
Environmental Science Chapter 3 Section 1
... tectonic plate – a block of lithosphere that consists of the crust and the rigid, outermost part of the mantle the continents are located on tectonic plates and move around with them much of the geologic activity at the surface of the Earth takes place at the boundaries between tectonic plates ...
... tectonic plate – a block of lithosphere that consists of the crust and the rigid, outermost part of the mantle the continents are located on tectonic plates and move around with them much of the geologic activity at the surface of the Earth takes place at the boundaries between tectonic plates ...
Study Guide 1
... Plate Tectonics Alfred Wegener’s observations supporting Continental Drift Differences between Plate Tectonics and Continental Drift Features of divergent, convergent, transform fault boundaries Layers of the Earth and their features, based on physical properties lithosphere (includes both crust ...
... Plate Tectonics Alfred Wegener’s observations supporting Continental Drift Differences between Plate Tectonics and Continental Drift Features of divergent, convergent, transform fault boundaries Layers of the Earth and their features, based on physical properties lithosphere (includes both crust ...
A note on the gravitational field of the right rectangular prism
... The recently released global crustal model CRUST 2.0 has been validated both globally and regionally focusing on its information content regarding the crust-mantle boundary. The numerical assessment of the metric information given by the database in terms of thickness and position of individual crus ...
... The recently released global crustal model CRUST 2.0 has been validated both globally and regionally focusing on its information content regarding the crust-mantle boundary. The numerical assessment of the metric information given by the database in terms of thickness and position of individual crus ...
Plate Tectonics
... ■ Although the jigsaw-puzzle fit of the southern continents was noted, opponents of Continental Drift argued that, even if continental displacement had occurred, a good fit between the continents today would be unlikely. What geological evidence did they cite to support this claim? – A) Deposition i ...
... ■ Although the jigsaw-puzzle fit of the southern continents was noted, opponents of Continental Drift argued that, even if continental displacement had occurred, a good fit between the continents today would be unlikely. What geological evidence did they cite to support this claim? – A) Deposition i ...
Dynamic Earth Unit 4 Study Guide Ans. key
... What is continental drift? a. Hypothesis where continents were once a single landmass that broke apart and drifted to their present locations. ...
... What is continental drift? a. Hypothesis where continents were once a single landmass that broke apart and drifted to their present locations. ...
Layers of the Earth - Atlanta Public Schools
... • The layer of rock that forms Earth’s outer surface. • The crust is up to 32 Kilometers (20 miles - here to Stone Mountain) thick. • The crust is made up of the continents and the ocean floor. • The crust is thickest under high mountains and thinnest beneath the ocean. • The continental crust consi ...
... • The layer of rock that forms Earth’s outer surface. • The crust is up to 32 Kilometers (20 miles - here to Stone Mountain) thick. • The crust is made up of the continents and the ocean floor. • The crust is thickest under high mountains and thinnest beneath the ocean. • The continental crust consi ...
Layers of the Earth Power Point
... • The layer of rock that forms Earth’s outer surface. • The crust is up to 32 Kilometers (20 miles - here to Stone Mountain) thick. • The crust is made up of the continents and the ocean floor. • The crust is thickest under high mountains and thinnest beneath the ocean. • The continental crust consi ...
... • The layer of rock that forms Earth’s outer surface. • The crust is up to 32 Kilometers (20 miles - here to Stone Mountain) thick. • The crust is made up of the continents and the ocean floor. • The crust is thickest under high mountains and thinnest beneath the ocean. • The continental crust consi ...
Notes Chapter 28
... each other. One result of two plates converging is subduction. A deep oceanic trench marks the boundary between a subducting and an overriding plate at a convergent boundary. ...
... each other. One result of two plates converging is subduction. A deep oceanic trench marks the boundary between a subducting and an overriding plate at a convergent boundary. ...
Evidence for plate tectonics
... Principles of plate tectonics The outermost portion of Earth is composed of a mosaic of thin rigid plates (pieces of lithosphere) that move horizontally with respect to one another Plates interact with each other along their edges (called plate boundaries) Plate boundaries have a high degree of tec ...
... Principles of plate tectonics The outermost portion of Earth is composed of a mosaic of thin rigid plates (pieces of lithosphere) that move horizontally with respect to one another Plates interact with each other along their edges (called plate boundaries) Plate boundaries have a high degree of tec ...
MS Word - Lehigh`s Environmental Initiative
... Investigation 2: How do we recognize plate boundaries? Investigation Sheet http://www.ei.lehigh.edu/learners/tectonics Read all instructions on your handout and answer each question in complete sentences. 1. What major plate lies west of the North American plate? ...
... Investigation 2: How do we recognize plate boundaries? Investigation Sheet http://www.ei.lehigh.edu/learners/tectonics Read all instructions on your handout and answer each question in complete sentences. 1. What major plate lies west of the North American plate? ...
Unit 6: Geology: Plate Tectonics Tectonic Plate Movement
... The ocean plate that is ________________________________________________________________________________________ into the asthenosphere. Typically the ___________________ the rock on the plate, the ________________________________ it will be. Once the plate __________________________________________ ...
... The ocean plate that is ________________________________________________________________________________________ into the asthenosphere. Typically the ___________________ the rock on the plate, the ________________________________ it will be. Once the plate __________________________________________ ...
Question 1:
... The previous figure shows the magnetic anomalies on the Atlantic oceans south of Iceland (bottom) and a cartoon version of the magnetic strip of the oceans at the top: How would explain the pattern of magnetic anomalies? Since through geological observations we know that the magnetic field is not ...
... The previous figure shows the magnetic anomalies on the Atlantic oceans south of Iceland (bottom) and a cartoon version of the magnetic strip of the oceans at the top: How would explain the pattern of magnetic anomalies? Since through geological observations we know that the magnetic field is not ...
divergent boundary
... continent it is called a RIFT or CONTINENTAL RIFT, e.g. African Rift Valley. • Where a divergent boundary forms under the ocean it is called an OCEAN RIDGE. ...
... continent it is called a RIFT or CONTINENTAL RIFT, e.g. African Rift Valley. • Where a divergent boundary forms under the ocean it is called an OCEAN RIDGE. ...
The Sea Floor
... • Composed of plates of crust and upper mantle. • These plates can contain continental/oceanic crusts or both. • The lithosphere floats on the denser, more plastic athenosphere. ...
... • Composed of plates of crust and upper mantle. • These plates can contain continental/oceanic crusts or both. • The lithosphere floats on the denser, more plastic athenosphere. ...
GEOL 106 Earthquake Country Mid Term I Study
... Elastic Rebound Theory: What is this and how does it relate to earthquakes? What event gave rise to this theory? What are the steps in the elastic rebound theory? What earthquake resulted in the evidence that led to this theory? Origin of the Earth and Time: What is the age of the Earth? What are th ...
... Elastic Rebound Theory: What is this and how does it relate to earthquakes? What event gave rise to this theory? What are the steps in the elastic rebound theory? What earthquake resulted in the evidence that led to this theory? Origin of the Earth and Time: What is the age of the Earth? What are th ...
GEOL 106 Earthquake Country Mid Term I Study
... Elastic Rebound Theory: What is this and how does it relate to earthquakes? What event gave rise to this theory? What are the steps in the elastic rebound theory? What earthquake resulted in the evidence that led to this theory? Origin of the Earth and Time: What is the age of the Earth? What are th ...
... Elastic Rebound Theory: What is this and how does it relate to earthquakes? What event gave rise to this theory? What are the steps in the elastic rebound theory? What earthquake resulted in the evidence that led to this theory? Origin of the Earth and Time: What is the age of the Earth? What are th ...
File - Mrs. DeMino`s Science Zone
... The Earth's top layer is covered by large slabs of crust, called tectonic plates. These plates float on the molten rock layer that exists underneath the crust. Earth’s plates are always moving a little, and slight slippage between plates causes tiny earthquakes every day. Sometimes though, two plate ...
... The Earth's top layer is covered by large slabs of crust, called tectonic plates. These plates float on the molten rock layer that exists underneath the crust. Earth’s plates are always moving a little, and slight slippage between plates causes tiny earthquakes every day. Sometimes though, two plate ...
Mid Term I - earthjay science
... Elastic Rebound Theory: What is this and how does it relate to earthquakes? What event gave rise to this theory? What are the steps in the elastic rebound theory? What earthquake resulted in the evidence that led to this theory? Origin of the Earth and Time: What is the age of the Earth? What ar ...
... Elastic Rebound Theory: What is this and how does it relate to earthquakes? What event gave rise to this theory? What are the steps in the elastic rebound theory? What earthquake resulted in the evidence that led to this theory? Origin of the Earth and Time: What is the age of the Earth? What ar ...
File - Ian Whaley Dillman EES
... Subduction Zones and Volcanoes At some convergent boundaries, an oceanic plate collides with a continental plate. Oceanic crust tends to be __Thinner___ and __denser__ than continental crust, so the denser oceanic crust gets bent and pulled under, or ___subducted___, beneath the lighter and thicker ...
... Subduction Zones and Volcanoes At some convergent boundaries, an oceanic plate collides with a continental plate. Oceanic crust tends to be __Thinner___ and __denser__ than continental crust, so the denser oceanic crust gets bent and pulled under, or ___subducted___, beneath the lighter and thicker ...
Earth`s Layered Interior - Donovan
... Middle layer is plastic-like in consistency and allows for the convective flow of materials o Heat rises to the surface, cools and drops back down 2,800 km in thickness and varies in temperature boundary between crust and mantle is known as the MOHO or the Mohorovicic Discontinuity named after ...
... Middle layer is plastic-like in consistency and allows for the convective flow of materials o Heat rises to the surface, cools and drops back down 2,800 km in thickness and varies in temperature boundary between crust and mantle is known as the MOHO or the Mohorovicic Discontinuity named after ...
Plate tectonics
Plate tectonics (from the Late Latin tectonicus, from the Greek: τεκτονικός ""pertaining to building"") is a scientific theory that describes the large-scale motion of Earth's lithosphere. This theoretical model builds on the concept of continental drift which was developed during the first few decades of the 20th century. The geoscientific community accepted the theory after the concepts of seafloor spreading were later developed in the late 1950s and early 1960s.The lithosphere, which is the rigid outermost shell of a planet (on Earth, the crust and upper mantle), is broken up into tectonic plates. On Earth, there are seven or eight major plates (depending on how they are defined) and many minor plates. Where plates meet, their relative motion determines the type of boundary; convergent, divergent, or transform. Earthquakes, volcanic activity, mountain-building, and oceanic trench formation occur along these plate boundaries. The lateral relative movement of the plates typically varies from zero to 100 mm annually.Tectonic plates are composed of oceanic lithosphere and thicker continental lithosphere, each topped by its own kind of crust. Along convergent boundaries, subduction carries plates into the mantle; the material lost is roughly balanced by the formation of new (oceanic) crust along divergent margins by seafloor spreading. In this way, the total surface of the globe remains the same. This prediction of plate tectonics is also referred to as the conveyor belt principle. Earlier theories (that still have some supporters) propose gradual shrinking (contraction) or gradual expansion of the globe.Tectonic plates are able to move because the Earth's lithosphere has greater strength than the underlying asthenosphere. Lateral density variations in the mantle result in convection. Plate movement is thought to be driven by a combination of the motion of the seafloor away from the spreading ridge (due to variations in topography and density of the crust, which result in differences in gravitational forces) and drag, with downward suction, at the subduction zones. Another explanation lies in the different forces generated by the rotation of the globe and the tidal forces of the Sun and Moon. The relative importance of each of these factors and their relationship to each other is unclear, and still the subject of much debate.