ELS- 2nd Quarter Flashcards
(129 cards)
Different Features of the Ocean Floor:
5 items
Continental margin
Abyssal plains and abyssal hills
Mid-ocean ridges
Deep-ocean trenches
Seamounts and volcanic islands
submerged outer edge of the continent where continental crust transitions into oceanic crust
Continental margin
it is an extremely flat, sediment-covered stretches of the ocean floor, interrupted by occasional volcanoes, mostly extinct, called seamounts
Abyssal plains and abyssal hills
a submarine mountain chain that winds for more than 65,000 km around the globe
Mid-ocean ridges
narrow, elongated depressions on the seafloor many of which are adjacent to arcs of island with active volcanoes; deepest features of the seafloor.
Deep-ocean Trenches
One of the causes of Seafloor Spreading is the
Continental drift theory
(4) Evidence that supports continental drift theory:
Fit of the continent
Matching of rock units across ocean basins
Distribution of fossils
Paleoclimate evidence (evidence of tropical climates and past glaciations)
In ____, he advance the theory of seafloor spreading. He proposed that seafloor spreading separates at mid-ocean ridges where new crust forms by upwelling magma. Newly formed oceanic crust moves laterally away from the ridge with the motion like that of a conveyor belt. Old oceanic crusts are dragged down at the trenches and re-incorporated back into the mantle. The process is driven by mantle convection currents rising at the ridges and descending at the trenches.
This idea is basically the same as that proposed by ______ ______ in ____
1960
Harry Hess
Arthur Holmes in 1920
Evidences That Lead to the Proposal of Seafloor Spreading
5 items
High heat flow along mid-ocean ridge axes
Distribution of seafloor topographic features
Sediment Thickness
Composition of oceanic crust
Distribution of submarine earthquakes
it led scientists to speculate that magma is rising into the crust just below the mid-ocean ridge axis
High heat flow along mid-ocean ridge axes
distribution of mid-ocean ridges and depth of the seafloor
Distribution of seafloor topographic features
fine layer of sediment covering much of the seafloor becomes progressively thicker away from mid-ocean ridge axis; seafloor sediment are not as thick as previously thought
Sediment thickness
consists primarily of basalt
Composition of oceanic crust
earthquakes do not occur randomly but define distinct belts (earthquake belts follow trenches, mid-ocean ridges, transform faults)
Distribution of submarine earthquakes
It is a scientific theory that explains how landforms are created from the movement of the Earth.
Plate Tectonics
The Earth’s crust is divided into _____ large plates and into several smaller plates.
Seven
Driven by ______ __________, the lithospheric plates ride over the soft, ductile asthenosphere.
Mantle Convection
Submerged volcanoes are called ____ while those that rise above the ocean surface are called ____ ____ . These features may be isolated or found in clusters or chains.
Seamounts
Volcanic Islands
Primarily, earthquakes & volcanoes occur in a pattern that runs between continents & oceans.
The Coast
Major ____ ____ are often formed inside continents or near their edge.
mountain ranges
(3) Different types of Tectonic Plate Boundaries:
- Convergent Plate Boundaries
- Divergent Plate Boundaries
- Transform Plate Boundaries
Occur when plates collide with each other. Volcanoes & earthquakes commonly occur along these boundaries.
Convergent Plate Boundaries
Occur when plates move away from another. When they move apart, water or magma fills the space & creates new land.
Divergent Plate Boundaries
Are also known as sliding boundaries. They occur when plates slide creating a break in the earth’s surface. This can create a cliff & often causes earthquakes along faults.
Transform Plate Boundaries