• Shuffle
    Toggle On
    Toggle Off
  • Alphabetize
    Toggle On
    Toggle Off
  • Front First
    Toggle On
    Toggle Off
  • Both Sides
    Toggle On
    Toggle Off
  • Read
    Toggle On
    Toggle Off
Reading...
Front

Card Range To Study

through

image

Play button

image

Play button

image

Progress

1/29

Click to flip

Use LEFT and RIGHT arrow keys to navigate between flashcards;

Use UP and DOWN arrow keys to flip the card;

H to show hint;

A reads text to speech;

29 Cards in this Set

  • Front
  • Back
Rock that is formed by weathering, erosion, deposition, and compaction
sedimentary
rock that is formed by cooling and solidification of a melt
igneous
rock that is formed by heat, pressure, and chemical activity
metamorphic
lithification
the transformation of loose sediment into solid rock through compaction and cementation
physical weathering
Rocks are broken by mechanical processes to form smaller rock fragments or sand/silt sized grains.
chemical weathering
takes place on/near earths surface. Atmosphere/rain is acidic. These acids attack and corrode rocks (old tombstones show chemical weathering very well).
natural cracks that form in rocks due to removal of overburden or due to cooling
joints
when water trapped in a crack freezes, it expands and causes the crack to open
wedging by frost
in arid climates, dissolved salt in groundwater precipitates and grows as crystals in open pore spaces in rocks. It then pushes apart grains and weakens the rock.
salt wedging
(tree/plant roots secrete acids and grow in small fractures in bedrock. With time, the plant roots grow in size, the increased size in root can break rocks.
root wedging
Rocks are heated by energy (light) from Sun. Rocks expand when heated, contract when cooled. Heat-cooling cycles weaken and break rock (Stone Mountain is the type locality)
thermal expansion
ls. Rain is slightly acidic due to ____ present in the atmosphere.
CO2
Halite dissolves completely in water
dissolution
Hydrolysis/Partial Solution
reaction of water and minerals “loosens” parent materials (Kfeldspar) and forms kaolin clay (basis of GA Kaolin Industry).
Oxidation
Iron (Fe) is oxidized by removing electrons by reaction with water. Result is a red colored soil.•
Hydration
absorption water by clay or clay minerals (gypsum, mica) – incr. volume deforms/expands soils.
What is the relation of surface area to weathering?
As rock breaks apart due to physical weathering, the surface area increases relative to volume.
What is the formula for surface area of a cube?

6(a)2

leaching
(top, or top soil and organic uppermost layer). (O and A horizon
subsoil
soil (zone of accumulation, accumulated from leaching zone, B- horizon)•
weathered rock or bedrock
(weathered by soil solutions, C-horizon
transition
on (E horizon)may or may not be seen in most soi
leaching
chemical weathering produces loose debris, new minerals. then rainwater carries dissolved ions and clay flakes downward. takes place in top soil
What process takes place in subsoil?
accumulation
Name soil types from thinnest to thickest
desert, temperate, tropical
Tropical soils are the thickest because the warm climate and heavy rainfall accelerates chemical weathering and allows for soils to be leached.
How does climate affect soil?
Slope steepness
a thick soil can accumulate under land that lies flat. On a steep slope, weather rock may wash away before it can become a soil.
Time
Young soils tend to be thinner than old soils.
What are the chemical weathering processes?
Hydrolysis/Partial Solution, Absorption, Oxidation, Dissolution