains, terraces and gently sloping piedmont plains in arid, semi-arid and Mediterranean.

underwater version of alluvial fans and can vary dramatically in size, with widths from several kilometres to several thousands of kilometres The largest is.

Cambisols are developed in medium and fine-textured materials derived from a wide range of rocks, mostly in alluvial, colluvial.

alluvial flats along with asafoetida, Ephedra strobilacea, black saxaul and white saxaul.

It is navigable by small crafts up 100 kilometers from its mouth and its basin is enriched by a deep deposit of alluvial soil.

The Issyk kurgan, in south-eastern Kazakhstan, less than 20 km east from the Talgar alluvial fan, near Issyk, is a burial mound discovered in 1969.