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Fresh Water Notes Chapter 12

Fresh Water Notes - Mrs. Smit's Science Classsmitscience.weebly.com/.../9/9/2199719/fresh_water_notes.pdf · 2019. 8. 22. · –about ¾ of fresh water is frozen –about ¼ of fresh

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  • Fresh Water Notes

    Chapter 12

  • Water Cycle

    • Water Cycle is a continuous moving of water from Earth’s surface to the atmosphereand back.

  • Water Cycle Parts

    • There are 3 Major Parts

    –Evaporation: liquid water changes to a gas water vapor

  • Water Cycle Parts

    –Condensation: water vapor cools and “clumps” around dust particles forms a cloud

  • Water Cycle Parts

    –Precipitation: Water vapor condenses and droplets get heavier

    •Examples

    –Rain

    –Snow

    –Sleet

    –Hail

  • Precipitation•Returns to earth and…

    –Soaks into the soilgroundwater

    –Runs off the land back to the ocean Run Off

  • Distribution of Earth’s Water

    • 97% salt water

  • Salt Water Locations

    • Location of Salt Water

    –Oceans

  • Saltwater: Oceans

    •Pacific

    –Largest

    –Deepest

  • Saltwater: Oceans

    •Atlantic

    –2nd largest

  • Saltwater: Oceans

    •Indian

    –Smallest liquid ocean

    –Deeper than Atlantic

  • Saltwater: Oceans

    • Arctic

    –Smallest

    –mostly frozen

  • Freshwater Location

    • 3% fresh water

    – about ¾ of fresh water is frozen

    – about ¼ of fresh water is underground

    – A tiny portion is in lakes and rivers

    – A tiny portion is in water vapor in atmosphere

  • Freshwater Location

    • Location of Fresh water

    –Ice

    •Locked in sheets at the poles

  • Freshwater Location

    –Rivers and Lakes

    •Important source of fresh water for communities

    •Very small amount of the worlds water

  • Freshwater Location

    –Groundwater

    • More water is stored underground than in all of Earth’s rivers and lakes.

  • Surface Water

    • Fresh water is found here

  • River Systems

    • Rivers start in the mountainsas run off from melting snow

  • Parts of A River System

    –Tributaries: streams & smaller rivers that feed into main river

  • Parts of A River System

    –Water Shed: land & area that supplies water to a river system

  • We live in the Mississippi River water shed

  • Parts of A River System

    –Divide: Land ridge that separates one water shed from another•The continental divide is the longestdivide in North America

  • Ponds

    • Characteristics of Ponds

    –Contain standing water (not moving)

    –Shallow

    •Sunlight reaches the bottom

  • Pond Formation

    • Ponds form in different ways

    –Rainfall

    –Melting snow and ice

    –Run off

    –Rivers

    –Ground water

  • Ponds are Habitats

    • Ponds are habitats for many animals

    –Habitat: the place an organism lives and gets what it needs to survive

  • Lakes

    • Characteristics of a lake

    –Deeper and bigger than ponds

    –Sunlight does not reach the bottom

    •No plants live on the bottom

    –Bottom is sand, pebble or rock

  • Formation of Lakes

    • Formed in several ways

    –Ice sheets melting (Glaciers)

    •Ex. Great Lakes

  • Formation of Lakes

    –Movement of Earth’s crust

    •Ex. Lake Victoria in Africa

  • Formation of Lakes

    –Volcanoes

    •From lava flow

    •Empty volcano craters

  • Formation of Lakes

    –Reservoir- a lake that stores water for human use

  • Wetlands

    • A land area that is coveredwith water during part or all of the year

  • Types of Wetlands

    • Three common types

    –Marshes- grassy areas covered by shallow wateror a stream

  • Types of Wetlands

    –Swamp- look like flooded forests

  • Type of Wetlands

    –Bogs- in cool areas

  • Wetlands

    • Everglades: Marshes in Florida

  • Importance of Wetlands

    • Importance of wetlands

    –Habitats to many species

    –Natural water filters

    –Flood controls

  • Water Underground

    • How water movesunderground

    • Trickles down between particles of soil and through cracks and spaces

    in layers of rock

  • Groundwater Movement

    • Different types of rock and soil effects how water moves–Large pore size water moves easilydownward•Permeable: water can passthrough

  • Groundwater Movement

    –Small pores- or no connected pores

    •Impermeable: water cannotpass

    through

  • Water Zones

    –Saturated Zone

    •Totally filled

    –water table: top of the saturated zone

  • Water Zones

    –Unsaturated Zone

    •Pores have some moisture but also some air

    •Not Filled

  • Bringing Up Ground Water

    • Springs: groundwater bubbles or flows out cracksin the rocks

    –Can be hot or cold

  • Bringing up Groundwater

    • Aquifers: any underground layer of rock or sediment that holds H2O

  • Bringing Up Groundwater

    • Wells

    –Location: below the water table

    •can be effected by drought (no rain)

  • Bringing Up Groundwater

    –Pumps

    •Mechanical

    •Overuse

    –Pump can become

    dry

  • Bringing Up Groundwater

    • Artesian Well: water rises because of the pressurewithin the aquifer

    –No pump necessary

    –Water spurts out

  • Bringing Up Groundwater

    • Geyser: fountain of boiling water and white steam bursts into air

    –Periodically erupts (on a regular schedule)

    •Heated by magma

    –Ex. Old Faithful