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Summary Grade 11 IEB Geography - Geomorphology $5.63   Add to cart

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Summary Grade 11 IEB Geography - Geomorphology

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This is an in-depth summary of Geomorphology in Grade 11 Geography.

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  • August 17, 2020
  • 15
  • 2018/2019
  • Summary
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Topography Associated with Horizontally Layered Rocks


CHARACTERISTICS AND PROCESSES ASSOCIATED WITH THE DEVELOPMENT
OF HILLY LANDSCAPES AND BASALTIC PLATEAUS

 Hilly landscape and basaltic plateaus develop in areas where rock strata are horizontal.
 Rock strata is uniformly resistant to erosion.



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Hilly Landscapes
 Layers of horizontal sedimentary rock with uniform resistance to erosion.
 Form a steep hilly landscape.
 Climate of area influences nature of slopes
 Humid Climates - form steep hills with rounded slopes as sheet wash takes place. Rainfall
removes surface material as it runs down slopes
 Arid Climates - form hills with narrow gullies and sharp ridges. Slopes are steep and
uneven as there is little rounding due to sheet wash. Also called badlands.


Basaltic Plateaus
 Fissure eruptions have caused lava to flow onto earth.
 Lave forms thick layers of basalt rock.
 These layers are horizontal and uniformly resistant to erosion.
 Layers of basalt give way to basaltic plateaus.

, CHARACTERISTICS AND PROCESSES ASSOCIATED WITH THE DEVELOPMENT
OF CANYON LANDSCAPES, KAROO LANDSCAPES AND SCARP RETREAT

 Canyon landscapes - develop in areas where rocks are stratified, and strata is horizontal.
 Rocks are not uniformly resistant to erosion.
 Karoo landscapes develops from the canyon landscapes.


Canyon Landscapes
 Result from horizontal strata vary in resistance to erosion.


How do canyons form?
 Tectonic uplift results in a large flat surfaced plateau.
 The horizontal resistant layer of rock prevents landscapes from becoming lower.
 Rivers erode vertically along joints and cracks and for deep, steep valleys.
 More resistant strata do not erode easily, form vertical cliffs, and less resistant strata
erode easily, form gentle slopes.
 Climates influences canyons:
 Humid Environment: water erodes slopes, makes canyon walls gentle and rounded.
 Arid Environment: there is little rainfall, slopes remain steep.


Karoo Landscapes
 Develop from canyon landscapes.
 Consists of flat-topped mountains/hills differing in width, steepness and concave-shaped
sides.
 Climate of Karoo is dry - little rain to make slopes gentle.
 Resistant layer of rock at top of landform which is called cap rock is usually sandstone and
softer shale below.
 Igneous intrusions can also for cap rock.


How does the Karoo landscape form?
 Floor of canyon gets wider and plateau surface gets narrower.
 Plateau remains at same height because of resistant cap rock.
 Develops into a mesa.
 When there is rain, water erodes the softer rock beneath cap rock and is formed into a
butte, pointed butte and then a conical hill.

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