Geologic Processes (2)

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Examples of Landforms
Plains, valleys, hills, mountains, volcanoes
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react with minerals to produce weak acids
Hydrogen ions in the H20
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2 types of geologic processes
Exogenous & Endogenous process
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occur on near the surface of the Earth
EXOGENOUS PROCESS
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natural occurrences that leave significant changes on the landscape, even in the ecosystem of an area.
EXOGENOUS PROCESS
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examples of exogenous process
weathering, erosion, mass wasting, sedimentation
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is the disintegration of rocks, soils, and minerals together with other materials through contact with Earth’s subsystems.
Weathering
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happens even without movement or transportation
Weathering
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2 types of weathering
Physical, chemical
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process by which rocks are broken into smaller pieces by external conditions.
Physical Weathering
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Types of physical weathering
Forst heaving & wedging, plant roots, Friction & Impact, Burrowing of animals, temperature changes
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Repititious freezing and thawing of water under patio
Frost Heaving
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causes the surface to heave when the ice expands under the patio and contract when ice melts
Frost Heaving
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water collects in rock crack, water freezes and expands, forcing crack to widen, Ice thaws, contracts and water gets deeper into cracks again, Repeated expansion and contraction causes further cracks till rock splits
Frost Wedging
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As the roots grow, they widen the cracks, eventually breaking the rock into pieces
Plant roots
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Trees can break apart even large rocks. true or false
true
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holes that expose new rocks to the efects of weathering
Burrowing of animals
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holes allow water and other weathering agents to reach the rock layer that had been covered by soil
Burrowing of animals
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repetition of cooling and heating over and over again
Temperature changes
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peeling away of large sheets of loosened rock materials
Exfoliation
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chemical reactions break the minerals in the rock into different materials
Chemical Weathering
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Types of Chemical weathering
oxidation, hydrolysis, Carbonation, Orgnaic acids, Acid rain
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process where iron combines with oxygen in the presence of water
oxidation
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chemical reaction between H+ and OH ions in water and the minerals in the rock
Hydrolysis
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The H ions in the water react with minerals to produce weak acids
Hydrolysis
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The reaction creates compounds which tend to be softer and weaker than the original parent rock material
Hydrolysis
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CO in the atmosphere dissolves in the droplets of water that make-up the clouds
Carbonation
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forms a weak carbonic acid
Carbonation
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reacts with certain rocks and minerals which include calcite, limestone, marble, chalk
Carbonic acid
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can make cracks in rocks and start the weathering process
Organic Acids
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Some living things produce acids that are released to the environment
Organic Acids
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example of orgnaic acids
Lichens, Mosses
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Pollution from the air contaminates the rain that causes rapid chemical weathering
Acid Rain
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the process by which Earth’s surface is worn away by wind, water, or ice.
Erosion
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it process moves rock debris or soil from one place to another.
Erosion
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Types of erosion
Geological and Accelerated erosion
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erosion caused by nature
Geological Erosion
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a normal process representing erosion of land in natural environment
Geological Erosion
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caused by the effect of rainfall, run-off, wind, topography, Atmospheric temperatures, gravitation process
Geological Erosion
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physical weathering occurs more quickly on a steep slope than on a gentle one
Topography
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gravity causes rock fragments to move down inclines
Gravity and Erosion
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movement of fragments down an incline, either be rapid or slow
Mass movement
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accumulation of fragments at the base of a slope
Talus
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may be reduced to smaller fragments through mechanical and chemical weathering
Talus
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erosion caused by human activities
Accelerated Erosion
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The potential for severe soil erosion and accelerated water runoff exists after a wildfire due to the lack of plant material to stabilize the soil.
Accelerated Erosion
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It is the movement of material on a downslope terrain due to gravity.
Mass Wasting
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usually happens in slopes, is dangerous, and may occur in areas that can trigger mass movement.
Mass Wasting
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can cause loss of life and injury, property damage, loss of capital assets, and interruption to economic activities.
Mass Wasting
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3 forms of mass wasting
Debris flow, Mud flow, Slump
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happens when a large amount of sediments (usually rocks of various sizes) fall downslope
Debris flow
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Unlike landslides, it does not need water to flow down.
Debris flow
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happens when combined soil and water flow downslope
Mud flow
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usually happens near rivers or streams where soils or sands are always moist or have been soaked in water for long time.
Mud flow
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is a slow downslope movement of loosely consolidated materials or rock and soil layers
Slump
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In time, the area would look curved because of the depression formed by the downslope movement of the land.
Slump
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The accumulation of materials (i.e soil, rock fragments, and soil particles) settling at the bottom.
Sedimentation
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Actually occurs in sediment in stream and sea erosion.
Sedimentation
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caused by forces from within or in the interior of Earth
ENDOGENOUS PROCESS
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The driving force is the thermal energy of the mantle and the crust.
ENDOGENOUS PROCESS
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responsible for earthquakes, movement of plates leading to development of continents, mountain building, volcanic activities, other movements related to Earth’s crust.
ENDOGENOUS PROCESS
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3 types of Endogenous process
Magmatism, Vulcanism/Plutonism, Metamorphism
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happens when magma is generated and develops into igneous(magmatic) rocks.
Magmatism
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take place either under the surface or on the surface to become part of the crust.
Magmatism
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very hot and is constantly moved by the internal heat that reaches the mantle of Earth through convection flow.
Magma
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layer where partial melting happens, origin of magma
asthenosphere (mantle)
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layer where magma rises
mantle
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Layer where magma differentiation in magma reservoirs (e.g. intrusion, stagnation, crystallization
Lithosphere (crust)
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Layer where intrusion and underplating happens
Moho discontinuity
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layer where volcanic erruption happens, entrusion of lava
Atmosphere (Troposphere)
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layer where volcanic gasses mix with the atmosphere
Atmosphere (Stratosphere)
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the process that usually happens after the magma is formed.
Vulcanism or Plutonism
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the magma that reaches the surface of Earth
Lava
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the process of changing the materials that make up a rock.
Metamorphism
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Types of Metamorphism
Contact and Regional Metamorphism
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a process when magma comes into contact with an existing rock and heat from the magma changes the structure and the mineral composition of the surrounding rock.
Contact Metamorphism
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It is a change in the structure, texture, or the chemical composition of a rock caused by a change of temperature or pressure over a large area
Regional Metamorphism
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are usually a result of the shifting of tectonic plates.
Regional Metamorphism
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