Geology Chapter: Weathering and Erosion
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Questions and Answers

What geological process involves the movement of weathered rock fragments?

  • Lithification
  • Weathering
  • Erosion (correct)
  • Deposition

Which statement best reflects the principle of uniformitarianism?

  • Geological changes occur at a uniform and predictable rate.
  • Understanding current geological processes helps interpret past events. (correct)
  • The Earth's landscape is primarily shaped by catastrophic events.
  • Geological processes happening today are different than those of the past.

What is the primary agent of change in the formation of stream valleys?

  • Earthquake tremors
  • Volcanic activity
  • Erosion by water (correct)
  • Glacial movement

Which geological process breaks down rocks into smaller pieces?

<p>Weathering (D)</p> Signup and view all the answers

What is the final step in the geological cycle that involves the accumulation of transported materials?

<p>Deposition (C)</p> Signup and view all the answers

Which principle states that sedimentary rock layers are originally laid down horizontally?

<p>Law of Original Horizontality (C)</p> Signup and view all the answers

Which geological principle helps determine the relative age of rock layers based on their position?

<p>Law of Superposition (A)</p> Signup and view all the answers

What are unconformities in geological terms?

<p>Gaps in the rock record (A)</p> Signup and view all the answers

What aspect of erosion varies based on location?

<p>The rate of erosion (D)</p> Signup and view all the answers

Which form of erosion is generally faster than wind or glacial erosion?

<p>Water erosion (B)</p> Signup and view all the answers

What primarily characterizes the youth stage of a stream valley?

<p>A steep gradient, fast-flowing water, and downward erosion. (D)</p> Signup and view all the answers

Which feature is indicative of the maturity stage of a stream valley?

<p>A floodplain. (A)</p> Signup and view all the answers

What distinguishes the old age stage of a stream valley?

<p>A broad, flat valley with a low gradient. (A)</p> Signup and view all the answers

What is the relationship between the base level of a stream and the sea level?

<p>The sea level represents the ultimate base level. (B)</p> Signup and view all the answers

How does a local base level impact stream erosion?

<p>It creates temporary stagnation, reducing erosion. (D)</p> Signup and view all the answers

What is the primary difference between bedrock and alluvium?

<p>Bedrock is solid rock, while alluvium consists of loose sediments. (A)</p> Signup and view all the answers

"Stream power" refers to:

<p>The rate of energy loss on a channel bed causing erosion. (C)</p> Signup and view all the answers

How does plucking contribute to bedrock channel formation?

<p>It removes large chunks of fractured rock. (A)</p> Signup and view all the answers

What distinguishes an anastomosing channel from other alluvial channel types?

<p>It comprises a network of interconnected streams. (C)</p> Signup and view all the answers

How are oxbow lakes formed?

<p>From the cutoff of a meandering stream loop. (D)</p> Signup and view all the answers

What geological process contributes to the formation of sedimentary rock from groundwater?

<p>Sediment cementation (C)</p> Signup and view all the answers

What consequence can occur when groundwater is excessively pumped out?

<p>Creation of sinkholes (B)</p> Signup and view all the answers

Which underground features are formed by groundwater dissolving rock?

<p>Caves (B)</p> Signup and view all the answers

What is the primary factor determining how much water soil can retain?

<p>Porosity (D)</p> Signup and view all the answers

In which type of aquifer is water trapped by impermeable layers?

<p>Confined aquifer (C)</p> Signup and view all the answers

Which factor does NOT affect the quality of spring water?

<p>Temperature of the aquifer (D)</p> Signup and view all the answers

How does gravity influence groundwater movement?

<p>By directing flow downhill (D)</p> Signup and view all the answers

What is the main characteristic of an unconfined aquifer?

<p>Water exits through surface depressions (C)</p> Signup and view all the answers

What does the permeability of soil describe?

<p>How quickly water passes through (A)</p> Signup and view all the answers

Which process can lead to the formation of natural springs?

<p>Aquifer leakage (B)</p> Signup and view all the answers

Flashcards

Weathering

The process of breaking down larger rocks into smaller pieces due to wind, water, and glaciers.

Erosion

The transportation of rock fragments from one location to another by natural agents like wind and water.

Deposition

The accumulation of eroded materials in a new area, forming new landforms.

Uniformitarianism

The principle that current geological processes can explain past geological events.

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Law of Original Horizontality

Layers of sediment are originally deposited horizontally under the action of gravity.

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Law of Superposition

In undisturbed layers, the oldest layer is at the bottom and the youngest is at the top.

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Crosscutting Relations

If a geological feature cuts through another, it is younger than the one it cuts.

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Unconformities

Gaps in the geological record where rock layers are missing due to erosion or non-deposition.

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Stream Valley

A depression formed by streams due to erosion of surrounding land.

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Aging Process of Stream Valleys

The changes a stream valley undergoes over time, shaped by continuous erosion.

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Stream Valley Aging Stages

The three stages are youth, maturity, and old age, each with different characteristics.

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Youth Stage

Characterized by steep gradient, fast flow, V-shaped valley, and downward erosion.

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Maturity Stage

Less steep gradient, slower water, U-shaped valley, and floodplain development.

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Old Age Stage

Extremely low gradient, broad flat valley, very wide slow-moving stream.

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Base Level

The lowest point to which a stream can erode, affects erosion and deposition.

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Ultimate Base Level

The sea level, the ultimate low point for stream erosion.

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Local Base Level

Temporary low points like lakes or dams where water can stall.

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Bedrock

A solid rock foundation often covered by loose soil and sediments.

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Stream Power

The rate of energy loss on a channel bed that causes erosion.

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Alluvial Channels

Changing river channels formed by erosion and sediment deposition over time.

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Groundwater

Water that seeps into the Earth's crust through rock and sediment.

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Porosity

The capacity of soil to hold water in its pore spaces.

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Permeability

The speed at which water passes through soil or rock.

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Gravity's role

Gravity pulls water downward, affecting its flow direction.

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Aquifers

Subsurface water reservoirs formed by saturated porous units.

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Confined Aquifer

An aquifer trapped between impermeable layers of rock.

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Unconfined Aquifer

An aquifer that is open to the surface and not trapped.

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Natural Springs

Points where groundwater flows to the surface.

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Sinkholes

Funnel-shaped holes that form when groundwater is removed.

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Water Quality

The purity and safety of water for consumption.

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Study Notes

Weathering, Erosion, and Deposition

  • Weathering breaks down large rocks into smaller pieces. This occurs due to wind, water, and glaciers.
  • Erosion transports these broken rock fragments from one location to another. This is done by agents like wind, water, and glaciers.
  • Water erosion is typically faster than wind or glacial erosion.
  • Deposition is the accumulation of eroded materials in new areas.
  • These processes shape landscapes over very long periods of time.

Uniformitarianism and Geologic Processes

  • Uniformitarianism is the idea that present-day geological processes can help understand past events.
  • Four key ideas for determining events in a landform diagram:
    • Law of original horizontality
    • Law of superposition
    • Cross-cutting relations
    • Unconformities

Stream Valleys

  • Stream valleys are depressions where water flows.
  • Erosion by flowing water shapes these valleys.
  • Stream valleys progress through stages:
    • Youth: Steep gradient, fast water, V-shaped valley, barriers to water
    • Maturity: Less steep gradient, slower water, U-shaped valley, floodplain development
    • Old Age: Extremely low gradient, wide and flat valley, very slow and wide waterway.

Base Level of a Stream

  • Base level is the lowest point water can erode a stream channel.
  • Types of base levels:
    • Ultimate base level (sea level)
    • Local (temporary) base level (e.g., lakes, dams, waterfalls)
  • Base level influences water velocity, height, and erosion/deposition.

Bedrock Channels

  • Bedrock is solid rock, often covered by alluvium (loose soil/sediment).
  • Bedrock channels are paths cut into bedrock.
  • Stream power is the rate of energy loss on a channel bed, leading to erosion.
  • Processes that create bedrock channels:
    • Abrasion: sandpaper-like effect from particles scraping.
    • Plucking (quarrying): large rock chunks are eroded and moved.

Alluvial Channels

  • Alluvial channels are river sections constantly changing shape from water flow, sediment, and deposition patterns.
  • Examples of alluvial channel types:
    • Meandering: winding loops with point bars
    • Braided: network of small interlaced channels, separated by sediment bars
    • Straight/Sinuous: linear appearance with sinuous flow, sand bars
    • Anastomosing: interconnected multiple streams
  • Features formed by alluvial channels:
    • Oxbow lakes: cut-off meandering loops
    • Floodplains: widened, flat areas next to rivers
    • Natural levees: sediment deposits along riverbanks
    • Terraces: step-like land features due to erosion and deposition

Groundwater

  • Groundwater is a significant portion of Earth's freshwater.
  • Two zones:
    • Saturated zone: completely filled with water
    • Unsaturated zone (vadose): above saturated zone, with soil moisture
    • Water table: boundary between the two zones.
  • Groundwater is stored in aquifers (underground reservoirs).
  • Groundwater movement shapes landscapes:
    • Carries sediment, forming sedimentary rock
    • Dissolves rock, forming caves and caverns
    • Can be heated, creating geysers
  • Removing groundwater too quickly can cause sinkholes.

Groundwater Flow

  • Groundwater flow depends on:
    • Porosity: amount of water soil/rock can hold
    • Permeability: rate of water passage through soil/rock
    • Gravity: pulls water downwards along a hydraulic gradient
  • Aquifers are underground water reservoirs (confined & unconfined).
  • Natural springs form where groundwater reaches the surface.
  • Spring water quality is affected by factors like proximity to human activity, and mineral composition.

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Description

This quiz covers essential concepts of weathering, erosion, and deposition, crucial processes influencing landscape formation. It also explores uniformitarianism and key geological principles that help us interpret landforms. Test your knowledge on how water shapes stream valleys and the stages of valley development.

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