Geography Chapter 15 - Groundwater & Karst Topography

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19 Terms

1
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Inputs vs Outputs

  • Inputs = water added to the system

    • Example: Precipitation

  • Outputs = water is lost from the system

    • Example: Evapotransportation

2
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What is evaporation?

  • moisture is lost to the atmosphere through the wind and sunlight

  • rates are affected by temperature, wind speed, humidity

3
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What is Transpiration?

  • biological process by which water is lost from a plant

  • Rates depend on time of year, type + amount of vegetation, availability of moisture, and the length of the growing season

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What is Groundwater?

  • fresh water (from raining or melting ice and snow) that soaks into the soil and is stored in the tiny spaces between rock

  • can stay underground for hundreds to thousands of years

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What is Groundwater? pt. 2

  • can come to the surface and help fill rivers, streams, lakes, etc.

  • can also come to the surface as a spring or be pumped from a well

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What is Porosity?

  • In order for groundwater to exist, there has to be porous layers

  • These are spaces within the soil which allows water to flow through them and be stored

<ul><li><p>In order for groundwater to exist, there has to be porous layers </p></li><li><p>These are spaces within the soil which allows water to flow through them and be stored</p></li></ul><p></p>
7
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What is Permeability?

  • Permeable = the ability for water to pass through rock layers

  • Impermeable = the inability for water to pass through rock layers

<ul><li><p>Permeable = the ability for water to pass through rock layers</p></li><li><p>Impermeable = the inability for water to pass through rock layers</p></li></ul><p></p>
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What is the Importance of Groundwater?

  • In the prairies groundwater is used extensively for crop irrigation

  • Areas with no mountain ranges with no rain rely on groundwater as their water source

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What are Groundwater zones?

  • When water infiltrates the ground a section of rock becomes saturated (zone of saturation)

  • The top of the saturated rock/soil is the water table

  • The portion of the rock that is not 100% saturated is called the zone aeration

<ul><li><p>When water infiltrates the ground a section of rock becomes saturated (<strong>zone of saturation</strong>)</p></li><li><p>The top of the saturated rock/soil is the <strong>water table</strong></p></li><li><p>The portion of the rock that is not 100% saturated is called the <strong>zone aeration</strong></p></li></ul><p></p>
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What is an aquifer?

  • Rock layer that can store and yield water

  • In dry areas aquifers provide clean water for drinking and irrigation by drilling a well

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Recharge vs Discharge Diagram

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Aquifers: Ordinary Wells

  • Ordinary Wells are located in-between permeable rock

  • Water is not under pressure and is forced to rise with a pump

<ul><li><p>Ordinary Wells are located in-between permeable rock</p></li><li><p>Water is not under pressure and is forced to rise with a pump</p></li></ul><p></p>
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Aquifers: Artesian Well

  • Artesian Well is drilled through the ground

  • Confined between two impermeable rock layers which causes a build up of pressure which causes the water to rise on its own

<ul><li><p>Artesian Well is drilled through the ground</p></li><li><p>Confined between two impermeable rock layers which causes a build up of pressure which causes the water to rise on its own</p></li></ul><p></p>
14
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What are some potential threats to our Groundwater?

  • contamination + Overuse and depletion

15
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How do Karst Landforms form?

  • Process is called: Carbonation

  • Limestone and Dolostone

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Landforms created by groundwater

  • Travertine Terraces:

    • Found in areas in where there is an abundant amount of hot groundwater

    • Hot water carries dissolved material and when it reaches the surface it quickly cools and deposits minerals on existing rock

<ul><li><p><strong>Travertine Terraces:</strong></p><ul><li><p>Found in areas in where there is an abundant amount of <strong>hot groundwater</strong></p></li><li><p>Hot water carries <strong>dissolved material</strong> and when it reaches the surface it quickly cools and deposits minerals on existing rock<strong> </strong></p></li></ul></li></ul><p></p>
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Karst Landscapes

  • Caves or Caverns

    • Found in areas with highly soluble rock such as limestone

    • Water moves through the rock, dissolving limestone

<ul><li><p><strong>Caves or Caverns</strong></p><ul><li><p>Found in areas with highly soluble rock such as limestone</p></li><li><p>Water moves through the rock, <strong>dissolving</strong> limestone</p></li></ul></li></ul><p></p>
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Sinkholes

  • As caverns increase in size the support decreases and the ground collapses

  • Forms a depression (sinkhole)

<ul><li><p>As caverns <strong>increase</strong> in size the support decreases and the ground collapses</p></li><li><p>Forms a <strong>depression</strong> (sinkhole)</p></li></ul><p></p>
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Why does Florida have so many sinkholes?

  • Most of Florida peninsula is made up of limestone and dolostone overlain by sand and clay

  • Carbonate rocks may dissolve (solution) forming karst terrain