Rivers features River Systems Four types braided meandering

Rivers features

River Systems Four types, braided, meandering, anastomosing and straight

Grand Canyon, erosion

River incision in Indus Suture Zone

River types

Braided rivers • Typically developed in mountainous terrain on higher gradients. Typified by high degree of seasonality. Permanent channels with ripple crossed bedded sands develop during periods of low flow. These channels meander between sand bars that are active only during flood stage, these develop larger scale cross beds. Sediments are typically sandy and pebbly, usually moderate to well sorted, texturally moderately mature.

Braided River

Braided geometry, Matanuksa River, Alaska

Braided River, Nubra, India

Braided River, Shyok River, India

Anastomosing River, Indian foreland

Meandering Rivers Typically developed in coastal plain areas, lower gradient. More continuous flow, finer grained sediment than braided. Channel sediment is marked by the deep stream migration of meanders and the construction of cross laminated sands on point bars in the inner bends of meanders. Channels are separated by levees from flood plains that are comprised of finer grained muds and sands deposited after breach of levee during flood stage, usually vegetated. Flood stage can lead to cut-off of meanders and breakthrough of river.

Meandering Rivers, contd. Abandoned meanders become Ox-bow lakes, filled by clays. Meandering river deposits typified by finingupward stratigraphy. Sediments are typically sandy, silty and clayey. Well sorted. Sandstones form isolated channels in finer background. Ancient example- Jurassic, Brent Group of North Sea. Modern example - Brazos and Mississippi Rivers.

Meanders in the Amazon Basin

Mc. Kenzie River meanders and glacial lakes