Get your Wikispaces Classroom now:
the easiest way to manage your class.
Pages and Files
English Do nows
English Vocabulary Homework
Global project Unit 1. Ancient Civilizations
Notebook Quarter Three
unit 1 ancient civilizations quiz answer key
UNIT FOUR global history notebook
Weathering and Erosion
Add "All Pages"
Weathering and Erosion
When the rock disintegrates into the water. Transportation of sediments.
Weathering is the breaking down of rocks at or near the surface of the earth.
Physically or chemically- The breakdown of rock into smaller pieces without chemical change.
If your lighting a piece of paper with a match or ripping a piece of paper - ripping the piece of paper would be a physical change.
- - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - - -
Ice Wedging (frost action)
- Water held in the crack of rocks wedges the rock apart when it freezes.
Root Wedging (plant action)
- Tiny roots grow into cracks in the rock and then as the root grows the rock splits.
When large masses of rock, mainly igneous, are lifted up to the surface the relief of overlying pressure causes the rock to expand. Upward expansions leads to curved breaks which may peel off in layers.
- The breakdown of rock through a change in mineral or chemical composition.
- The chemical reaction of oxygen with other substances. Iron is most easily attacked resulting in rust. (Iron Oxides)
- When carbon dioxide dissolves into water. It dissolves many common minerals.
Minerals Resistance To Weathering
- Different minerals and rocks ave different physical and chemical properties which allow them to weather at different rates.
- Almost unchanged by chemical weathering. It is hard and does not have cleavage so it also resists mechanical weathering.
FELDSPAR, MICA, CALCITE, AND GYPSUM
- Affected by both types of weathering and will break down into clay with calcite and gypsum dissolving and being carried of in solution.
Is the least resistant to mechanical weathering.
- Is the most resistant to mechanical weathering.
The type of cement which holds the sandstone together determines how resistant the rock is
- Low resistance
- High resistance.
Rocks which contain the mineral calcite, such as
calcite, are somewhat resistant to mechanical weathering but is the
least resistant to chemical weathering.
FACTORS AFFECTING RATE OF WEATHERING
The closer to the surface of the earth, the faster it will weather.
- Rate and type of weathering depends on exposure of rocks to air, water and the action of living things
The greater the surface area exposed to weathering the faster the rate of weathering.
Two samples of the same material having the same mass can have different surface areas. If one sample is a large piece of marble with a mass of 50g, and the other is 50g of many small pieces of marble. The smaller size pieces will have the greater surface area.
^ increase surface area by breaking it down into more pieces ^
Climate Effect On Weathering
Is usually greater in
Is usually greater in
(cold and warm)
Soil is made of loose, weathered rock and organic material in which plants with roots can grow. The rock material is composed of sand, silt, and clay.
- Parent material is the material from which a soil is formed.
- Soil that has the bedrock beneath the soil as a parent material.
- Soils formed from deposits left by winds, rivers, and glaciers.
Random; Most of the transported soil are in New York.
SOIL LAYERS: V
Darkest color due to organic material.
1.) Clay is washed to the subsoil
2.) May contain soluble minerals, such as calcium and magnesium carbonates.
3.) Color is usually red-brown from iron oxides that form above and wash down.
- Made of slightly weathered parent material (Rock Fragments)
-tropical soils form in areas with high temperatures and heavy rainfall. a thick infertile soil profile are results of heavy rain.
- grassland soils form in areas with enough rainfall for heavy grass, but not trees about 1 meter thick and fertile.
Forest soils form in humid regions with cool seasons. soil frofile is less then 1 meter thick with well developed A, B, AND C horizons.
desert soils form in very dry climates. soil profiles is a few centimeters thick and be very fertile when they are watered:
Arctic soils form at high elevations and high latitudes. poorly drained surfaces and the bottom layers are constantly frozen.
Movements of loose earth material down a slope.
Gravity is an aid in weathering and erosion. Steep slopes weather to gentile slopes.
Slow, imperceptible down slope movement of the soil. Causes objects that are fixed in the soil to lean downhill water in the soil is what adds the weight.
- the rapid movement of a water saturated mass of soil.
- occurs when a section of land moves downhill as a whole because of a plane of weakness in the underlying soil.
- sudden movement of a mass of bedrock or loose rock down the slope of a hill or mountain. (avalanche - snow, ice, rock and soil)
- is a pile of rock fragments at the base of a cliff.
-wind transports materials causing their particles to move in different ways
- a method of transport by which strong winds cause small particles to stay airborne for long distance.
- causes a bouncing of motion of larger particles. saltation accounts for most sand transport by wind.
Wind Erosion is greatest in arid climates with little vegetation.
- process of erosion found in wind, water, and ice. it occurs when particles such as sand rub up against the surface of rocks or other materials.
- rocks shaped by windblown sediments.
Wind deposition occurs in areas where wind velocity decreases.
- piles of windblown sand that have a gentle side and a steep side.
The gentler slope occurs when the side on which the wind is blowing. the steeper slope occurs on the side protected from the wind.
- thick deposits of fine lightweight particles that are carried by the wind in great quantities of long distances. they are some of the most fertile soils.
Louis Agassiz is known for the idea that glaciers once covered many parts of the world.
- accumulations of ice larfe enough to survive summer melt0 forms from snow under pressure which turns to ice.
- the lowest level that permanent snows reach in summer.
Firn- granular ice material formed in snow fields from freshly fallen snow becoming compressed and re crystallizing.
-the lower layers become ice and begin flowing down or outward because of overlying pressure.
- occur in mountain regions above the snow line
- flow downhill and carve out U-shaped valleys.
- a glacier that spreads over a wide geographic area. form in polar areas where the snow line is close to sea level and wide areas are above the snow line.
- 20,000 years ago, new york state was covered by huge ice sheet that originated in canada.
- the overlying weight of snow and ice causes grains of ice to partially melt and refreeze. as the happens ice grains slip past each other and move downhill.
- glacier movement more rapidly at the surface than at the base and faster at the center than at the sides. friction with the valley walls slow the flow.
Crevasses- cracks across the width of the glacier that form when glaciers move over steep slopes.
Ice front is the end of a glaciers
-the ice front is stationary as long as the rate of movement and melting are equal
-A glacier recedes when it melts faster than normal
-a glacier advances when the rate of movement is greater then the rate at which it melts.
Pieces of rock are picked up as glaciers move and then dragged along the bedrock and/or valley wall.
-fine sand acts as sandpaper and polish the bedrock
-larger sediments leave long parallel scratches called striations
Calving- when blocks of ice break off into the sea
-The finger lakes of NY were formed as advancing ice deeply scoured out valleys.
-Glacial trough are formed when a glacier carve out a valley forming a u-shape valley.
- valley glaciers leave sharp mountain tops while continental glaciers leave rounded tops.
HERE ARE A FEW DEPOSITIONAL FEATURES OF GLACIERS.
-Moraine is a glacial deposit of unsorted rock material.
Ground moraine- carried along the bottom
lateral moraine- lonh lines of rock pieces along the valley sides
Medical moraine- when two glaciers come together and there lateral moraines join together.
a half-open steep-sided hollow at the head of a valley or on a mountainside, formed by glacial erosion
arete- a sharp mountain ridge
horn- a hard permanent outgrowth, often curved and pointed, found in pairs on the heads of cattle, sheep, goats, giraffes, etc., and consisting of a core of bone encased in keratinized skin.
tarn- small lake at the base of a cirque
hanging valley- a valley that is cut across by a deeper valley or a cliff.
crevasse- deep open crack.
roches moutonees- outcrop of bedrock which has become elongated. sculpted by a glacier one side smooth and the other is left rough.
striations- marked with straie
drift- be carried slowly by a current of air or water
an unstratified sediment consisting of particles of various sizes and deposited by melting glaciers or ice sheets.
forms along the side of a glacier
media merging lateral moraines of two glaciers form a moraine in the middle of the glacier.
ground- a melting glacier deposits till in a thin layer over a broad area.
recessional- deposits of till that form at the end of a glacier as it retreats.
terminal- the end found at the farthest advance of a glacier
- material carried away from a glacier by meltwater and deposited beyond the moraine.
- a steep-sided mound of sand and gravel deposited by a melting ice sheet.
- a vessel, usually made of metal and with a handle, used for boiling liquids or cooking foods; a pot.
- a low oval mound or small hill, typically one of a group, consisting of compacted boulder clay molded by past glacial action.
- finely powdered rock formed by glacial or other erosion.
- not even or regular in pattern or movement; unpredictable
: her breathing was erratic.
- a long ridge of gravel and other sediment, typically having a winding course, deposited by meltwater from a retreating glacier or ice sheet.
Erosion and Deposition
Erosion- the process by which earth materials are moved by natural agents like water, wind, and ice.
Running water is the most effective agent of erosion.
is where running water gets its' energy.
Rocks are both weathered both Chemically and Physically by running water.
- the rerm given to the use of sand, pebbles, and even boulders as cutting tools to grind away at the steam bed. during this process the "tools" themselves wear down.
- water dissolves soluble minerals.
Rivers carry rock material in three ways.
this is material that is dissolved from the bedrock. most commonly found in solution are compounds of calcium and magnesium.
when small rock particles, such as clay silt and fine sand, are kept from sinking by the turbulence of the stream. this gives the water a muddy look.
- sand, pebbles, and some boulders which move along the stream bed.
is indicated by both the total amount sediment in a stream and by the size of the particles being moved.
The stream discharge and speed will determine the carrying power of the stream.*
- volume of water flowing past a given point at a given time
- generally determined by the steepness, or gradient, of its bed.
- a stream moving at high speed with a high discharge can carry much larger sediments then a slow moving stream. Example: spring time snow melting and excessive rain.
The Rover Valley
Rivers tend to have a
valley because they tend to flow at high speeds and dig into the stream bed.
is the lowest level a river can cut into its bed.
-To form a permanent stream rain water must flow down a slope and dig deep to cut into the water table. this wearing away of the land to form a stream valley is called headward erosion.
V-SHAPED VALLEY ! VVVV
-A Divide is an area of high land that separates one river valley from another.
-On either side of a divide a river system may form.
is all of the land that drains into the river either directly or through its tributaries.
Water flowing over a steep cliff will result in a waterfall. waterfalls are not permanent structures.
is the erosional process occurring at the base of a waterfall. here water carrying sediment plunges down and back into the stream bed and cliff below. this causes the rocks at the top of the falls to overhand. over time this overhand will collapse and the stream will move back towards its source.
Deposition occurs when a stream either decreases in speed or discharge.
- generally the speed decreases when its slope decreases or its bed widens. The greatest loss of speed occurs when a river empties into a quiet body of water.
- a decrease in discharge would occur if a river traveled through an area with low precipitation.
-as rivers begin to decrease their slope they move slower and will begin to move side to side.
- as the valley wall on either side is eroded the valley floor is widened.
is the widened valley floor area which will accumulate water during times of excess rain when the river floods.
Erosion and Deposition in a River
are broad curves in the river.
(each bend or turn)
- Erosion is greatest on the outside of a meander where water is flowing the fastest.
- deposition is greater on the inside of the meander where the water flows slower.
this is called an oxbow lake:
Meanders can only become so before they break through into another meander. the river then deposits mud and silt along the end of the abandoned meander. The now separated meander becomes a lake.
Running Water Deposits Well- Sorted particles
- when sediments are suddenly deposited into water. the particles separate by size with the largest on the bottom and smallest on the top.
the larger and rounder usually settle in to the bottom.
- when rivers empty their sediments into quiet bodies of water. particles are sorted by size with larger particles being found closer to the shore and smaller particles being carried out into the body of water to be deposited.
the first particle to be deposited is going to be the largest one.
: a fan-shaped deposit of sediment at the mouth of a river.
River Deposition- rivers deposit their bed load when they slow down. This can occur in these ways.
-slope of land decreases
-stream channel widens
-stream empties into a lake or ocean.
A stream that flows year-round because its bed lies below the water table, or because more water is supplied from upstream than can infiltrate the
A stream is a flowing body of water with a current, confined within a bed and stream banks. Depending on its locale or certain characteristics
source - the fouintain head of a stream where water begines to folw
mouth- the opening of a stream where it empties into another water body
tribuatry- any stream that flows water to another stream
watershed-an area or region drained by a river
channel- the area of a valley occupied by running water
valley- any low writing land bounded by higher ground
meanders- a winding curve or bend of a river
valley- any low writing land bounded by higher ground
meanders- a winding curve or bend of a river
help on how to format text
Turn off "Getting Started"