Unit 3 Vocabulary The Hydrosphere. 1.Water Cycle - the unending circulation of Earth’s water supply. 2.Infiltration - the movement of surface water into.

Slides:



Advertisements
Similar presentations
6.1 Running Water Oceans – 97 % Glaciers/ice – 2 %
Advertisements

Running Water and Groundwater
Groundwater Chapter 16.
CHAPTER 6.3 WATER BENEATH THE SURFACE
Groundwater Chapter 6.3.
Prentice Hall EARTH SCIENCE
Prentice Hall EARTH SCIENCE
Running Water and Groundwater
Running Water and Groundwater Chapter 5
Water Beneath the Surface
Water.
Surface Water and Groundwater. Running Water and Groundwater % of where the Earth’s water is located –Oceans (salt water) – 97 % –Freshwater trapped in.
The Work of Streams. Erosion Usually happen by streams flowing through their channels and lifting loose particles by abrasion, grinding, and by dissolving.
Running Water & Groundwater
6.3 Water Beneath the Surface
Water Beneath the Surface
Chapter 16 Study Notes: Groundwater.
Running Water and Groundwater
PG.81 Sources of water. Water on earth All water on earth constitutes the hydrosphere 97% is stored in oceans 2% in glaciers 1% lakes, streams, ground.
Tarbuck & Lutgens. Stanley C. Hatfield Southwestern Illinois College.
Running Water and Groundwater. Earth as a system: the hydrologic cycle  Illustrates the circulation of Earth's water supply  Processes involved in the.
Chapter 10: Ground water Review Designed by: Meghan E. Dillner.
There is a continuous movement of WATER from the atmosphere to the earth’s SURFACES and then back to the ATMOSPHERE. This cycle of water movement.
WATER ON AND UNDER GROUND. Objectives Define and describe the hydrologic cycle. Identify the basic characteristics of streams. Define drainage basin.
Chapter 9 1. Water cycle- Each part of the cycle drives the other parts.
Earth as a System: The Hydrologic Cycle
 Erosion  process by which wind, water, ice, or gravity transports soil and sediment from one location to another.
Groundwater.
© 2012 Pearson Education, Inc. Earth Science, 13e Tarbuck & Lutgens.
Chapter 6. Where is our water? Water Cycle Evaporation from the ocean and other water sources Precipitation over the ocean and land Water runs from high.
Ground Water.  Much of the water in soil seeps downward until it reaches the zone of saturation  Zone of Saturation  Is the area where water fills.
EARTH SCIENCE Prentice Hall EARTH SCIENCE Tarbuck Lutgens 
Warm-Up:  How is weathering and erosion different?
Unit 3 - Hydrosphere Study Guide Answer Key.
Sculpting the Earth’s Surface Running Water AndGroundwater.
Fresh Water Vocabulary Hi, I’m Mike Krzyzsyhjski !
Fresh Water Vocabulary HELLO DUKE, GREAT YEAR SO FAR!
Running Water and Groundwater
Ch. 9 Water Erosion and Deposition
Running Water and Groundwater
Groundwater, Running Water and Estuaries
Freshwater Vocabulary
Earth Science, 13e Tarbuck & Lutgens.
Surface Water and Groundwater
Chapter 6 Running Water and Groundwater
Water Beneath the Surface
EARTH SCIENCE KESSEL.
2.3.2a Water Cycle, Surface Water, and Ground Water
Water Cycle #12.
Water Cycle It keeps cycling back
GROUNDWATER.
Water Erosion and Deposition
Prentice Hall EARTH SCIENCE
Precipitation = Evaporation
Running Water & Groundwater
2.3.2a Water Cycle, Surface Water, and Ground Water
Water Erosion and Deposition
Water Cycle It keeps cycling back
Water Vocab.
Groundwater.
Running Water and Groundwater
Running Water Earth Science Chapter 6
Groundwater.
The Work of Streams.
Prentice Hall EARTH SCIENCE
Running Water and Groundwater
Groundwater.
Precipitation = Evaporation
Water Beneath the Surface
Groundwater Chapter 6.3.
Presentation transcript:

Unit 3 Vocabulary The Hydrosphere

1.Water Cycle - the unending circulation of Earth’s water supply. 2.Infiltration - the movement of surface water into rock or soil through cracks and pore spaces

3. Transpiration - plants absorb water and release it into the atmosphere. 4. Gradient - the slope or steepness of a stream channel 5. Stream Channel - the course the water in a stream follows.

6. Discharge - the volume of water flowing past a certain point in a given unit of time. 7. Tributary - a stream that empties into another stream. 8. Base Level - the lowest point to which a stream can erode its channel.

9. Meanders - a stream with many bends 10. Bed Load - the part of a stream’s load of solid material that is made up of sediment too large to be carried in suspension. 11. Capacity - the maximum load a stream can carry.

12. Alluvium - the sorted material deposited by a stream. 13. Delta - an accumulation of sediment formed where a stream enters a lake or ocean. 14. Natural Levee - a landform that parallels some streams.

15. Floodplain - the side-to-side cutting of a stream eventually producing a flat valley floor. 16. Flood - Occurs when the discharge of a stream becomes so great that it exceeds the capacity of its channel and overflows its banks.

17. Drainage Basin - the land area that contributes water to a stream. 18. Divide - an imaginary line that separates the drainage basin of one stream from another.

19. Zone of Saturation - the area where water fills all the open spaces in sediment and rock. 20. Groundwater - the water within this zone 21. Water Table - the upper limit of the zone of saturation

22. Porosity - the percentage of the total amount of rock or soil that consists of pore space. 23. Permeability - a material’s ability to release a fluid.

24. Aquifer - permeable rock layers or sediments that transmit groundwater freely. 25. Spring - a flow of groundwater that emerges naturally at the ground surface. 26. Geyser - an intermittent hot spring or fountain in which a column of water shoots up with great force at various intervals.

27. Well - a hole bored into the zone of saturation 28. Artesian Well - any formation in which groundwater rises on its own under pressure. 29. Cavern - a naturally formed underground chamber.

30. Travertine - the calcium carbonate that is left behind producing the limestone that creates this. 31. Karst Topography - landscape that has been shaped largely by the dissolving power of groundwater.

32. Sinkhole - a depression produced in a region where groundwater has removed soluble rock.