Weathering and Erosion
Never the worse for wear
U shaped valley's
A U-shaped valley or glacial trough is formed by the process of glaciation. It has a characteristic U shape, with steep, straight sides and a flat bottom.
Picture taken at:
Location
Rocky shore line
A rocky shore is an intertidal area of seacoasts where solid rock predominates. Rocky shores are biologically rich environments, they are a useful "natural laboratory" for studying intertidal ecology. Also good for other biological processes.
Picture taken at:
Location:
Cut Bank
A cut bank, also known as a river cliff or river-cut cliff, is the outside bank of a water channel , which is continually undergoing erosion
Picture taken at:
Location:
Point Bar
A point bar is a depositional feature made of sediment that accumulates on the inside bend of streams and rivers below the slip-off slope. Point bars are found in abundance in mature or meandering streams. They are crescent-shaped and located on the inside of a stream bend.
Picture taken at:
Location:
Glacial Erractics
Boulders that are moved by glaciers
Picture taken at:
Location:
Metamorphic Scarp
Soil creep
Downhill creep, also known as soil creep or commonly just creep, is the slow downward progression of rock and soil down a low grade slope
Picture taken at:
Location:
Soil slump
A slump is a form of mass wasting that occurs when a coherent mass of loosely consolidated materials or rock layers moves a short distance down a slope.
Picture taken at:
Location:
Igneous scrap
Picture taken at:
Location: