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3842:278 Geomorphology

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Isostasy. Imbalance results in isostatic anomalies. Negative anomalies crust rises ... Glacio-isostasy. Result of accumulation or ablation of ice. Isostatic ... – PowerPoint PPT presentation

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Title: 3842:278 Geomorphology


1
38/42278Geomorphology
  • Topic 3 Endogenic and Climatic Effects
  • Chapter 2 Ritter et al
  • Chapter 3 Trenhaile

2
Primary External Controls
  • Endogenic processes
  • Determines lithology and structure
  • resisting forces
  • Climatic
  • Determines temp, precip, rates, intensity
  • Driving forces
  • Induce threshold events

3
Endogenic Effects
  • Tectonic processes that create/deform crust
  • Mountian building or orogenic events
  • Meso scale
  • Epeirogenic processes deform the crust
  • Macro scale
  • Volcanic activity
  • Regional scale
  • Influence topographic expression

4
Tectonic Processes
  • Cause changes in crustal thickness
  • Result in isostatic adjustments
  • Vertical movement of crust
  • Slow response

5
Isostasy
  • Imbalance results in isostatic anomalies
  • Negative anomalies crust rises
  • Positive anomalies crust subsides
  • Affect PE of exogenic systems
  • Base level changes
  • Incision or aggradation
  • Uplift normally gt denudation
  • Disequilibrium or threshold

6
Glacio-isostasy
  • Result of accumulation or ablation of ice
  • Isostatic rebound continues
  • Initially rapid (100m/ka)
  • Decreasing (5m/ka)
  • Total hundreds of metres
  • Isostatic adjustment of sea level, base level
    drops, stream incision

7
Hot Spots
  • Concentration of radioactive energy
  • Thermal expansion of upper mantle
  • Vertical displacement of several hundred metres

8
Tectonic Geomorphology
  • Emphasis on neotectonism
  • Focus on
  • impacts of tectonic actvity on process and form
  • What land form can tell us about tectonic
    activity
  • Measurable qualities of landforms
  • Type of tectonism
  • Rate

9
Fault-bounded Mountains
  • Mountain front sinuousity
  • Ratio of curved to straight line distance
  • Valley width to height ratio

10
Characteristic Landforms
11
Fault-scarp Analysis
  • Erosion and deposition on scarp face
  • Indicates relative age
  • Est. of absolute age
  • Dependent on rate of processes

12
Plate Margins
  • Emergent coastlines
  • Raised terrace
  • Narrow continental shelf
  • Coastal Cliffs
  • Incised river valleys
  • Submergent Coastlines
  • Wide continental shelf
  • Deposition
  • Low, wide coastal plain

13
Plate Margins
  • Emergent coastlines
  • Result of sea-level drop or tectonic uplift
  • If tectonic, suggests active plate margin
  • Characterized by
  • Raised terraces
  • Narrow continental shelf
  • Coastal cliffs
  • Incised river valleys

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15
Plate Margins
  • Submergent coastlines
  • Result of sea-level rise or tectonic subsidence
  • May indicate passive plate margin
  • Characterized by
  • Flooded estuaries
  • Coastal deposition
  • Low, wide coastal plain
  • Wide continental shelf

16
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17
Volcanism
  • Three different types of neotectonic activity
    result in distinctive landforms
  • Plateaus
  • Cones
  • Calderas

18
Volcanism
  • Plateaus
  • Extrusion of low viscosity basaltic lava
  • Extensive areas of overlapping flows
  • From numerous fissures and vents

19
Volcanism
  • Cones
  • Single vent
  • Shields Volcanoes
  • Effusive eruptions, low viscosity magma
  • Low, wide shields volcanoes
  • Composite Volcanoes
  • Explosive eruptions, high viscosity magma
  • Steep sided

20
Volcanism
  • Calderas
  • Collapse of cone into magma chamber
  • Large diameter (much larger than crater)
  • Associated ring fractures

21
Climatic Geomorphology
  • Philosophical approach to study of geomorphology
  • Based on the relationship between climate and
    landform
  • Certain landforms develop under particular
    climatic condition

22
Climatic Geomorphology
  • Climate determines
  • Rate
  • Effectiveness
  • . . . of geomorphic processes
  • Referred to as climate-process system
  • Processes that function most efficiently in any
    climate will prevail

23
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25
Climatic Geomorphology
  • BUT, landforms vary due to geographic variations
    in
  • Lithology
  • Structure
  • Seasonality
  • Changing climate (relic landforms)
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