Geology of the Ocean

Origin of Earth 4.6 billion years ago began as giant disk of dust and gases orbiting the sun grains came together forming comets, asteroids, planets (The Nebular Theory)

Earth Structure Density Stratification core – very dense (iron & nickel) –inner core is solid –outer core is liquid (viscous); creates magnetic field mantle – dense rock, mostly solid does NOT melt because of rapidly increasing pressure

Earth Structure (cont.) asthenosphere – upper part of mantle, nearly molten, flows very slowly –Hot, partially melted lithosphere – rigid outer layer ( mi. thick) – floats in the asthenosphere –Comprised of crust and uppermost portion of the mantle

Earth Structure (cont.) crust – upper part of lithosphere – rigid because of low temperature two types: continental crust – thicker than oceanic crust, lighter in color, less dense oceanic crust – thinner, darker, more dense

Kontinentalverschiebung Theory of Continental Drift Proposed in 1912 by Alfred Wegener –c–continents fit together like pieces of a jigsaw puzzle. –S–Suggested that 200 million years ago, continents formed one big land mass Pangaea similarities in fossils and rock formations on different continents bordered by the Atlantic Ocean

Continental Drift Geologists ignored his theory initially…continents did not fit together exactly like “puzzle pieces”. Harry Hess – Continents floated on asthenosphere (semi-fluid) Used the end of the continental shelf to put continent pieces together—fit exactly

Isostasy Lithospheric plates float in the asthenosphere in a balance called Thicker (less dense rocks) continental crust floats higher than thin oceanic crust Large glaciers weigh down crust, when glaciers melt, plates rise (can be measured).

Plate Tectonics Lithosphere (crust) is made of several very large plates which move. Theory explains geological changes and features and events such as earth quakes, continental drift and volcanoes.

Plate Boundaries (3 types) 1.Divergent boundaries – Found at Mid-ocean ridges – –plates move away from each other –new crust formed –seafloor spreading – crust forms from magma at a rift valley

Divergent Boundaries

Divergent boundaries Midocean Ridges Mid-Atlantic Ridge –most prominent feature steep-sided, very tall mountains rift valley km wide –small e-quakes occur frequently on crests

Divergent boundaries Rises –Shorter than ridges because plates spread apart faster –Have less time to accumulate –Frequently found in Pacific Ocean

Convection Currents –Causes molten magma to rise through mantle and into crust creating oceanic ridges

Magnetic Reversals Magnetic bands show that new crust is formed and moves away from the ridge over time, has allowed us to date oceanic crust

Convergent Boundaries –Plates converge (come together) –Crust is destroyed-(recycled into mantle) or pushed up to form mountains.

Convergent Boundaries

Convergent boundaries Subduction – zone where dense lithosphere (crust) sinks into mantle and is reabsorbed – Occurs widely in western Pacific basin

Convergent boundaries Trenches –D–Deepest part of the ocean floor –M–Most occur in Pacific (esp. western Pacific) –M–Most of Pacific Ocean bordered by trenches

Transform Boundaries Transform faults – plates slide past each other. – Result in earthquakes – Ex. San Andreas fault in California

Seafloor Features Principal boundary between continents and ocean basins is called the continental margin … Continental shelf Continental slope Continental rise

Continental shelf The relatively flat, submerged margin of a continent between the shoreline and depth of 200 meters.

Continental slope steep portion at the end of the continental shelf that ends at the beginning of the ocean basin

Continental rises Occur at the base of the continental slope… slopes gently…connects with the deep-sea floor

Deep-Ocean Floor (30% or Earth’s surface) abyssal hills – cover about 80% of Pacific floor and half of the Atlantic – typically 200m high (many extinct volcanoes) –Are very short compared to midocean ridge mountains abyssal plains – flat deep ocean floor

Hot spots –midocean ridges (Iceland) –in middle of crustal plates (Hawaii) –remain fixed for a very long time

Hot Spots Example: Hawaii –plates move over hot spots and form chains of volcanoes –youngest islands remain active while near hot spot –after crust moves away, volcano becomes extinct