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Published byStephen Hudson Modified over 6 years ago
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Coming up… Friday 2/10: Today 1/31: Thursday 2/2: Monday 2/6:
Finish ocean water properties (density) Intro to Sediments Begin sediment lab Thursday 2/2: Finish sediment lab Discuss ocean sediments Monday 2/6: Ocean Acidification Wednesday 2/8: Wrap up loose ends Review time Friday 2/10: -- Unit 1 Oceans Test…and begin Unit 2: The Atmosphere!
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Bellwork 2/3 Look at your Part 1: Biogenous Sediments observations…
Are all of the sediments found in the same places? What might account for differences in locations? For example, are Coquina, Chalk, and Siliceous Ooze found in the same areas?
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Bellwork 2/8 Remember, you have a very short lab quiz today! What causes ocean water to change density? How does this relate to the creation of ocean currents?
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Then we’ll begin Unit 2—THE ATMOSPHERE!
Coming up… Tuesday 2/6: Finish ocean water properties (density) Intro to Sediments Thursday 2/8: Lab Quiz!! Discuss ocean sediments Begin Sediment Lab Monday 2/12: Finish Sediment Lab Begin Ocean Acidification Wednesday 2/14: Finish Ocean Acidification Friday 2/16: Wrap up loose ends Review Ocean Test Tuesday 2/20! Then we’ll begin Unit 2—THE ATMOSPHERE!
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Sediments & Ocean Water Properties …a two way street
Ocean currents & water density help us understand the formation and distribution of sediments Sediments help us understand how ocean water features mechanically work and how the ocean has changed over time
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Today: Brief look at the sediment types
Quick discussion of how/why sediments are distributed differently
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Biogenous Sediment Shells and skeletons of marine animals and algae
Can be large grained …. Ex: shells from larger organisms ….or tiny grained Ooze: greater than 30% biological shells Mostly plankton & diatom “skeletons” (both microscopic organisms that live in the open ocean) Siliceous & Calcareous
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Macroscopic (large grain) sediment is found along continental shelves
Why? Microscopic (tiny grain) is found along the sea floor
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Before we talk about Lithogenous Sediments…
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Lithogenous Sediment Weathered from continental rocks and transported to the ocean Rivers/Streams Continental Shelf & Rise (beaches) –course grains Why? Abyssal plains—fine grains
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Hydrogenous Sediment Minerals that crystallize directly from seawater through chemical reactions Typically found in “open ocean” Basins & Abyssal plains
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With that very basic introduction, we’re going to start our Sediment Investigation
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