Chapter 9: Weathering, Karst Landscapes, & Mass Movement Flashcards
Geomorphology
A subfield in which there is an investigation of the origin, evolution, and distribution of surface land forms.
Orogenesis
Plate tectonics, earthquakes, folding, faulting, volcanoes. The creation of new landforms new mountains in particular.
Denudation
A process where you have these landforms that are worn away and rearranged. Weathering and erosion
Weathering
A process where you have the breakdown of rocks just below the surface. Only the break up of rock not the transportation.
Mass Movement
The movement of surface materials Like soil, rocks, vegetation. Material that has been weathered that has been broken up into smaller pieces and then can be transported to a different location
Erosion
The transportation of materials to different locations, materials that have been weathered and transported elsewhere. Transported via different mediums like through the water, ocean, stream systems, frozen water, wind,
Slope
Any sort of incline or angled surface. The steepness of an inclined surface,
Angle of Repose
The maximum incline at which sediments on a slope can remain at rest before gravity begins to pull them down slope. The highest angle at which material is going to stay in place on a slope. Usually between 33 and 37 degrees.
Stable slope
A situation where the strength of the slope is going to exceed the force of gravity, lower likeyhood of mass movement
Unstable slope
A situation where the strength of the slope does not exceed the force of gravity, could be an indication of some sort of failure like a rock slide or and landslide type thing.
Bedrock
The parent rock from which Regolith and soil develop, rock that is weathered into smaller pieces.
Regolith
An unconsolidated in the snice that it is not in destink layers, its all mixed up together, it is on top of or covering bedrock.
Physical Weathering or Mechanical Weathering: Frost Action
When water freezes it expands, especially in colder climates where you have regular freeze and thaw cycles sometimes on a daily basis or a longer period of time, water gets in between parts of the rock cracks within the rock and then freezes nd expands and contracts and breaks part of the rock.
Salt Crystal Growth- Crystallization
Most common in arid environments and drier areas, you have what’s known as crystallization occur the moisture inside of a rock in particular something like sandstone where there are a lot of tiny air gaps and water will go down there evoate and leave behind salt crytsals
Salt Crystal Growth/Salt Weathering
As slt crystals grow going to get bigger in size and going to exert enough force that they’ll start to break apart the individual grains in the rock.