Marine Sediments Flashcards
why marine sediments are interesting to oceanographers.
Reveals Earth’s history.
Provides clues to past geographic distributions of marine organisms, movements of the ocean floor, ocean circulation patterns climate changes on Earth and global extinction.
four primary types of marine sediment
Lithogenous
Biogenous
Hydrogenous
Cosmogenous
List the past conditions that scientists can infer by analyzing marine sediments.
Sea surface Temperature Nutrient supply abundance of marine life atmospheric winds ocean current patterns volcanic eruptions major extinction events changes in Earth’s climate movement of tectonic plates
paleoceanography
The study of how the ocean, atmosphere, and land have interacted to produce changes in ocean chemistry, circulation, biology and climate.
lithogenous sediment
Derived from pre-existing rock material that originates on the continents of islands from erosion, volcanic eruptions, or blown dust. Also referred to as terrigenous sediment.
Characteristics of Lithogenous Sediment
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List the transportation mechanism that carry sediment to the ocean
Streams, wind, glaciers, and gravity.
List the submarine transportation mechanisms that carry sediment beyond the continental margin
Turbidity currents
In which marine region do the largest marine sedimentary deposits form
Around the margins of the continents.
why most lithogenous particles, including most sand (but not Hawai’i sand), are quartz
Quartz is a major component of most rocks and since it is resistant to abrasion it can be transported long distances.
the primary sediment transportation mechanism from the Sahara Desert to the ocean.
Prevailing winds
list the primary sediment sizes from coarse-grained to fine-grained.
Boulder, cobble, pebble, granule, sand, silt, clay
why lithogenous sediments tend to become finer with increasing distance from shore.
Because high-energy transporting media predominate close to shore and lower-energy conditions exist in the deep-ocean basins.
Define well-sorted sediment and poorly-sorted sediment.
Well-sorted sediment is sediment composed of particle that are primarily the same size whereas poorly-sorted sediment is sediment that is comprised of a variety of differently sized particles.
Define neritic deposits and pelagic deposits.
Neritic deposits are found on continental shelves and in shallow water near islands and are generally coarse grained; pelagic deposits are found in deep-ocean basins and are typically fine grained