Key concepts Flashcards
Give examples of the following landform classifications
Morphological
Genetic
Morphological (size, shape, composition, location)
EG Plateau, Basin, Ridge, Terrace
Genetic (Fluvial, Glacial, Weathering, Coastal)
EG Moraine ridge, river terrace, sinkhole, glacial trough
Whats the difference between erosional and depositional forms
erosional - removal of material ( frost weathering)
depositional - addition of material (Scree slope)
Briefly describe the functional approach
based on the identification and explanation of process-form links
Form - interpreted from mapping, lab experiments (analysis) and computer simulations (modelling)
Distribution and intensity of process is interpreted from distribution of forms (climatic geomorphology)
Equilibrium form to be restored after a disturbance by high magnitude
Breifly describe the historical (evolutionary) approach
focuses on progressive changes in landscape through time
can be used to
- reconstruct past environments
- determine effects of future changes (landscape sensitivity)
recognises that landforms are transient, a stage in an evolutionary sequence operating on a very long timescale
Why are landscapes different ?
Resistance - Force - Time
Resistance - mechanical strength and chemical composition of materials. RESISTANCE to weathering and erosion across earths surface
Land forming processes vary over time. many processes related to climate which varies over space
TIME - physical changes are only observable over a long time period.
prolonged action of a process can lead to sudden and spectacular change to a land form = THRESHOLD RESPONSE
What are formative events and give examples
events which change the landscape by bringing about a recognisable and persistent response (their thresholds have been reached)
E.G.
- Floods sustained rainfall = landslides, debris flow, sinkhole formation)
- Earthquakes
define:
- Post-event readjustment
- Form constant
post event readjustment periods of variable length which immediately follow each formative event, in which the landscape readjusts to its new state.
Form constant - periods of variable length which follow from periods of adjustment, when no change occurs (thresholds are not exceeded)
What are the three fundamental factors of Selby’s model of the tempo of landscape evolution
- The magnitude of formative events
- The frequency of formative events
- The time taken for the landscape to readjust to an event