* involves the *physical breakdown* **(disintegration)** and *chemical alteration* **(decomposition)** of rock at or near the Earth’s surface
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Mechanical Weathering
* __Accomplished by physical forces__ that break the rock into smaller and smaller pieces __without changing the rock’s mineral composition__. * the disintegration of Earth's materials makes __*detrital sediments*__
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Frost Wedging
* When water enters the joints, alternate freezing and thawing episodes ***pry the rock apart.*** * After water works its way into the cracks in the rock, t__he freezing water enlarges the cracks, and angular fragments are eventually produced__.
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Salt Crystal Growth
* __Force exerted by a salt crystal that forms as water evaporates__ from pore spaces or cracks in rocks can cause the rock to fall apart. * __Infiltration of salty waters__ on rocks or soils from groundwaters or salty seawater.
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Sheeting
* Also known as ***exfoliation***, it is caused by the expansion(pressure release) of crystalline rock as erosion removes the overlying material(overburdened rock)
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Abrasion
* Wearing away of rocks by the **constant collision of loose particles**
* This can be due to water, wind, or ice.
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Biological Activity
* __Plants and animals__ as agents of mechanical weathering * Wedges in rocks and soils form through plant growth (rooting) and motor activities of animals and even humans (like burrowing or shoveling).
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Chemical Weathering
* Involves __a chemical transformation of rock__ into one or more new compounds. * Decomposition of rocks and minerals by chemical processes
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Dissolution
* dissociation(splitting) of molecules into ions * the process by which a mineral completely dissolves in water or other acidic solutions * a common example includes the __________ of calcite and salt
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Oxidation
* reaction between minerals and oxygen dissolved in water * the ***reaction of oxygen with iron-bearing minerals*** in rock.
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Hydrolysis
* change in the composition of minerals when they react with water * occurs when silicate minerals react with water so that the mineral recombines with the water molecule to form a new mineral. * For example, consider the mineral potassium feldspar
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Spheroidal weathering
* A form of chemical weathering where a generally spherical boulder is c***racked & split off into curved layers*** on a much smaller scale
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Climate
? Cold and dry
? High temperature and high rainfall
A factor that affects weathering:
* __The presence of water__ which is an important chemical weathering agent increases the rate of weathering. * __High temperature__ enhances chemical reactions.
? What climate causes a slow rate of chemical weathering
? What climate causes a high rate of chemical weathering
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Rock Type
A factor that affects weathering:
* The minerals that constitute rocks have different susceptibilities to weathering. * Those most stable to surface conditions will be the most resistant to weathering.
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Rock Structure
A factor that affects weathering:
* rate of weathering is __*affected by the presence of joints, folds, faults, bedding planes*__ through which agents of weathering enter a rock mass.
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Topography
? Steep slopes
? Gentle slopes
A factor that affects weathering:
* Weathering may occur more quickly on a steep slope than on a gentle one
? In what kind of slope is physical weathering faster
? In what kind of slope is chemical weathering faster
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Time
A factor that affects weathering:
* Longer exposure to weathering agents could mean a higher degree of weathering processes have occurred. The rock has been weakened; therefore, easier to be a break. * Length of exposure to agents of weather determines the degree of weathering of a rock
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Erosion
* the incorporation and transportation of material by a mobile agent such as water, wind, or ice
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Deposition
* the settlement of material on a definite location; the inability of a mobile agent to transport deposits material.
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* Running Water * Ocean or Sea Waves * Groundwater * Glacier * Wind * Gravity
* What are the basic agents that drive sediment transport?
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Hydrologic Cycle
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Drainage basin
* the area drained by a stream and its tributaries
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Divides
* boundaries between drainage basins
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Laminar flow
* fluid travels smoothly or in regular paths
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Turbulent flow
* irregular fluctuations of liquid * the speed of water is continuously undergoing changes in direction & magnitude
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Overland flow
Encompassed by Running Water
* surface run-offs * water flow down to a drainage basin due to a drainage divide, form rills and gullies on the surface due to erosion(rill & gully erosion) * can erode before forming rills and gullies by sheet erosion
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Streamflow
Encompassed by Running Water
* water flow in drainage basins(valley formation) * turbulent flow of water is usually in river channels
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Velocity
A factor affecting stream
* dictates the ability of a stream to erode & transport * controlled by __*gradient, channel size & shape, channel roughness and the amount of water flowing in the channel*__
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Gradient
A factor affecting stream
* slope of the stream expressed as the vertical drop of a stream over a specified distance * reserves much more enrgy the steeper it gets
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Channel
A factor affecting stream
* stream path; straight channel can cause smooth stream(smooth erosion) while curved/banked channel can slow the stream and make it turbulent
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Discharge
A factor affecting stream
* volume of water passin through a cross-section of a stream during a given time * as the discharge increases, the width of the channel, the depth of flow or flow velocity increase individually or simultaneously
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Slows the velocity
* What happens to the velocity when a channel is widened by soft rock and becomes rough & boulder strewn? * what happens to the velocity when the channel is wide & shallow, increasing friction?
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Stream velocity increases
* What happens to the velocity when a landslide narrows a channel? * What happens to the velocity when a channel is semicircular? * What happens to the velocity when bridge, piers or other obstructions are put up?
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Headward Erosion
Styles of erosion
* makes a river longer * happens near its source * surface run-off and flow cause erosion at the point where the water enters the valley head
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Vertical Erosion
Style of erosion
* makes a river channel deeper * this happen more in the upper stages of a river
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Lateral erosion
Style of erosion
* makes a river wider * this occurs mostly in the middle and lower stages of a river
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Quarrying
Erosion process in running water
* involves the removal of blocks from the bed of the channel
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Abrasion
Erosion process in running water
* bed & banks of a bedrock channel are ceaselessly bombarded by particles carried into the flow
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Corrosion/Solution
Erosion process in running water
* a procces in which rock is gradually dissolved by the flowing water
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Dissolved Load
Running Water: Transport sediment
* solution * transportation of dissolved mineral which is moved and dispersed in stream * usually came from groundwater
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Suspended Load
Running Water: Transport Sediment
* suspension * fine sediments(such as clay) transported in streams as suspended sediments * usually came from flooding/run-offs
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Bed Load
Running Water: Transport Sediments
* coarse grains * transportation by traction(rolling of gravels such as boulders) and saltation(skidding or jumping movements of smaller gravels such as pebbles)
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Bedrock Channel
Running Water: Channel Formation
* channel which consists and generally formed by rocks whereas its pattern is geologically structured * definite and uniform structure
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Straight Channel
Running Water: Channel Formation; Bedrock Channel
* form where a stream erodes sediments in a constant patter without drstic change in its path/flow
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Alluvial Channel
Running Water: Channel Formation
* watewr path whereas it has no definite patter and it changes its structure * composed of unconsolidated sediments
* form where streams that transport much of their load in suspension generally move in sweeping bends
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* River valleys, waterfalls, potholes, terraces, gulley/rills * Meanders(exhibit erosion & depositional features), oxybow lake, peneplain
* What are the of Erosional Landforms from Running water as an agent of erosion
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* Alluvial fans/cones, natural leeves, deltas
* What are the Depositional landforms from running water as an agent of erosion?
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Deltas
Running Water: Deposits According to Agents of Erosion
* form where sediment-charged streams enters the realtively still water of a lake, an inland sea, or the ocean
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Natural Levees
Running Water: Deposits According to Agents of Erosion
* meandering rivers that occupy valleys with broad floodplains, tend to build _____ ______ that parallel their channels on both banks
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Alluvial Fan
Running Water: Deposits According to Agents of Erosion
* Are fan-shaped deposits that accumulate along steep mountain fronts * When a mountain stream emerges onto a relatively flat lowland, its gradient drops and its deposits a large portion of sediment load
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Waves
Ocean or Sea Waves
* energy transported to a medium * are caused by energy transferred by wind or storm in the ocean’s surface
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* Wave Height * Wavelength * Wave period
Characteristics of a Wave
* What do you call the vertical distance between trough and crest? * What do you call the horizontal distance between successive crests(or troughs)? * What do you call the time it takes one full wave to pass a fixed position?
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* Wind speed * Length of time the wind has blon * Fetch or distance that the wind has traveled across open water
* What are the factors that affect the Height, Length & Period of a Wave?
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Hydraulic Action
Shoreline Erosion Process of Ocean/Sea Waves:
* Rock wedging and disintegration due to wave slap
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Abrasion
Shoreline Erosion Process of Ocean/Sea Waves:
* the sawing and grinding action of the water armed with rock fragments
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Corrosion
Shoreline Erosion Process of Ocean/Sea Waves:
* dissolution of rocks due to constant wave current
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Wave Refraction
Transportation by Waves and Currents:
* bending of waves making wave front parallel to the shore
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Longshore Current
Transportation by Waves and Currents:
* erosion of sediments/soils by angled/oblique wave to the shore
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Rip Current
Transportation by Waves and Currents:
* Concentrated movement of water that flow in the opposite direction from breaking waves
* What are the Depositional Features from Ocean/Sea Waves as an agent of erosion
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Glaciers
* a moving body of ice on land that moves downslope or outward from an area of accumulation
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Ice Sheets(continental glaciers)
Types of glaciers:
* Cover large areas of the land surface * unconfined by topography * cover Antartica and Greenland
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Outlet glacier
* when a glacier flows out of an ice sheet, ice cap or icefield
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Valley(Alpine) Glaciers
Types of glaciers; Ice Sheets:
* bounded by vallewys and tend to long and narrow * can be formed when an outlet glacier forms and slides away from an icefield * Can also be formed on their own, starting from high up on a mountain range and flowing down within the steep V between two peaks
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Ice Shelf
Types of glaciers:
* a thick slab of ice, attached to a coastline and extending out over the ocean as a seaward extension of the grounded ice sheet
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Cirque Glaciers
Types of glaciers:
* snow that accumulates in small depressions on the side of a mountain, eventually compacting into glacier ice * when the glaciers are built up and shifted, they erode the depression to form bowl shaped valleys called corries or ______ * may sometimes accumulate enough ice to spill over and form valley glaciers
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Firn
Glaciers: Glacial Formation
* a recrystallized snow that is dense and is in granular form with a texture like coarse sand * basic structure that is pressurized to form glacial ice
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* plastic flow * basal slip
Glaciers: Glacial Movement
* Glaciers move to lower elevations by _______ ____ due to great stress on the ice at depth; * and _____ ____ facilitated by meltwater which acts as a lubrican between the glacier and the surface over which it moves
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* Plucking * Abrasion
Glaciers: Glacial Erosion
* What do you call lifting piecies of bedrock beneath the glacier? * What is the grinding and scraping by sediment already in ice called?
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* Glaciated Valleys * Glacial Through * Truncated Spurs * Hanging Valleys * Paster Noster Lake * Cirque * Tarn * Col * Aretes and Horns * Rouches Moutonnees
* What are the landforms created by glacial erosions?
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Glacial Till
Glaciers: Glacial Deposits
* deposited as glacial ice melts and drops its load of rock fragments
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Stratified Drift
Glaciers: Glacial Deposits
* deposited by the glacial meltwater and thus has experienced the sorting action of water
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Wind
* a relatively insignificant erosional agent * Dryness and scant vegetation are important prerequisites for it to be an effective errosional force
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Dunes(Sand Deposits)
Type of Wind Deposits:
* Hills or ridges of wind-blown sand
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Loess(Silt Deposit)
Type of Wind Deposits:
* Extensive blankets of silt that were once carried in suspension
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Barchan
Wind: Type of Sand Dune
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Transverse
Wind: Type of Sand Dune
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Barchanoid
Wind: Type of Sand Dune
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Longitudinal
Wind: Type of Sand Dune
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Parabolic
Wind: Type of Sand Dune
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Star
Wind: Type of Sand Dune
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Groundwater
* represents the largest reservoir of freshwater that is readily available to humans * erodes sediments chemically rather tham mechanically(Weathering and movement of solution)
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Zone of soil moisture
Distribution of Groundwater
* area where water is molecularly atrracted and suspends
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Unsaturated(Vadose) Zone
Distribution of Groundwater
* contains both air and water * water cannot be extracted through wells
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Saturated(Phreatic) Zone
Distribution of Groundwater
* where all the open spaces in sediments and rocks are completely filled with water
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Groundwater
Distribution of Groundwater
* water present in the phreatic zone
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Water table
Distribution of Groundwater
* the upper limit of the phreatic zone(boundary with the valdose zone; “water level”)
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Capillary fringe
Distribution of Groundwater
* Just above the water table * zone where water can penetrate
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Graining Streams
Stream-Groundwater Interaction:
* inflow of groundwater through the streambed * higher elevation of water table * receive water from he groundwater system
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Losing Stream
Stream-Groundwater Interaction:
* lower elevation of water table * water from streambed follow down to groundwater * can be connected ot disconnected * provide water to the groundwater system * (disconnected) may form a buldge in the water table when it is separated from the groundwater system by the unsaturrated zone
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Porosity
* Factor affecting the storage and movement of groundwater * percentage of total volume of rock or sediment containing pore spaces
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Permeability
* Factor affecting the storage and movement of groundwater * the ability to transmit fluid
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Aquitards
* Factor affecting the storage and movement of groundwater * impermeable layers that hinders water movement
Ex. clays have mcuh smaller pores
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Aquifiers
* Factor affecting the storage and movement of groundwater * Permeable layers that transmit groundwater freely
Ex. Sand & gravels have much larger pores
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Specific Retention
* Factor affecting the storage and movement of groundwater * the ratio of the volume of water that a given body of rock or soil will old against the pull of gravity to the volume of the body itself
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Specific Yield
* Factor affecting the storage and movement of groundwater * also known as the drainable porosity * is a ration, less than or equal to the effective porosity