STREAM bar deposited on the inside of a curve in the STREAM, where the water velocity is low.
A point bar is a body of sediment, often sand and/or gravel, that forms on the inside of a stream meander, where the current slows.
A low arcuate ridge of sand and gravel developed on the inside of a stream meander by accumulation of sediment as the stream channel migrates toward the outer bank.
A low ridge of sediment that forms along the inner bank of a meandering stream.
A crescent-shaped accumulation of sand and gravel deposited on the inside of a meander bend.
the area on the upstream end of a gravel bar which can contain superficial concentrations of flour gold in a thin surface layer.
A sand or gravel bar formed on the inside of a river bend.
An accreting (growing) gravel deposit on the inside of a stream bend.
Elongated, gently to moderately inclined low ridge within the stream channel built up by channelled stream flow.
An arcuate (curved or bow-shaped) ridge of sand* and gravel* developed on the inside of a growing meander (loop) in the course of a stream.
Stream bar deposit that is normally located on the inside of a channel bend.
The low, crescent-shaped deposit of sediment on the inside of a meander.
An alluvial feature that results from the deposition of sediments along the inside edge of a stream meander.
