Chapter 15 Flashcards
Mechanical weathering
physical disintegration of rock without changes to its chemical composition
frost wedging
freeze-thaw action of water; ice wedges downward in openings, ice melts and water falls further down large opening, process repeats; frost shattering
salt wedging
salt left behind from evaporated water collects and pries apart rock openings
temperature changes
diurnal and seasonal temperature fluctuations modify volumes slightly; fracturing of rock over long time periods
Exfoliation
curved layers peel off of bedrock; create exfoliation dome; due to weathering, exfoliation can occur in granite through expansion—the material on top of the item is no longer present and no longer provides pressure
Chemical Weathering
decomposition of rock material through chemical alteration of minerals; greater surface area is decomposed faster; MOISTURE IS REQUIRED
high temp and precipitation increases chemical weathering
Oxidation
oxygen is combined with metallic elements in minerals to form new products
Biotic Weathering
plants and animals alter rock structure; impact of lichens and burrowing of animals
Mass weathering
process by which weathered material is moved short distances by gravity
factors affecting weathering
angle of repose, impact of water on lubrication of rock material
Fall
rockfall, talus/scree;
talus apron: uniform accumulation of rockfall material
talus cones: material tends to collect in cone shaped heaps
Slide
landslide, instantaneous mass slope collapse with NO FLUID flow lubrication
- SLUMP: rotation of sliding materials
- initiated from added weight from rainfall or earthquakes
- rock or avalanches
- lost material leaves a land scar
- damming of valley streams
Flow
wasting initiated or enhanced by the addition of water; water is the primary force, clay enhances the motion
- earthflows: water saturated land moves downhill
- mudflows: originated in arid basins; muddy downslope flows that can accumulate in large rock material
Creep
unobtrusive downslope flow of soil and regolith; freeze/thaw and wet/dry effects
- principle variables: slope angle, vegetative cover, moisture supply
- soilfluction: soil flowage
- terracettes