Erosion + Weathering + Mass Wasting Flashcards

1
Q

Mechanical Weathering

A

Physical disintegration and
reduction in size of the rocks, but it doesn’t change the rocks chem. composition.

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2
Q

Exfoliation w/ Mech. Weathering

A

When rock layers peel off in sheets due to temp changes. Kinda like the outer layer or skin of a brown onion

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3
Q

Exfoliation Process w/ Mech. Weather

A
  1. Daytime heat makes outer rock expand
  2. Cool nights contract it
  3. This repeats over time and the rocks outer layer eventually peels

Common in deserts/mountains, where temp. swings are common/large

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4
Q

Process of Frost Wedging (sometimes Freeze-thaw weathering) w/ Mech. Weather

A
  1. Water enters cracks in rocks
  2. At night it freezes and expands (which expands the size of the crack)
  3. It melts during the day, and more water can now enter that crack
  4. Over time, this will eventually break the rock from the inside.
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5
Q

Process of Salt Wedging w/ Mech. Weather

A
  1. Salty water enters rocks cracks
  2. When the water evaporates, it leaves salts behind
  3. The salt crystals grow/expand (puts excessive pressure on the rock)
  4. Over time, this will eventually break the rock from the inside.
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6
Q

Process of Thermal Stress Weathering w/ Mech. Weather

A
  1. The rocks expand when they get hot during the day
  2. It contract as it cools during the night
  3. The stress from this constant expansion + contraction weakens the rock.
  4. Over time, pieces break off

Common in deserts/mountains, where temp. swings are common/large

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7
Q

Process of Abrasion w/ Mech. Weather

A
  1. Rocks grind against each other (from wind, gravity, or water movement).
  2. From friction, fragments scrape off or edges become smoother.
  3. Over time, rocks are worn down, broken, or rounded without any chemical change.

diff bw this and abrasion in erosion is this happens in the same spot, abrasion in erosion happens through other means

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8
Q

Chemical Weathering

A

Chemical weathering decomposes, dissolves, alters, or weakens the rock through chemical processes, which changes their composition over time, forming residual materials

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9
Q

Carbonation w/ Chem. Weather

A

When CO2 reacts w/ rainwater or moisture in the surrounding environment to produce carbonic acid, a weak acid that reacts w/ carbonic bedrock to form karst landscapes.

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10
Q

Where does Carbonation (w/ Chem Weather) usually occur and why

A

Its more common in humid, warm climates because higher temperatures and moisture accelerate the chemical reactions, but it can also occur in wet, moist conditions where there is plenty of water to dissolve carbon dioxide.

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11
Q

Hydrolysis w/ Chem. Weather

A

The breakdown of rocks and minerals due to interactions with water. The new compound tends to be softer/weaker than the original parent rock material.

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12
Q

Hydrolysis Process w/ Chem. Weather

A
  1. Water reacts with minerals in the rock
  2. Chemical reactions occur, where water breaks down original minerals into new minerals
  3. The rocks composition then changes, which weakens and breaks it down over time
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13
Q

Whats some extra stuff to know ab Hydrolysis

A
  1. It can also cause certain minerals to expand; facilitates mech. weathering
  2. Usually affects igneous rocks (bc they’re composed of silicate materials) which readily combine with water
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14
Q

Hydration Process w/ Chem. Weather

A
  1. Water molecules combine with minerals in rocks.
  2. The rock then expands or changes into a softer mineral.
  3. Over time, the rock weakens and/or breaks apart.
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15
Q

Whats the difference between hydration and hydrolysis.

A

In Hydration: - Water is added
- Minerals change from (swells/weaken)
In Hydrolysis: - Water reacts chemically
- New minerals are created

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16
Q

Oxidation w/ Chem. Weather

A

Oxygen and water react with iron-rich minerals, weakening it. It accelerates rock decay.

Oxidation weakens the rock, then other weathering processes breaks down the rock fully.

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17
Q

Hydraulic Action w/ Erosion

A

Water repeatedly hits like a rock or sum shit similar and over time, the waves wear down the rock into sediments.

Like a hose spraying at dirt on a wall, but over a long period of time

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18
Q

Abrasion w/ Erosion

A

Movement agents (wind, water, ice) carries particles, which scrape against rocks surfaces, which ends up wearing and eroding the rock over time.
Sometimes, rocks are carried by waves/ the ocean, and they hit cliffs, eroding them over time.

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19
Q

Corrosion w/ Erosion

A

Refers to chem. erosion, where water dissolves minerals from the rock, particularly in areas with soluble rocks, and ends up transporting them away

20
Q

Attrition w/ Erosion

A

A process where rocks and sediments become smaller, rounder, and smoother as they rub/collide/break down during transportation by water or wind.

21
Q

Biological Weathering

A

The disintegration/decay of
rocks and minerals caused by chemical or physical agents of organisms.

22
Q

Explain organic activity from Lichen and Algae w/ Biological weathering

A

Organisms (like lichen and algae) live on bare rock, extracting minerals from it through ion-exchange mechanisms. Because the rocks minerals has been leached off, it then weakens/breaks it down.

23
Q

Explain organic activity from Decaying plants w/ Biological weathering

A

The decaying of plant materials can also produce acidic compounds which dissolve the exposed rock

The presence of organisms growing/ expanding/moving across the surface of the rock exerts a small amount of abrasion and pressure, that gradually causes the mechanical weathering of the rock as the organisms extract various minerals.

24
Q

Biological Weather. w/ plant roots

A

When plant roots penetrate into cracks/crevices of rocks and causes it to split/break into smaller particles through mech. weathering.

Its the most common form of bio weather, its a very gradual process, and fairly effective at breaking rocks w/ pre-existing weakness (fracture, fault, joint)

25
Biological Weather. w/ Organism Activity (Burrowing and Tunnelling)
Some organisms (small animals, worms, termites, and other insects) tunnel into rocks or cracks in rocks, causing it to breakdown and disintegrate.
26
Biological Weather. w/ Organism Activity (Acid secretion)
Some organisms (snails, barnacles, limpets) attach themselves to rocks and secrete acids that chemically dissolves the rocks surface.
27
Differential Weathering
Refers to the different rates of weathering due to different types of rocks, textures, or other characteristics. Contributes to unique formation of many landforms, like pedestals, waterfalls, and monadnocks
28
What 3 factors cause differential in weathering
1. The type of weathering process (mechanical, chemical, biological) 2. The rock that is being weathered and its properties (some rocks are more durable/resistant to weathering than others) 3. Climate (if talking about same kind of rock) --> e.g Limestone weathers quicker in wet climates than in dry climates.
29
Water (Fluvial) Erosion
Water erodes rocks + shapes the landscapes by removing and transporting weathered materials from their source, to another location where they are deposited, and either stored or transported to another location.
30
Rain Splash Erosion w/ Fluvial Erosion
Occurs when the impact of a rain drop loosens and mobilises particles.
31
Sheet Erosion w/ Fluvial Erosion
A process where particles loosened by rain-splash erosion are transported by runoff water down the slope of a surface.
32
Rill/Gully Erosion w/ Fluvial Erosion
When water concentrates during sheet erosion and erodes small rills or gullies into the surface that channel the flow downslope.
33
What landscapes are formed by Fluvial Erosion
V shaped River valley Fluvial forms pathways for surface and groundwater flow and carves v-shaped river valleys that continue to erode, transport, and deposit weathered sediments across the landscape.
34
Wind (Aeolian) Erosion
Wind erodes materials by picking them up and temporarily transporting them from their source to another location where they are deposited, and either stored or re-mobilized and transported to another location.
35
Deflation Erosion w/ Aeolian Erosion
Movement or transport of particles through the air or along the ground
36
Abrasion Erosion w/ Aeolian Erosion
When wind-driven particles wear down and shape the landscape by scraping and grinding against rock surfaces. Has to be wind driven, otherwise it isn't aeolian erosion
37
Ice (Glacial + Periglacial) Erosion
When particles are incorporated into glacial ice through plucking, then are transported downslope within the glacier. The friction + abrasion of the ice and rock moving across the bedrock erodes the surface of the bedrock and often leaves scrapes, grooves, striae, or polished rock surfaces.
38
Gravitational Erosion
Gravity facilitates the down slope transportation of loosened, weathered materials and enables them to move without movement agents, However, these agents can act as catalysts for gravity related erosion.
39
Rock Falls w/ Mass Wasting
Rocks dislodge b/c their ∆ potential energy is too much to maintain, so pot. energy --> kinetic energy, which causes the rock fragment to fall, restoring equilibrium. forms talus or scree.
40
What aids/causes Rock Falls
The rocks may be loosened by a recent rainfall or snow melt-water event that facilitates the movement of the rock (before they fall from the force of gravity)
41
Landslides w/ Mass Wasting
Mass-wasting events where large amounts of weathered rock material slide down a hill slope or mountain side primarily by gravity related erosion.
42
What aids/causes Landslides
Nearly all landslides are triggered by an earthquake, or lubricant agent such as rainfall, or a snow or ice melt-water event. During intensive rainfall, soil and weathered rock material become unstable and loosened from the saturated conditions that separate the individual grains and other material fragments. The increased fluid pressures coupled with the loosened materials succumbs to gravity related erosion and the weathered materials plunge downhill as a powerful landslide.
43
Debris and Mud Flows w/ Mass Wasting
When heavy rainfalls produce large amounts of runoff that transport eroded soils, sediments, and plant debris down slope where the flows eventually spreads out across valley bottoms. Sometimes the debris and mudflows follow existing drainage paths and other times they carve out new paths as they flow downhill
44
Slump w/ Mass Wasting
A fairly common form of mass wasting where the rock or soil collapses, breaks off from the hill, rotates slightly, and slumps/falls downhill.
45
Creep w/ Mass Wasting
Creep is the slowest mass-wasting process and involves a very gradual downhill movement of soil, bedrock, and weathered rock fragments. Usually, the entire slope is slowly creeping downhill as a complete unit. Creep processes occur to some degree on nearly every hill slope because of gravity
46
With Creep, what accelerates it and what is it evidenced by
Creep is evident by bent or extended tree trunks that are adjusting to the slow movement of the soil, regolith, and weathered material they are rooted into. Freeze-thaw cycles and saturated conditions may accelerate creep processes but usually only for a short time-period.
47
Deposition
Deposition is a constructive process that lays down or places weathered and eroded materials in a location that is different from their source. Its applied to any consolidated or unconsolidated materials that have accumulated as a result of some natural process or agent. Deposits can result from all kinds of weathering, and water, wind, ice, or gravity-related erosional processes