weathering, erosion, deposition, and landscapes …€¦ · web viewwhen an agent of erosion...
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Name _______________________________________ Period __________Weathering, Erosion, Deposition, and Landscapes Outline
Weathering The ________________ of ______________ due to ____________ or
_____________ changes
Physical Weathering Changes the ___________ and/or _____________ of a ____________
without changing the ______________ composition
In ________________ action, __________ seeps into ____________ in
rocks. The water ________________ as it _____________ and makes
______________ in the rock a little larger
When the ___________ melts and the liquid ___________________,
the rock is left more ___________________
Over time, the ______________ and ________________ in the cracks
will cause the rock to _______________
Physical Weathering ____________ roots grow in rock ________________ and gradually
_________ the rock ___________
_________________ that _________________ beneath the ground will
______________ new rock _____________ to __________________
__________________________ occurs when rock ________________ are
carried in water, they __________ and _____________ against other ____________
Chemical Weathering When rocks are _____________ to the _______________ and
_______________, they often undergo ______________ in the _______________
composition of rock, forming new ________________________
Usually requires ___________ and __________ to bring about _________
changes
Therefore, it takes place more ____________ in ___________,
_________ climates
Soil Formation Soil is a _____________ of weathered __________ and ___________
remains the usually covers _____________
The weathering of ________ produces ____________ layers
The ___________ layer is usually the best for
growing ____________ because it is rich in
______________ remains called ____________
The next layer is usually ______________
enriched from ___________________ transporting
________________
The ________________ layer is composed of
____________-up ______________
Erosion of Sediments ____________________ are rocks that have been _____________ into
_________
_________________ is the _______________ of ________________ away
from their place of ______________ and __________________ them elsewhere
_____________, ___________, ____________, and __________ erode
sediments
Erosion by Water The _______________ particles are carried in ____________________
The _____________ and most ___________ particles are __________ or
________________ along the streambed
Particles of low ______________, such as _____________ remains, are
carried along the _____________ by ________________
Velocity of Streams The _____________ of a stream is controlled by the
____________ and the _____________ of water
_______________ in the stream (________________)
As the stream ________________ increases, so does
the ______________ of the water ________________ in the
stream
______________ is also increased by an _____________ in the
____________ of ___________ in the stream
There is a direct __________________ between the ____________ of a
________ and the __________ of the _____________ it can transport
_____________ grains of _____________ can only be ______________ by
fast-moving water
Streams with _____________, ____________ valleys often develop _____-
shaped curves called _____________________
At the ____________ in the _____________, the _____________-flowing
water swings to the ______________ of the _________, causing _____________
along the ______________ bank
The _____________ moving water stays to the ____________ of the
_________, causing _______________
Erosion by Wind _______________ can pick up _____________ rock materials, such as
_________, _________, and _______, and ___________ them away
_____________ erosion occurs mostly in _________ areas, such as
____________ and _________________
___________ blown by the wind can ___________ down material on a rock’s
surface
Erosion by Ice If more ____________ accumulates in the __________ than _________ in the
______________, the __________ on the bottom turns to __________
If it becomes ___________ enough, its ___________ will cause it to
_________ under the pull of ___________
A ____________ is a large mass of __________ ice
As a glacier ____________, it carries, pushes, and drags loose ________
material
The ___________, with pieces of __________, smoothes, striates
(____________),
and _______________ bedrock
As a glacier _______________ through a ______________, it will make a
___-shape instead of a ____-shape caused by ________
When the ___________ melts, unsorted ___________ and ___________ are
left scattered around on _______________ and sides of valleys
Deposition When an agent of erosion _____________, or
lays down ___________ and ________________ of
earth materials (___________________)
Also called ________________________-
Most ________________ takes place in
_____________
Deposition Factors Particle _____________
____________ particles (clay and silt) settle more ______________
than cobbles and boulders
Particle ________________
Friction between _____________ and the ______________ of particles
___________ down ___________
________________, _____________ particles settle more
___________
Particle ______________
___________ particles settle _____________, ________ dense particles
take ________________ time to settle
Settling ___________ and ___________
____________ that settle at a _____________ rate
require __________ time
As the rate of settling ____________, the
settling time _____________
Sorting of Sediments __________________ sorting occurs at the
_________ of __________
The ____________ sediments can be carried a __________ distance
from shore
_________________ sorting occurs when a landscape
____________ a variety of particle sizes in to still water
Deposition by Wind Usually sorts _____________ by __________
___________ bedding ____________ meet a
different ____________
Deposition by Gravity At the _________ of a _________, where __________ of weathered rock
have __________, you will find __________ of many different __________
The ______________ are not _______________
Deposition by Glaciers Occurs when a ____________ melts and sediments are ____________
Glacial _____________ are large ___________ that have been
____________ by glacial _______________ without being ______________ into
small particles
They are often found _____________ above __________ valleys
_____________ and striations (_________________) indicate transport by
______
Alpine Glaciers Also known as ______________ glaciers, occur in ______________ regions,
and may ________ out __________-shaped ____________ with their moving
_______
Continental Glaciers Also known as ________ sheets causes _____________ of the ________ as
rocks are __________ within the _____________ or ____________ under the
flowing ice
Glacial Features __________ _________ – when glaciers act like ______________, grinding
the ______________ edges from the __________________ and _______________
hard bedrock _____________
__________________ – parallel ______________ and _____________ in the
bedrock left by the _____________ in the glacier
________________ – accumulation of _________ and _____________ that
builds up in ____________ of the flowing ice
___________________ – where the ice front ____________ its southward
advance, _________ of unsorted __________ and __________ remain
________________ – _________ spots in the glacial deposits and places
where large, ___________ ice blocks ______________ leave these dry
___________ and ___________ called _______________ _________________
North American Continental Glaciation
The Oceans and Coasts
_________________ covers almost _____% of our planet
The average _________ is about ________ (______)
One ___________ of ____________ contains about _______% of dissolved
_____
Sodium chloride (_____________) is the most _______________
When __________________ of ocean water causes the _________ to become
too _____________ to stay in solution, they are _____________ as
_______________
The _________ of the oceans are places of __________ caused by the action
of ___________ and ___________________ currents
Beach ________________ are _______________ and reduced in ________
by ________________ as the energy in the breaking _____________ causes the
______________ to __________ against one another
____________ is often transported along the ____________ and just outside
the breaking waves in the zone of _______________
_______________
This __________________ of sand builds the
_______________ of the ocean ____________
including sand bars, barrier islands, and sand spits
Landscapes
A _____________ on Earth’s ____________ with physical ____________,
such as ________, ____________, and ________________
The ___________ (__________________) and _____________ of the
landscape is determined by the ____________, ______________, geologic
_____________, and human activities
Topographic _______________ is the change in _______________ between
the _________ and the _________ places
Landscape Regions ___________________ landscapes have the greatest ___________ between
the highest ___________ and the deepest ____________
A great __________ of _______ types are common
____________ are common where _____________ tectonic _______
collide
Stream ______________ are __________, and the ___________
moving streams quickly __________ deep _________ between the mountain
peaks
_____________ landscapes are relatively _________ or ___________
uplands where streams have ________ deep ___________
Commonly underlain by flat layers of _________________ rock
Less topographic __________ than mountains but _________ relief
than the plains
_____________ have the least topographic __________
They may contain a _______ small ______, but are generally ______
and at ________ elevation
Commonly underlain by flat layers of _______________ rock
Climate Influence on Regions
___________, ____________ climates usually have ___________ landscapes
_________ are _________ as steep because moist climates promote a
protective cover of _________________
___________ cover _________ the soil from rapid ________ and
________
__________ (______) climates usually produce _______ soils with ______
humus
With _________ plant cover to protect the soil, _________ is carried
_________ during ____________
Large areas of __________ bedrock and ________ rock faces are the
result
Landscape Regions of the US
_____________ rocks will form ________ and __________
_____________ of the _____________ rock will make the major
___________
____________ will tend to follow zones of __________ rock and flow
__________
Human Activities Can Affect Landscapes
____________ and _______________ projects can accelerate ____________
and _____________ landscape development
______________ and ______________ must be guided in _____________
their projects by appropriate _______________ practices
Weathering, Erosion, Deposition, and Landscapes Outline -Teacher Guide (Key)© Lisa Michalek
Weathering The breakdown of rocks due to physical or chemical changes
Physical Weathering Changes the size and/or shape of a rock without changing the chemical
composition In frost action, water seeps into cracks in rocks. The water expands as it freezes
and makes cracks in the rock a little larger When the ice melts and the liquid evaporates, the rock is left more porous Over time, the freezing and melting in the cracks will cause the rock to
crumble Plant roots grow in rock crevices and gradually push the rock apart Animals that burrow beneath the ground will expose new rock surfaces to
weathering Abrasion occurs when rock particles are carried in water, they bump and rub
against other rocks
Chemical Weathering When rocks are exposed to the atmosphere and hydrosphere, they often undergo
changes in the chemical composition of rock, forming new substances Usually requires heat and water to bring about chemical changes
Therefore, it takes place more rapidly in warm, moist climates
Soil Formation Soil is a mixture of weathered rock and organic remains the usually covers bedrock The weathering of soil produces horizon layers
The top layer is usually the best for growing crops because it is rich in organic remains called humus
The next layer is usually mineral enriched from groundwater transporting minerals The lowest layer is composed of broken-up bedrock
Erosion of Sediments Sediments are rocks that have been broken into fragments Erosion is the transporting of sediments away from their place of origin and depositing
them elsewhere Gravity, water, wind, and ice erode sediments
Erosion by Water The smallest particles are carried in solution The largest and most dense particles are rolled or bounced along the streambed
Particles of low density, such as organic remains, are carried along the surface by flotation
Velocity of Streams The velocity of a stream is controlled by the slope and the amount of water flowing in the
stream (discharge) As the stream gradient increases, so does the velocity of the water flowing in the stream Velocity is also increased by an increase in the quantity of water in the stream There is a direct relationship between the velocity of a stream and the size of the particles
it can transport Large grains of sediment can only be eroded by fast-moving water Streams with broad, flat valleys often develop S-shaped curves called meanders At the bends in the stream, the fastest-flowing water swings to the outside of the bends,
causing erosion along the outer bank The slowest moving water stays to the inside of the bends, causing deposition
Erosion by Wind Wind can pick up loose rock materials, such as sand, silt, and clay, and carry them away Wind erosion occurs mostly in dry areas, such as deserts and beaches Sand blown by the wind can erode down material on a rock’s surface
Erosion by Ice If more snow accumulates in the winter than melts in the summer, the snow on the bottom
turns to ice If it becomes thick enough, its weight will cause it to move under the pull of gravity A glacier is a large mass of moving ice As a glacier moves, it carries, pushes, and drags loose rock material The glacier, with pieces of rock, smoothes, striates (scratches),
and grooves bedrock As a glacier moves through a valley, it will make a U-shape instead of a V-shape caused
by water When the ice melts, unsorted rocks and boulders are left scattered around on hilltops and
sides of valleys
Deposition When an agent of erosion deposits, or lays down particles and fragments of earth
materials (sediments) Also called sedimentation Most deposition takes place in water
Deposition Factors Particle Size
Smaller particles (clay and silt) settle more slowly than cobbles and boulders Particle Shape
Friction between water and the surfaces of particles slows down settling Smooth, rounded particles settle more slowly
Particle Density
Denser particles settle faster, less dense particles take more time to settle Settling Rate and Time
Sediments that settle at a faster rate require less time As the rate of settling increases, the settling time decreases
Sorting of Sediments Horizontal sorting occurs at the end of streams
The smaller sediments can be carried a greater distance from shore Vertical sorting occurs when a landscape dumps a variety of particle sizes in to still water
Deposition by Wind Usually sorts sediments by size Cross bedding layers meet a different angles
Deposition by Gravity At the base of a cliff, where pieces of weathered rock have fallen, you will find pieces of
many different sizes The sediments are not sorted
Deposition by Glaciers Occurs when a glacier melts and sediments are released Glacial erratics are large rocks that have been transported by glacial ice without being
broken into small particles They are often found high above stream valleys
Rounding and striations (scratches) indicate transport by glaciers
Alpine Glaciers Also known as valley glaciers, occur in mountain regions, and may carve out U-shaped
valleys with their moving ice
Continental Glaciers Also known as ice sheets causes sculpting of the land as rocks are carried within the
glacier or dragged under the flowing ice
Glacial Features Glacial Polish – when glaciers act like sandpaper, grinding the jagged edges from the
mountains and smoothing hard bedrock surfaces Striation – parallel grooves and scratches in the bedrock left by the rocks in the glacier Drumlins – accumulation of rock and soil that builds up in front of the flowing ice Moraines – where the ice front stops its southward advance, piles of unsorted soil and
rock remain Kettles – Low spots in the glacial deposits and places where large, buried ice blocks melt
leave these dry depressions and ponds called Kettle Lakes
The Oceans and Coasts Seawater covers almost 71% of our planet The average depth is about 4 km (3 mi) One Liter of seawater contains about 3.5% of dissolved solids
Sodium chloride (table salt) is the most common
When evaporation of ocean water causes the salts to become too concentrated to stay in solution, they are precipitated as sediment
The edges of the oceans are places of change caused by the action of waves and longshore currents
Beach sediments are rounded and reduced in size by abrasion as the energy in the breaking waves causes the particles to rub against one another
Sand is often transported along the beach and just outside the breaking waves in the zone of longshore transport
This movement of sand builds the features of the ocean shorelines including sand bars, barrier islands, and sand spits
Landscapes A region on Earth’s surface with physical features, such as hills, valleys, and streams The shape (topography) and composition of the landscape is determined by the climate,
bedrock, geologic structures, and human activities Topographic relief is the change in elevation between the highest and the lowest places
Landscape Regions Mountain landscapes have the greatest relief between the highest peaks and the deepest
valleys A great variety of rock types are common Mountains are common where converging tectonic plates collide Stream gradients are high, and the fast moving streams quickly erode deep valleys
between the mountain peaks Plateau landscapes are relatively flat or rolling uplands where streams have cut deep
valleys Commonly underlain by flat layers of sedimentary rock Less topographic relief than mountains but more relief than the plains Plains have the least topographic relief They may contain a few small hills, but are generally flat and at low elevation Commonly underlain by flat layers of sedimentary rock
Climate Influence on Regions Moist, Humid climates usually have rounded landscapes Slopes are not as steep because moist climates promote a protective cover of vegetation
Plants cover protects the soil from rapid runoff and erosion Arid (dry) climates usually produce thin soils with little humus With little plant cover to protect the soil, sediment is carried away during rainfall
Large areas of exposed bedrock and steep rock faces are the result
Drainage Patterns Harder rocks will form hills and ridges Erosion of the weaker rock will make the major valleys
Streams will tend to follow zones of weaker rock and flow downhill
Human Activities Can Affect Landscapes Farming and construction projects can accelerate erosion and effect landscape
development