Earth Sci - The G's Flashcards
weathering
the breakdown of rock into smaller and smaller pieces
sediments
fragments of weathered rock
erosion
the movement of rock fragments (may also cause further weathering of fragments into even smaller pieces)
deposition
the drop off of rock fragments at a new location
6 agents of erosion/deposition
(unsorted) gravity, groundwater, glaciers
(sorted) waves, wind, water
gravity
force behind all erosion
erosion vs deposition (which one is dominant)
erosion - kinetic energy/speed of agent is high
deposition - kinetic energy/speed of agent is low
- weathering (definition + when it occurs)
definition: breakdown of rocks at Earth’s surface
occurrence: occurs due to exposure of the lithosphere to air, water, chemicals, and organisms
- physical weathering (definition)
breakdown of rocks without change in the rock’s composition
frostaction (physical weathering) (definition + climate)
definition: when water expands as it freezes (approx. 10%) and causes cracks in rocks to grow larger
climate: alternating between freezing/thawing (causes most damage) (temps above/below 0o), cold & wet climate
abrasion
collisions and scraping between rocks as they move
exfoliation
the “peeling away” of rock layers. the removal of overlaying rock layers reduces pressure and the rock expands upwards, resulting in exfoliation (like an onion)
plantaction
when plants help to breakdown rock (root wedging)
lichens
can cause both physical and chemical weathering of rocks
- chemical weathering (definition + occurrence)
definition: breakdown of rock with a change in the rock’s composition
occurrence: typically involves air, water, and/or chemicals
oxidation
when oxygen combines with other elements to form a new compound (e.g. rust)
carbonation
carbon dioxide can combine with water to form a mild acid which can weather rocks (can form from other pollutants as well).
calcite is particularly susceptible (H2O+CO2⟶H2CO3)
hydrolysis
water can react with minerals in a rock (e.g. water reacts with feldspar to produce clay minerals)
dissolving
when a rock becomes incorporated into liquid water to form a solution (solvene does dissolving, solute gets dissolved)
- factors affecting the rate of weathering
particle size, particle shape, rock hardness, climate
particle size
- smaller particles have more surface area than an equal volume of larger particles
- small rocks weather faster than an equal volume of large rocks
particle shape
- as rocks weather, their shape becomes more rounded
- angular rocks have more surface area than an equal volume of rounded rocks, therefore angular rocks weather faster than rounded rocks
rock hardness
rocks have specific chemical and physical properties that influence the rate and manner in which they weather
which rocks are resistant to weathering?
rocks that tend to be resistant will be
- higher in elevation
- jut out from a cliff
- steep cliff face
climate
frost action: climate should be cold/wet (alternating between freezing and thawing)
most chemical weathering: climate should be hot/wet
- sediments and soils