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What are the three type of bathymetric soundings |
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Multibeam sidescan and echo |
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a mountain rising from the ocean seafloor that doesn't reach to the water's surface,and isn't an island Hawaiian Emperor seamount chain is a well-known example of a large seamount |
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is an isolated underwater volcanic mountain, with a flat top over 200 metres below the surface of the sea As the mid-ocean ridges spread apart, the guyots move with them, thus continually sinking deeper into the depths of the ocea |
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Earths Structure by composition |
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Definition
Crust- Fe-poor Rock) Mantle(Fe-richRock) MetallicCore(Ni/Fe) |
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Term
Earths crust by physical properties |
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Definition
Lithosphere (Crust andRigid Upper Mantle Asthenosphere (Toothpaste Upper Mantle) Mesosphere (Mantle) Outer Core (Liquid Ni/Fe Inner Core (Solid Ni/Fe) |
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Definition
The outer shell of the earth, the lithosphere, is broken into a few(10-20) internally rigid plates in continuous relative motion. |
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Divergent Plate boundaries |
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Definition
Plates Move Apart at Mid-Ocean Ridges or Continental Rifts Lithosphere is Created |
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Convergent Plate boundaries |
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Definition
Plates Collide at Trenches or Continent to Continent Lithosphere subducted to Mantle Lithosphere Raised to Himalayas |
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Transform Plate boundaries |
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Definition
Lithosphere is Conserved Transform Faults (San Andreas) No volcanism Moderate to Severe Earthquakes Transform (strike-slip) faults Connect spreading segments |
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Term
What boundary has Shallow Focus (mild) Earthquakes Basaltic Volcanism (non explosive) Normal Faulting (extension) |
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Definition
Divergent plate boundaries |
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Term
How are rift valley's formed |
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Definition
as the content undergoes extension crust is thinned and rift valley is formed |
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Term
What are features of convergent plate boundaries |
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Definition
• Ocean trenches • 1. Ocean crust - ocean crust • 2. Ocean crust - continental crust • 3. Continental crust - continental crust • Shallow-, mid- and deep-focus earthquakes • Volcanism (explosive) • Mountain building |
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Content to Content collision |
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Definition
Buoyant continental crust just won’t go down. Massive Mountain building Thickest crust No volcanism |
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Definition
• Localized regions of high heat flow in the mantle. • Cause melting in the overlying crust. • Remain fixed for between 20 million and 100 million years. • Massive Volcanic (non-explosive) eruptions |
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Definition
originate at CMB thought to remain stationary relative to one another |
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Term
What drives the plates and earths thermal engine |
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Definition
1. Original heat of planetary formation Kelvin: Earth was originally molten Cooling ever since Age of Earth=30My 2. radioactive decay (K, U, Th) 3. Heat of crystallization at outer/inner core boundary |
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plates are moving down slope due to gravity, from high elevation at ridges to low elevation in trenches. |
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Subducting slab sinking into mantle pulls the rest of the plate behind it. |
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