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Ox-bow lake formation
Outer Bend ➡ Faster water flow ➡ Erosion (abrasion, hydraulic action)
Inner Bend ➡ Slower water flow ➡ Deposition (sand, rocks)
Continuous erosion ➡ Meander neck narrows
Flood ➡ Water cuts through meander neck (faster route)
Original meander sealed ➡ Oxbow Lake formed
Oxbow Lake ➡ Gradually fills ➡ Becomes bog (vegetation, sediment)
formation of waterfall
Water flows over hard rock and soft rock. Hard rock resistant erosion → the soft rock gets eroded faster
Hydraulic action & abrasion erodes the river bed more.
force of water undercuts the hard rock forming an overhang
plunge pool is formed at the foot of the river → to the sheer impact of the water.
After some time, the undercut area has no more support for overhang of hard rock → collapses into the plunge pool.
Pieces of the overhang erode plunge pool.
The waterfall now retreats upstream, forming a gorge (deep and narrow valley)
formation of spit
prevailing winds blow at an angle
swash moves beach material towards direction
backwash drags sediment perpendicular to angle
zig-zag motion → longshore drift
spit formed → material depositing at change in coastline direction
recurved end form when wind approach in different direction
formation of cliff cave arch stack stump
Cliff ➡ Erosion (hydraulic action, abrasion) ➡ Rock layers exposed
Cave ➡ Erosion on weak rock ➡ Undercutting at base of cliff
Arch ➡ Cave on both sides of headland ➡ Erosion breaks through ➡ Arch formed
Stack ➡ Collapse of arch ➡ Sea erodes base ➡ Stack formed
Stump ➡ Stack collapses ➡ Sea erosion ➡ Stump remains