weathering Flashcards
denudation
lowering of continental surfaces
3 elements of denudation
- weathering
- mass wasting/mass movement
- erosion
weathering AKA
how to lower
two types of weathering
- physical
- chemical
physical weathering
breaks down big rocks into smaller pieces BUT the chemical composition does NOT change
physical weathering AKA
disintegration
chemical weathering
big rocks are broken down to smaller rocks WITH their chemical composition changing (become new rocks)
chemical weathering AKA
decomposition
mass wasting is
the transfer of material downhill via GRAVITY
erosion is the
transfer of material by water, wind or ice
weathering is the
IN SITU breakdown of rock
what are 4 thing that control weathering
- rock properties
- climate
- soil and vegetation
- length of exposure
how are some rock properties affect weathering
- hardness
- composition
- solubility
- zones of weakness aka joints
how does climate affect weathering
depending on the temp and moisture, it can either accelerate or inhibit weathering
how do soil and vegetation affect weathering
exposes rock to variations in moisture and chemistry
physical weathering AKA
mechanical weathering
physical weathering converts rock into smaller pieces that can be act on more by
erosion
how do physical weathering and surface area relate
as the rock is broken down to smaller pieces, there is more surface area
an increase in surface area by physical weathering allows for _____
more reactions to take place
important physical weathering processes
- frost action
- salt weathering
- pressure-release jointing
- biological forcesq
what is frost action
the weathering processes caused by repeated cycles of freezing and thawing
describe the process of frost action
meltwater leaks into cracks and freezes causing fissures to expand under pressure and, with repeated cycles, shatter the surrounding rock.
where does frost action take place
in places that often go through rises and falls in temp through zero (like the Himalayas)
salt crystal growth process
- as water evaporates, it leaves salt in the rocks
- over times the crystallization breaks apart the rock
where does salt crystal growth happen
- dry environments
- areas with lots of ocean spray
pressure-release jointing process
- rocks in the surface are exposed to high levels of pressure and heat that stick them together
- as they reach the surface, there is less pressure which causes them to break apart
what is the result of pressure-release jointing
slab-like layers or sheets break loose
how can biological activity act as physical weathering of rocks
- plant roots can break up the rock as they push through
- some animals can break rocks as they make homes (clams)
what does chemical weathering involve reactions between
air and water and minerals in the rock
where is chemical weathering going to occur FASTER
in places with warm temps and lots of water
why does chemical weathering happen in places with lots of water and warm temps
because these conditions promote faster chemical reactions
how can chemical weathering accelerate physical weathering
it makes the rocks more susceptible to physical weathering as the crystal structures are disrupted
important chemical weathering processes
- hydrolysis and hydration
- dissolution of carbonates
hydrolysis is the _____ of a molecule by the _____ of a water
breaking and addition
what do the free hydrogen or hydronium ions in WATER do in hydrolysis
participate in chemical reactions that make NEW compounds
what can be the result of hydrolysis
crystal structure of weaker minerals may breakdown = granular disintegration
dissolution of carbonates
reaction where carbon combines with minerals and dissolves them
what forms in the dissolution of carbonates
weak carbonic acid (water and carbon dioxide)
dissolution of carbonates is related to
kast topography
kast topography
the solution of carbonate rock results in a landscape of pitted, bumpy surface with vast underground channels or caverns
what are the 3 conditions for karst topography
- rocks with equal or over 80% calcium carbonate AND have jointing
- climate must be warm and moist
- there must be vegetation to increase CO2 in soil
where do physical/mechanical weathering dominant
drier, cooler climates
where does chemical weathering dominant
moister, wetter climates
benefits of weathering
- produces parent material for soils
- releases/produces minerals not able to be access another way
4 categories of soils
- gravel
- sand
- silt
- clay
order of soils based on largest to smallest particle size
- gravel
- sand
- silt
- clay