The features of plate tectonics

Students build sea floor models showing ages of the rock combined with a written assignment explaining sea floor spread to parents. The same holds for the African, Eurasianand Antarctic plates. Geological field work varies depending on the task at hand. Deformational events are often also associated with volcanism and igneous activity.

Greater understanding of the ocean floor and the discoveries of features like mid-oceanic ridges, geomagnetic anomalies The features of plate tectonics to the mid-oceanic ridges, and the association of island arcs and oceanic trenches occurring together and near the continental margins, suggested convection might indeed be at work.

Therefore, when various scientists during the early sixties started to reason on the data at their disposal regarding the ocean floor, the pieces of the theory quickly fell into place.

Certainly there is no evidence that the moon has expanded in the past 3 billion years; other work would soon show that the evidence was equally in support of continental drift on a globe with a stable radius. Where this occurs an oceanic trench forms on the sea floor and the sinking plate becomes a subduction zone.

Because the Pacific Plate is one of the faster moving plates, this type of volcanism produces linear chains of islands and seamounts, such as the Hawaiian - Emperor chain, the Line Islands, the Marshall-Ellice Islands, and the Austral seamount chain.

Physical Geology by Carla W. This gravitational sliding represents a secondary phenomenon of this basically vertically oriented mechanism.

In effect, the ocean basins are perpetually being "recycled," with the creation of new crust and the destruction of old oceanic lithosphere occurring simultaneously. Reasoning in an opposite way, the continents might have shifted and rotated, while the pole remained relatively fixed.

Plate Tectonics Map - Plate Boundary Map

Many of these organisms could not have traveled across the vast oceans that currently exist. If this is the case, then it can also convect. Major features of California geology, including the Channel Islands, are the result of plate tectonics. The concept that mountains had "roots" was confirmed by George B.

Most earthquakes occur in narrow belts that correspond to the locations of lithospheric plate boundaries. When rock units are placed under horizontal compressionthey shorten and become thicker. The addition of new rock units, both depositionally and intrusively, often occurs during deformation.

In the previous lesson and performance assessment, students learned that different landforms develop on plate boundaries. Roll over the images and click on the zoom tool to take a close look. Previously, geologists could only use fossils and stratigraphic correlation to date sections of rock relative to one another.

All students in the class collaborate using a process to assemble 18 pieces of the crust into a whole.

In the diagram to the right, the dark stripes represent The features of plate tectonics floor generated during "reversed" polar orientation and the lighter stripes represent the polar orientation we have today. As the ocean floor is spread apart cracks appear in the middle of the ridges allowing molten magma to surface through the cracks to form the newest ocean floor.

The magnetic north and south poles reverse through time, and, especially important in paleotectonic studies, the relative position of the magnetic north pole varies through time. The shaded stripes also represent older and older rock as they move away from the mid-oceanic ridge.

The Hawaiian Islandsfor example, consist almost entirely of layered basaltic lava flows. Wegener could not explain the force that drove continental drift, and his vindication did not come until after his death in Magma intruding into the ridge would push lithosphere apart at the ridge.

Oceanic crust is denser because it has less silicon and more heavier elements " mafic " than continental crust " felsic ". Many of these organisms could not have traveled across the vast oceans that currently exist.

Certainly there is no evidence that the moon has expanded in the past 3 billion years; other work would soon show that the evidence was equally in support of continental drift on a globe with a stable radius.Plate tectonics also has provided a mechanism for Alfred Wegener's theory of continental drift, in which the continents move across the surface of the Earth over geologic time.

They also provided a driving force for crustal deformation, and a new setting for the observations of structural geology. The Plate Tectonics Teaching Packet is available for purchase here. Click here for Table of Contents. Over pages of ready-to-run materials covering: The Theory of Plate Tectonics.

Plate tectonics has revolutionized virtually every discipline of the Earth sciences since the late s and early s. It has served as a unifying model or paradigm for explaining geologic phenomena that were formerly considered in unrelated fashion.

Plate tectonics describes seismic activity. From the deepest ocean trench to the tallest mountain, plate tectonics explains the features and movement of Earth's surface in the present and the past.

Plate tectonics is the theory that Earth's. Plate tectonics, from Greek "builder" or "mason", is a theory of geology that has been developed to explain the observed evidence for large scale motions of the Earth's lithosphere.

What Is Plate Tectonics?

Plate tectonics (from the Late Latin tectonicus, from the Greek: τεκτονικός "pertaining to building") is a scientific theory describing the large-scale motion of seven large plates and the movements of a larger number of smaller plates of the Earth's lithosphere, since tectonic processes began on Earth between 3 and billion years model .

The features of plate tectonics
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