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The Dynamic Earth:

The Dynamic Earth:. UNIT 2 (ch. 3). 3.1 OBJECTIVES. Describe the composition and structure of the Earth. Describe the Earth’s tectonic plates. Explain the main cause of earthquakes and their effects. Identify the relationship between volcanic eruptions and climate change.

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The Dynamic Earth:

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  1. The Dynamic Earth: • UNIT 2 (ch. 3)

  2. 3.1 OBJECTIVES • Describe the composition and structure of the Earth. • Describe the Earth’s tectonic plates. • Explain the main cause of earthquakes and their effects. • Identify the relationship between volcanic eruptions and climate change. • Describe how wind and water alter the Earth’s surface.

  3. Earth--a system • The Earth can be divided into 4 different parts: • geosphere (rock); most is located in the Earth’s interior. • atmosphere (air); gases--nearly all of which are found in the first 30km above the Earth’s surface. • hydrosphere (water); oceans, atmosphere, land, and soil. • biosphere (living things); ~9km above the Earth’s surface down to the bottom of the ocean.

  4. Seismic waves: learning about the Earth’s interior • seismic waves: waves that travel through Earth’s interior during an earthquake. • http://www.ccmr.cornell.edu/education/ask/?quid=1374 • 3 layers (based on their composition/chemistry...less dense --> more dense): • crust--thin outer layer; light elements; <1% of the Earth’s mass • mantle--64% of Earth’s mass; made of rocks of “medium” density • core--made of the most dense elements; ~3400km in radius

  5. Earth’s Structure--based on physical (not chemical) properties • 5 layers: • lithosphere (outer layer) -- includes the crust and the uppermost part of the mantle; divided into tectonic plates • asthenosphere -- solid layer of the mantle; made of rock that flows very slowly & allows tectonic plates to move on top of it • mesophere -- lower part of the mantle • outer core -- made of liquid nickel & iron • inner core -- a sphere of solid nickel & iron at the center of the Earth • http://chemistry.about.com/od/chemistry101/f/What-Is-The-Difference-Between-A-Chemical-Property-And-A-Physical-Property.htm

  6. Assignment: outliningchecked tomorrow • pg. 67-70 • Earthquakes • Volcanoes • Erosion • complete either in your notebook along with your notes OR on your iPad using whatever format you typically take notes in. • Check the section objectives at the beginning of the powerpoint to make sure that you are thorough with your notes!

  7. 3.2: The Atmosphere • Made up of gases: ~78% Nitrogen, ~21% Oxygen, ~1% “other”... carbon dioxide, water vapor, methane,... • constantly changing (volcanoes, photosynthesis, pollution) • insulates the Earth’s surface, important to support life • pulled toward the surface by gravity: density increases the closer you get to the Earth’s surface

  8. 4 Layers • Based on temperature • Troposphere: weather; densest layer; temp decreases with increasing altitude • Stratosphere: temp increases with increasing altitude...why? Ozone absorbs the sun’s UV energy and warms the air. **Ozone (O3) reduces the amount of UV radiation that reaches Earth...IMPORTANT!

  9. Mesosphere: coldest layer • Thermosphere: farthest layer from the Earth’s surface; lower portion is called the ionosphere...produces the aurora borealis (Northern lights)

  10. Energy in the Atmosphere • Energy from the sun is transferred in the atmosphere by 3 mechanisms (fig. 15 pg. 74-75): • radiation: across space (feeling the warmth of a fire) • conduction: flow of heat from a warmer object to a colder object when the 2 are in direct physical contact with one another (this is how air near the Earth’s surface is heated). • convection: transfer of heat by air currents (hot air _______ and cool air ______); **convection currents

  11. Heating the Atmosphere • ~1/2 of the solar E that enters the atmosphere actually reaches the surface. • the other 1/2 is absorbed or reflected by clouds, gases, dust, or the Earth’s surface (land and water). • greenhouse effect: the process in which gases trap heat near the Earth • w/o this process, the Earth would be too cold for life to exist. • gh gases: water vapor, CO2, methane, nitrousoxide. • http://epa.gov/climatestudents/basics/today/greenhouse-effect.html

  12. 3.3: Hydrosphere • Water cycle: the continuous movement of water into the air, onto land, and then back to water sources. • evaporation / transpiration • condensation • precipitation • others!!

  13. Create a Conceptual Model • Use the educreations app to create a visual that depicts the water cycle and the processes involved. • Additionally, you will need to explain (by recording your voice) the cycle and how all of the processes are interconnected. • Submitted to me by Thursday (mmahar@gulllakecs.org)

  14. World Ocean • The interconnected oceans of the Earth: Pacific (largest and deepest point), Atlantic, Indian, Arctic (sea ice = frozen sea water; pack ice = a large mass of sea ice) • ~70% of the Earth’s surface • difference compared with freshwater? (more salt...higher salinity)

  15. Our Temperature Regulator • our oceans absorb over 1/2 the solar radiation that reaches the planet’s surface • Water absorbs and releases heat slower than land --> atmospheric T changes much more slowly than if there were no oceans • without the oceans, our atmosphere and surface temperatures would be too extreme to support life!

  16. Freshwater & Groundwater • Fresh: < 3%; most is locked up in icecaps and glaciers...the “rest”, lakes, rivers, wetlands, soil, rock layers below the surface, and in the atmosphere • Ground: < 1%; our drinking water AND supply for many agricultural / industrial uses • aquifer: a rock layer that stores and allows the flow of groundwater. • recharge zone: the surface of land where water enters an aquifer.

  17. Biosphere...the ‘skin’ of the apple :) • ~12km down into the ocean and ~9km up into the atmosphere • HOW? • liquid water • moderate temperatures • energy source (T, photosynthesis, food chains/webs) • requirements are continuously cycled • gravity (atmosphere and cycling of materials)

  18. closed vs. open systems • open systems: both matter and E are exchanged btwn. the system and the surrounding environment • closed systems: E enters and leaves the system, but matter does not. • Earth?

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