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< WEATHERING > CHEMICAL WEATHERING differential weathering
MECHANICAL WEATHERING PHYSICAL WEATHERING SPHEROIDAL WEATHERING
abrasion carbination
frost wedging Goldrich Stability Series hydration
hydrolysis ice wedging oxidation
< EROSION > BED LOAD CREEP
DEBRIS FLOW differential erosion DISSOLVED LOAD
LAHAR landslide MASS WASTING
MUDFLOW ROCK GLACIER ROCK SLIDE
SALTATION SEDIMENT LOAD shoreline erosion
SLUMPING SOLIFLUCTION
ABRASION - is a form of physical weathering where rocks tumble over one another
rounding corners from angular, to sub-rounded, to rounded ;
CARBINATION - the reaction of carbonate and bicarbonate ions with minerals.
Carbonation is especially active when the reaction environment is abundant with
carbon dioxide ; INDEX - goemorphology - weathering
CHEMICAL WEATHERING - The process that changes the chemical makeup of a rock or
mineral at or near the Earth’s surface ; INDEX - goemorphology
CREEP - slow dowhill movement of regolith due to seasonal expansion and
contraction that results from freeze / thaw and wet / dry cycles ;
S.A: mass wasting ;
DIFFERENTIAL EROSION - variable rates of rock weathering associated with
resistance of rock to weathering. While softer are eroded and carried away,
harder and more resistant rocks remain to form ridges, hills, or mountains ;
SYN. DIFFERENTIAL WEATHERING
DISSOLVED LOAD - a significant portion of the total stream load where chemically
dissolved sediment combines with bed load & sediment load within a stream ;
INDEX - geomorphology - erosion
DISSOLUTION - the hydrolysis of limestone and rocks high in salt ; S.A: hydrolysis ;
FROST WEDGING - a form of physical weathering that breaks rocks by liquid water
freezing within a pore space and exerting an outward force ; SYN. ICE WEDGING
EROSION - sediment transport by wind, water, glaciers, or gravity ; S.A: mass
wasting / landslide ;
HYDRATION - an inorganic chemical reaction where the rigid attachment of H+ and
OH- ions to a reacted compound. In many situations the H and OH ions become
a structural part of the crystal lattice of the mineral ;
HYDROLYSIS - the reaction between mineral ions and the ions of water (OH- and H+).
Its the primary method of weathering silicate and alumino-silicate minerals
because of their electrically charged crystal surfaces ; S.A: DISSOLUTION ;
OXIDATION - a form of chemical weathering where oxygen reacts with other
elements in the rock ; INDEX - goemorphology - weathering
PHYSICAL WEATHERING - a process that break rocks without changing its chemical
compostion ; SYN. MECHANICAL WEATHERING
ROCK GLACIER - a mass wasting erosion process similar to glacial erosion except
the ratio of ice and rock are reversed ;
SALTATION - a sediment transport process that moves large material by a hoping or
bouncing motion ; S.A: traction ;
SALT CRYSTALLIZATION - a form of physical weathering similar to frost wedging.
This type of weathering occurs when salt water penetrates rock pores and
generates salt crystals as the water evaporates. The crystal growth produces
an outward force ;
SLUMPING - a type of mass wasting erosion often called a slope failure ;
SOLIFLUCTION - similar to creep, this form of mass wasting occurs when water
saturated soil, like thawing permafrost, slowly moves downhill to create
distinctive features called solifluction lobes ;
SPHEROIDAL WEATHERING - a type of chemical weathering that rounds off angluar
rock surfaces due to the larger surface areas ;
STREAM LOAD - the solid matter carried by a stream as bed shear stresses increase
to remove material from the stream bed ; INDEX - goemorphology - erosion
TRACTION - a sediment transport process that moves large material by rolling
or sliding across the bottom of a river or stream bringing interaction with
the sbustratum ; S.A. saltation ; INDEX - goemorphology - erosion
QUARTZ (chemical weathering) - quartz grains + silica solution
FELDSPAR (chemical weathering) - clay minerals + mineral solution
GRANITE (chemical weathering)
-----------------------------
anorthite + water + CO2 = KAOLINITE + calcium bicarbonate
orthoclast + water + CO2 = KAOLINITE + potassium bicarbonate
albite + water + CO2 = KAOLINITE + sodium bicarbonate
LANDFORM - MOUNTAIN CHAIN
Mid-Atlantic 10,000 mi : 16,000 km
Andes 4,500 mi : 7,242 km FOLD 25 MYA
Rocky's 3,000 mi : 4,800 km FOLD 300 MYA - core 1-B
Ural 1,570 mi : FOLD 300 MYA
Himalya's 1,400 mi : 2,300 km FOLD 50 MYA
Alp's 500 mi : 800 km FOLD 65 MYA
Sierra Neveda 400 mi : 650 km FAULT-BLOCK 40 MYA
Cascade 700 mi : 1,100 km FOLD 37 MYA - north 400 MYA
Appalachian's 2,200 mi : 3,500 km FOLD 480 MYA
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