Weathering and Erosion
Weathering is the gradual breakdown of pre-existing rock due to natural processes. These processes can be very quick, but some may take thousands of years to occur.
Rocks are weathered by their exposure to the elements- like rain, freeze and thaw and acid rain! They are broken into smaller pieces, and then can undergo chemical changes. Erosion is the process of moving these weathered materials.
A lot of incredible landforms are made by these processes.
Physical weathering is processes that break down the rock without changing the chemical composition.
|Half-dome in Yosemite Park is a great example.|
Plant and Animal Action-
Animals also have an effect on rocks. The most common effect posed by animals is burrowing, or creating tunnels under ground. Ants, worms, weasels, mice, etc.. can all create an extensive tunnel system. These tunnels allow water and air to reach points below ground, and begin the weathering process.
Humans have a dramatic effect on rocks. Human technology has allowed us to level mountains, cut out roads and tunnels.
To find physical plant weathering look for growing vegetation on top of rocks.
Changes in temperature-
As a rock is heated by the sun, its temperature can increase dramatically, and at night it cools down. As this process occurs over and over again, the bonds of the rock molecules can break, leading to cracks in the rock. These cracks then allow a path for other agents of weathering. This form of weathering looks exactly like ice wedging in this region of the world. If you lived down south the extreme head would play a bigger part in weathering rocks.
Chemical weathering is the breakdown of rock through changes in its chemical makeup. These changes either break down the rock or weaken the rock to allow for physical weathering.
The atmosphere is composed of 21 percent oxygen. When oxygen combines with an iron rich rock, a process called oxidation occurs. The result is iron oxide. This reaction does not weather the rock. If, however, water is present at the time of oxidation, the result would be rust.
The result is much the same as an iron nail. When these bonds are rearranged, the bonds of the rock are weakened. If you compare a rusty nail to a regular nail, the unweathered nail is much stronger.
To find oxidation look for the tell tale signs of orange or red rust on cars, rocks and metal objects outside.
Slick Rock in Utah are the favorite red rocks ride of moutnain bikers. The rocks are rustier than the bikes in this climate.
Dissolving a rock in water is yet another form of chemical weathering. It is called solution. Solution occurs when compounds are dissolved into water. Halite, gypsum, and limestone are most susceptible to solution. Most compounds are at least slightly soluble in water, so water is called the universal solvent.
Dissolution is difficult to discern without lab equipment.
Carbonic acid can devastate rocks made of calcite. Rocks such as limestone and dolomite can be entirely dissolved, leaving extensive caverns. In states with bedrock composed of calcite, such as Florida this process can cause extensive damage to structures above. Often, caverns are cut out of the rock, the structures on top are heavy, and everything on top collapses into the cavern, leaving what is called a sinkhole. This sinkhole can swallow many houses at a time.
|Sea Caves form from Carbonation. A sea cave was featured in the movie Cast Away. For more on Sea Caves click here.|
Normal rain is at a pH of 5.6. Plants and animals love it. Pollution from cars, factories, and coal burning plants are creating rain so caustic that sometimes it rains at pH of 4. If an entire lake was that pH, it would be crystal clear but lifeless.
To see the effects of acid rain, find a lifeless pond of water or go to a cemetery and find a grave stone that is very, very worn- chances are it is made of limestone or marble both of which are made of calcite which dissolve in acid (remember our HCL test?).
Plants decompose into a weak acid that can help break down rocks such as limestones and marbles.
A sure way to find rocks that are decomposing by organic acids is to find a rock with either moss or lichen on it.
Climate, which is usually measured in terms of temperature and moisture, can drastically affect the rate and type of weathering. In an area with cold temperature, for instance, frost wedging would be the dominant form of physical weathering. Chemical weathering occurs most rapidly in a hot and moist climate. In New York, the climate can range from hot to cold. Hot moist summers and cold winters make for a climate that promotes weathering.
The particle size of the material can affect the rate of weathering. The smaller the particle size, the faster it will weather. The more surface area that is exposed, the more it will weather.
Rock that is exposed to the atmosphere tend to weather much quicker. Bed rock that is covered by soil and vegetation may not weather as quickly.
All chemical and physical properties are determined by the mineral composition of the rock. Mineral composition is more important in determining the rate of chemical weathering. Those minerals that are most reactive with acids, water, and air are weathered at a more rapid rate.
Mineral composition also affects physical weathering. Minerals that are soft (hardness lower thaan six) can be easily abraided and blasted.
Weathering is a slow process. When we speak of time in a geologic sense, millions of years are often used as the units. The bedrock of Greenland has barely been weathered, and its age is over 3.5 billion years. The longer that a rock has been exposed to the weather, the faster it weathers.
The rock that soil comes from is called the parent rock, and soil that forms from the bedrock directly below is called residual soil. If the soil is from material that was transported, the soil is called transported soil. Transported soil often has a different composition that the bedrock directly below.
Cool landsforms like this one in Arches National Park Utah are from wind and water weathering of soft rock.
Erosion is the movement of weathered rock. Streams, waves, floods, and winds are just a few of the agents of erosion. Glaciers can erode as well as well as gravity that continues to bring sediments downhill.
Mass wasting is the downhill movements of material due to gravity. This type of movement is going on at all times on most hills, but at different rates . As the slope of the material increases, the rate increases. The steepest slope at which the material will remain stable is called the angle of repose. Size, density, and shape of particles determine the angle of repose. As the slope's angle increase past the angle of repose, the slope becomes unstable, and mass wasting occurs. If the angle is slightly above the angle of repose, mass wasting is slow, as in hillside creep. If the angle is great, then slides may occur.
Types of mass wasting-
Rockfall- rock falls occur when large fragments of rock either fall from a cliff, or bounce down the side of a hill
Rockslides- rock slides occur on slopes that are less steep when rocks slide down the entire slope, rather than falling through the air.
Slump- a process in which a mass of bedrock or soil slides down a slope in one large mass. The mass slides down a curved plane of weakness. The slump block rotates and comes to rest tilted toward the cliff.
Mudflow- mudflow is the rapid, downhill flow of a fluid mixture of rock, soil, and water. Mudflows generally occur when there are long periods of rainfall, and the water content of the soil builds up. The watery soil runs downhill, and thickens up as it travels downhill and picks up rocks and soil.
Erosion by Moving Water
All precipitation that is not absorbed by the ground is called runoff. Runoff can sometimes transport sediment, and often ends up in streams.
Streams are bodies of running water that flows under the influence of gravity. The running water cuts into the surface of the earth, building a channel. This channel is surrounded by a bank on either side.
Material that is carried by water is called the stream's load. The faster a stream, the larger the load. A slow moving stream does not have the energy to carry a large load. Large sediments are usually dragged or pushed, a process called traction. Saltation is when particles bounce along the stream bed. Suspension is the process of sediments picked up by the stream. When rocks are dissolved, they are said to be carried by the process of solution.
When the load of a stream is a resistant rock, it can abraid the surface of bedrock. This prolonged scratching can gouge rock, and eventually a canyon can be formed. The Grand Canyon was created in this manner.
Steam Velocity Lab
As the stream gradient increases, the stream velocity _Question 1_.
As the volume of water in a stream increases, the velocity of the stream _Question 2__.
The majority of the water in any stream will eventually end up on the earth's oceans. The ocean's waves can be very destructive. Formations such as sea cliffs, caves, stacks, and terraces may result. Oceanic waves cause longshore drift (longshore currents), which can move sediments along the coast.
Deflation is the process of wind picking up sediment and transporting it. Abrasion is the process in which wind blown sediments collide and wear rocks down.
When deflation is concentrated, a deflation hollow is formed. There are thousands of such hollows on the Great Plains. In wet years, they fill in with grass or water. In dry years, the grass dies, exposing the hollow to even more deflation.
When deflation occurs in the desert, the water table may be exposed. Vegetation forms around the hollow, and an oasis is formed. After deflation occurs for a period of years, only the objects that could not be transported by wind are left, usually large particles. An area with only these particles left is called desert pavement. Large particles that are exposed to abrasion become ventrifacts. The rock has a flattenned, pitted surface where it was exposed to abrasion by wind.
As sand travels through the desert, being eroded by wind, dunes start to form. The gradual slope that sand is blown along is called the wind face. The steep slope that faces away from the wind is called the slip face.
How does sediment behave when it is deposited in water?
The densier, rounder and larger sediment the faster it falls.
When a sediment laden stream or river enters a lake or ocean, the larger sediment is deposited near the shore with smaller sediments falling out of the water colum further offshore.
When a stream is recently formed, it generally flows quickly. The stream wears a long v-shaped valley into the ground.
In a mature stream, the slope gets eroded over time, and the slope becomes much less steep. The water flows more slowly and sediment accumulates at the bottom of the valley. Water flows around obstacles, rather than over them, and the stream's path forms curving loops called meanders. If the river overflows, the water slows down, deposits its load, and a broad flat floodplain is formed.
Old Age Streams
In an old stream, a large peneplain is formed. This is the area that used to be the floodplain, that had the stream meander though it. This peneplain has oxbow lakes and cutoffs.
When a stream meanders, the outside of the meander is heavily eroded. Thats where you can find cliffs. The inside of the meander is where a sand beach can be deposited. The water moves faster toward the outside of the bend because of the water's inertia. Because the water can't "turn" it bashes into the far side. Meanwhile, the water on the inside of the bend is moving slower. Heavier sediments will fall out of the stream creating a great flat beach to camp on!
Glaciers form after long periods of snowfall, usually in the mountains. After many meters of snowfall, the snow at the bottom begins to recrystalize under the great pressure caused by the weight of the overlying snow. As the snow begins to crytalize into solid ice, the pressure continues to increase. This squeezing motion forces the ice to begin flow as a liquid.
As glaciers move along, the bottom melts, and refreezes. As this occurs, the rocks and sediment lying under the glacier are picked up and frozen into the ice. This process is called plucking. Sediments the size of boulders can be plucked and carried thousands of miles. Sometimes a plucked scraps on the bedrock as the glacier grids slowly onward. This causes deep grooves in the rock called glacial scratches.
As the glacier begins to recede, or melt, it deposits these sediments. Boulders that are not native to the area that they are deposited on are called Erratics. Large holes or depression that are plucked by glaciers are called Kettles. The sediment that is pushed by the glacier, similar to a bulldozer, is then deposited as the glacier recedes. This is called Morraine. Long Island is one long morraine deposit from a bulldozing glacier 11,000 years ago. Glacial deposited sediments are unsorted.