File
... 17. What are the three types of plate collisions that occur at convergent boundaries? Oceanic–oceanic convergence: the subduction of one oceanic plate beneath another at a deep-ocean trench. Oceanic–continental convergence: the subduction of a denser oceanic plate beneath a less-dense continental ...
... 17. What are the three types of plate collisions that occur at convergent boundaries? Oceanic–oceanic convergence: the subduction of one oceanic plate beneath another at a deep-ocean trench. Oceanic–continental convergence: the subduction of a denser oceanic plate beneath a less-dense continental ...
Chapter 3 Notes - Todd S. Thuma Homepage
... a. Cools & shrinks denser rock sinks deeper away from ridge b. Sediment gradually builds up, deeper toward basin margins 4. Forms passive ('Atlantic-type') basin margins a. No mountain building or subduction b. Thick sediment and older oceanic crust c. Important economically - oil, gas Oceanograph ...
... a. Cools & shrinks denser rock sinks deeper away from ridge b. Sediment gradually builds up, deeper toward basin margins 4. Forms passive ('Atlantic-type') basin margins a. No mountain building or subduction b. Thick sediment and older oceanic crust c. Important economically - oil, gas Oceanograph ...
Plate Tectonic Notes
... • Mid-Ocean Ridges are found winding around the Earth in all oceans. • They look like mountain ranges. • Most stay under the surface of the water. • Iceland is one area of the mountain range that rises above the surface of the North Atlantic Ocean ...
... • Mid-Ocean Ridges are found winding around the Earth in all oceans. • They look like mountain ranges. • Most stay under the surface of the water. • Iceland is one area of the mountain range that rises above the surface of the North Atlantic Ocean ...
Plate Tectonics
... positions). This was based on observations of similarities in the outlines of continents especially South America and Africa, along with fossil and climate evidence, which seemed to suggest the continents were once connected. This was a radical idea as it was long thought that continents and ocea ...
... positions). This was based on observations of similarities in the outlines of continents especially South America and Africa, along with fossil and climate evidence, which seemed to suggest the continents were once connected. This was a radical idea as it was long thought that continents and ocea ...
"Inside Earth" Chapter 1 Section 4
... Chapter 1, Section 4: Sea-Floor Spreading Evidence for Sea-Floor Spreading * Mid-Ocean Ridges are chains of volcanoes that wind around Earth; the system is more than 50,000 km long. Most of the mountains are deep underwater, but the island of Iceland is a part of a mid-ocean ridge. What is Sea-Floor ...
... Chapter 1, Section 4: Sea-Floor Spreading Evidence for Sea-Floor Spreading * Mid-Ocean Ridges are chains of volcanoes that wind around Earth; the system is more than 50,000 km long. Most of the mountains are deep underwater, but the island of Iceland is a part of a mid-ocean ridge. What is Sea-Floor ...
Geological slant on plates
... overlying crust. Together they form a layer called the lithosphere which is around 50km thick. Although the upper and lower mantle are effectively welded together, there is nevertheless a sharp division between the two called the Moho (Mohorovicic discontinuity), defined by differences in seismic wa ...
... overlying crust. Together they form a layer called the lithosphere which is around 50km thick. Although the upper and lower mantle are effectively welded together, there is nevertheless a sharp division between the two called the Moho (Mohorovicic discontinuity), defined by differences in seismic wa ...
PDF file of Lecture 4a - Earth`s Interior and Tectonics
... Pangaea broke up about 200 my ago and continents slowly moved to present positions ...
... Pangaea broke up about 200 my ago and continents slowly moved to present positions ...
ES Ch 3 Test
... Fill in the line to complete each statement. Continental Drift, Sea-Floor Spreading, Deep-Ocean Trench, Plates, Rift Valley, Mid-Ocean ...
... Fill in the line to complete each statement. Continental Drift, Sea-Floor Spreading, Deep-Ocean Trench, Plates, Rift Valley, Mid-Ocean ...
SEISMIC ACTIVITY (mainly shallow earthquakes)
... TOPOGRAPHY and gravity along mid-ocean-ridges provide important information about processes which are responsible for their formation. The high topography is a result of thermal expansion and lower density (). i.e. a mass-deficiency/volume which is isostatically compensated by the topography (mid- ...
... TOPOGRAPHY and gravity along mid-ocean-ridges provide important information about processes which are responsible for their formation. The high topography is a result of thermal expansion and lower density (). i.e. a mass-deficiency/volume which is isostatically compensated by the topography (mid- ...
Plate Tectonic Theory
... • There are 5 main layers, from surface to center: – Lithosphere (crust): solid outermost layer, about 5-50km deep; – Asthenosphere: the lower layer of the earth's crust; less rigid than the lithosphere—more slushy/flexible – Mantle: region below crust extending down to Earth's core; some molten roc ...
... • There are 5 main layers, from surface to center: – Lithosphere (crust): solid outermost layer, about 5-50km deep; – Asthenosphere: the lower layer of the earth's crust; less rigid than the lithosphere—more slushy/flexible – Mantle: region below crust extending down to Earth's core; some molten roc ...
179 Core Idea ESS2 Earth`s Systems ESS2.A: EARTH MATERIALS
... and the biosphere (living things, including humans). These systems interact in multiple ways to affect Earth’s surface materials and processes. The ocean supports a variety of ecosystems and organisms, shapes landforms, and influences climate. Winds and clouds in the atmosphere interact with the lan ...
... and the biosphere (living things, including humans). These systems interact in multiple ways to affect Earth’s surface materials and processes. The ocean supports a variety of ecosystems and organisms, shapes landforms, and influences climate. Winds and clouds in the atmosphere interact with the lan ...
Table 1. Plate Boundaries of an Unkn
... To complete this worksheet, see the instructions in the textbook (Chapter 3 Investigation). Table 1. Plate Boundaries of an Unknown Ocean and Continents This perspective view shows two continents, labeled A and B, separated by an ocean. • Use the topography to identify possible plate boundaries and ...
... To complete this worksheet, see the instructions in the textbook (Chapter 3 Investigation). Table 1. Plate Boundaries of an Unknown Ocean and Continents This perspective view shows two continents, labeled A and B, separated by an ocean. • Use the topography to identify possible plate boundaries and ...
The Earth Handbook
... As rivers carve through Earth’s surface, carrying water according to gravity from higher to lower ground, they pick up and transport rocks and sediment. This first causes erosion and eventually deposition, when the rivers drop the rocks in the sea or in river beds. (11) Tap the river to speed it up. ...
... As rivers carve through Earth’s surface, carrying water according to gravity from higher to lower ground, they pick up and transport rocks and sediment. This first causes erosion and eventually deposition, when the rivers drop the rocks in the sea or in river beds. (11) Tap the river to speed it up. ...
Marine Primary Productivity: Measurements and Variability
... the Nile Delta. This "Nile bloom" provided sustenance to sardines and other pelagic fishes. It also constituted a large source of detrital material, which forms a vital source of food for commercially valuable organisms such as shrimp. ...
... the Nile Delta. This "Nile bloom" provided sustenance to sardines and other pelagic fishes. It also constituted a large source of detrital material, which forms a vital source of food for commercially valuable organisms such as shrimp. ...
Slide 1
... • Magnetic fields are produced by the motion of electrical charges. For example, the magnetic field of a bar magnet results from the motion of negatively charged electrons in the magnet. • The origin of the Earth's magnetic field is not completely understood, but is thought to be associated with ele ...
... • Magnetic fields are produced by the motion of electrical charges. For example, the magnetic field of a bar magnet results from the motion of negatively charged electrons in the magnet. • The origin of the Earth's magnetic field is not completely understood, but is thought to be associated with ele ...
Plate Tectonics Notes
... Matching rocks on different continents Land animals on different continents Glacial marks in now tropical areas Tropical plants in Antarctica ...
... Matching rocks on different continents Land animals on different continents Glacial marks in now tropical areas Tropical plants in Antarctica ...
Ch 9 ES Website-Coon - Sonoma Valley High School
... exists in the form of several mountain belts that end at one coastline, only to reappear on a landmass across the ocean. ...
... exists in the form of several mountain belts that end at one coastline, only to reappear on a landmass across the ocean. ...
Chapter 9 Plate Tectonics
... Oceanic Ridges and Seafloor Spreading _______________ valleys are deep faulted structures found along the axes of divergent plate boundaries. They can develop on the seafloor or on land. _______________ spreading produces new oceanic lithosphere. _______________ Rifts When spreading center ...
... Oceanic Ridges and Seafloor Spreading _______________ valleys are deep faulted structures found along the axes of divergent plate boundaries. They can develop on the seafloor or on land. _______________ spreading produces new oceanic lithosphere. _______________ Rifts When spreading center ...
Remote Sensing (RS) and Geographic Information Systems (GIS)
... • All major landmasses gather into one supercontinent • Remaining 70% of Earth’s surface is one super-ocean ...
... • All major landmasses gather into one supercontinent • Remaining 70% of Earth’s surface is one super-ocean ...
Sea-Floor Spreading
... sound waves off under-water objects and then records the echoes of these sound waves. The time it takes for the echo to arrive indicates the distance to the object. ...
... sound waves off under-water objects and then records the echoes of these sound waves. The time it takes for the echo to arrive indicates the distance to the object. ...
Plate Tectonics Earth`s outer shell, the lithosphere, long
... As eons pass, continents and other land masses collide, break apart, and drift across the planet on the fiery mantle beneath, opening and closing oceans along the way. Subsequently, their relative position to the equator, the poles, and each other changes over long periods of time. For instance, Afr ...
... As eons pass, continents and other land masses collide, break apart, and drift across the planet on the fiery mantle beneath, opening and closing oceans along the way. Subsequently, their relative position to the equator, the poles, and each other changes over long periods of time. For instance, Afr ...
Basic Act on Ocean Policy (Act No. 33 of April 27, 2007) Table of
... Article 25 (1) The State shall take necessary measures for the coastal sea areas and land areas, where recognized suitable for the measures to be implemented in a unified manner upon the natural and social conditions, to be managed properly, by the regulatory and other measures to the activities imp ...
... Article 25 (1) The State shall take necessary measures for the coastal sea areas and land areas, where recognized suitable for the measures to be implemented in a unified manner upon the natural and social conditions, to be managed properly, by the regulatory and other measures to the activities imp ...
Plate Tectonics Earth`s outer shell, the lithosphere, long thought to
... As eons pass, continents and other land masses collide, break apart, and drift across the planet on the fiery mantle beneath, opening and closing oceans along the way. Subsequently, their relative position to the equator, the poles, and each other changes over long periods of time. For instance, Afr ...
... As eons pass, continents and other land masses collide, break apart, and drift across the planet on the fiery mantle beneath, opening and closing oceans along the way. Subsequently, their relative position to the equator, the poles, and each other changes over long periods of time. For instance, Afr ...
Chapter 9: Our Living Earth PowerPoint print-off
... • Place of maximum surface shaking • Place directly above the focus The focus is also called the hypocenter ...
... • Place of maximum surface shaking • Place directly above the focus The focus is also called the hypocenter ...
Geology of Australia and New Zealand, HWS/UC 2007 2. Plate
... high elevations of the mountain ranges. Also note how relatively thin is the rigid outer part of the earth, the lithosphere. Most of the earth is relatively plastic, i.e. is capable of flowing over geologic periods of time. ...
... high elevations of the mountain ranges. Also note how relatively thin is the rigid outer part of the earth, the lithosphere. Most of the earth is relatively plastic, i.e. is capable of flowing over geologic periods of time. ...
Ocean
An ocean (from Ancient Greek Ὠκεανός, transc. Okeanós, the sea of classical antiquity) is a body of saline water that composes much of a planet's hydrosphere. On Earth, an ocean is one of the major conventional divisions of the World Ocean, which covers almost 71% of its surface. These are, in descending order by area, the Pacific, Atlantic, Indian, Southern, and Arctic Oceans. The word sea is often used interchangeably with ""ocean"" in American English but, strictly speaking, a sea is a body of saline water (generally a division of the world ocean) partly or fully enclosed by land.Saline water covers approximately 72% of the planet's surface (~3.6×108 km2) and is customarily divided into several principal oceans and smaller seas, with the ocean covering approximately 71% of Earth's surface. The ocean contains 97% of Earth's water, and oceanographers have stated that only 5% of the World Ocean has been explored. The total volume is approximately 1.35 billion cubic kilometers (320 million cu mi) with an average depth of nearly 3,700 meters (12,100 ft).As it is the principal component of Earth's hydrosphere, the world ocean is integral to all known life, forms part of the carbon cycle, and influences climate and weather patterns. It is the habitat of 230,000 known species, although much of the oceans depths remain unexplored, and over two million marine species are estimated to exist. The origin of Earth's oceans remains unknown; oceans are thought to have formed in the Hadean period and may have been the impetus for the emergence of life.Extraterrestrial oceans may be composed of water or other elements and compounds. The only confirmed large stable bodies of extraterrestrial surface liquids are the lakes of Titan, although there is evidence for the existence of oceans elsewhere in the Solar System. Early in their geologic histories, Mars and Venus are theorized to have had large water oceans. The Mars ocean hypothesis suggests that nearly a third of the surface of Mars was once covered by water, and a runaway greenhouse effect may have boiled away the global ocean of Venus. Compounds such as salts and ammonia dissolved in water lower its freezing point, so that water might exist in large quantities in extraterrestrial environments as brine or convecting ice. Unconfirmed oceans are speculated beneath the surface of many dwarf planets and natural satellites; notably, the ocean of Europa is estimated to have over twice the water volume of Earth. The Solar System's giant planets are also thought to have liquid atmospheric layers of yet to be confirmed compositions. Oceans may also exist on exoplanets and exomoons, including surface oceans of liquid water within a circumstellar habitable zone. Ocean planets are a hypothetical type of planet with a surface completely covered with liquid.