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Geomorphology
Study of the shape of Earth’s surfacee/landforms.
Source to Sink Perspective
Creation of materials that onset geomorphic processes and where those materials go.
Physiographic Provinces
Areas with similar geographic processes that produce similar landforms, as well as similar tectonic origin and climate.
Mass Conservation
Differences between inputs and outputs. (I - O = deltaS).
Inputs include:
Precipitation, Tectonic Uplift
Outputs include:
Stream flow, Evaporation, Erosion, Landslides
Energy Conservation
Potential Energy converts to Kinetic Energy (Landslides)
Force Balance
Driving and resisting forces equally acting on something. (Ex: Boulder balancing on a hill)
Driving Forces
Gravity, wind
Resisting Forces
Slope terrain, Friction
Thresholds
Point in which further change in conditions causes a major change in landscape. Can change steady states (Deforestation can cause increase in fluvial sediment flux).
Steady State
landscape oscillates around a mean condition. (Mountain erosion over 1000s of years, Fluvial sediment flux)
Magnitude Frequency Relationship
Larger magnitude events happen less frequently than smaller magnitude events.
Herodotus (484-430 BCE)
First “historian”, estimated Nile River growth rates, observed silt deposition
Aristotle (384-322 BCE)
Proposed silt deposited by rivers would will seas and flood land
Nicholas Steno (1638-1686)
Proposed laws od superposition, and modern topography
Charles Lyell (1797-1875)
Proposed uniformitarianism
Mary Somerville (1780-1872)
Wrote “The Connection of the Physical Sciences and Physical Geography”, emphasized the interdisciplinary nature of science.
G.K. Gilbert
Published “Geology of the Henry Mountains”, studied how erosional processes shape modern geologic features.
William Morris Davis
Proposed the cycle of erosion:
Marie Curie
Developed theory of radioactivity
Plate Tectonics (as a concept)
Arose and pointed answers to how mountains form.
Baynold and Leopold
Applied physics and engineering framework into geomorphology.