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The Sea Floor

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The Sea Floor
Continental Margin= shelf and slope and rise
- extends from shoreline to shelf break
- depth= 135 m
- extends from shoreline to shelf break
submarine canyons
- undersea landslides
- deposition of sed. to form submarine fans
- due to turbidity currents
carbonate materials and reefs
- depends on climate
- needs warm water
- needs clean H2O= lots of sunlight
- fringing reefs (along shore)
- barrier reefs (separated from shore by lagoon)
- atoll (circular reef around submerged volcanic island)
- depends on climate
abyssal plains
- landforms in deep ocean
- basalt underlies ocean floor BUT in abyssal plains, surface covered with sediment
- turbidity deposits
- pelagic deposits
- wind blown and ice transported materials
- cosmic (meteoritic debris)
- products of submarine weathering
- basalt weathering= clay deposits
- calcareous ooze
- siliceous ooze
- shells of siliceous plants and animals
- lithifies to form chert
- basalt underlies ocean floor BUT in abyssal plains, surface covered with sediment
- landforms in deep ocean
ocean ridges
- very extensive
- marks divergent plate boundaries
- sea floor spreading
- continuously forming new ocean crust
- fissure eruptions of basalt magma
- ocean crust
- pillow basalts
- erupted along ocean ridges from fissures
- dykes of gabbro
- feeders to pillow basalt
- deep-sea sediment
- mostly pelagic
- on top of pillow basalt
- Moho makes up bottom of ocean crust
- boundary btw. earth's crust and mantle
- pillow basalts
- continuously forming new ocean crust
ocean trenches
- deepest part of ocean
fracture zones
seamounts and oceanic islands
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- Year 1 Geology Mind Map on The Sea Floor, created by Sarah Lavallée on 12/09/2018.
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- Sarah Lavallée
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