Sediments that consist of mineral grains that were eroded from continental rocks are called

Sediments that consist of mineral grains that were eroded from continental rocks are called terrigenous.

Terrigenous sediments are significant weathering outputs of rocks revealed at the Earth’s surface. They are taken to the ocean by streams, blows, and glacier and may be redistributed in the ocean by flows. Therefore, shifts in distribution, grain size, and flux of terrigenous aquatic sediments endure hints to important paleoclimate variables such as gust pace and direction, aridity, antagonistic movement, and ocean flows.

sediment layers stop spreading when they reach a barrier or they run out of sedimentary material. lateral spreading is the movement of gently to steeply sloping, saturated soil deposits caused by earthquake-induced liquefaction. i hope this . : )