LANDFORMS AND THEIR EVOLUTION Flashcards
type of plain forming as a result of
stream erosion is called a
peneplain
The divides between drainage basins are likewise lowered until they are almost completely flattened leaving finally, a lowland of faint relief with some low resistant remnants called
monadnocks
aterfalls and rapids may exist in this stage
youth
Streams divides are broad and flat with marshes, swamp and lakes in this stage
youth
Erosional landforms by running water
Valleys, Potholes and Plunge Pools ,Incised or Entrenched Meanders, River Terraces
DEPOSITIONAL LANDFORMS
Alluvial Fans, Deltas Floodplains, Natural Levees and Point Bars Meanders Braided Channels
a deep valley with very steep to straight sides
gorge
steep step-like side slope
Canyon
But very deep and wide meandersb can also be found cut in hard rocks
Incised or Entrenched Meanders
basically products of erosion as they result due to vertical erosion by the stream into its own depositional floodplain
River Terraces
This load becomes too heavyn for the streams to be carried over gentler gradients and gets dumped and spread as a broad low to high cone shaped deposit called
alluvial fan
In meanders there is active
deposition along the
convex bank
In meanders there is active undercutting along the
concave bank.
Any limestone or dolomitic region
showing typical landforms produced by the
action of groundwater through the processes
of solution and deposition is called
Karst
topography
EROSIONAL LANDFORMS for groundwater
Pools, Sinkholes, Lapies and
Limestone Pavements, caves
Depositional Landforms for groundwater
Stalactites, Stalagmites and Pillars
Small to medium sized round to sub-rounded
shallow depressions called
swallow holes
is an opening more or less circular at the top and funnel-shapped towards nthe bottom
Sink hole
The term is sometimes used to refer the collapse sink
doline
when sink holes and doline join , long,
narrow to wide trenches called
valley sinks or Uvalas form.