key terms
... are considered body waves. continental crust (167): That portion of the Earth’s crust which lies beneath the Earth’s continents. Thickness averages 35 kilometers. It is thicker and less dense than oceanic crust. The continents “float” higher on the denser mantle than the adjacent oceanic crustal seg ...
... are considered body waves. continental crust (167): That portion of the Earth’s crust which lies beneath the Earth’s continents. Thickness averages 35 kilometers. It is thicker and less dense than oceanic crust. The continents “float” higher on the denser mantle than the adjacent oceanic crustal seg ...
coral reefs - bankstowntafehsc
... - a zone extending from Latitudes 30°N to 30°S of the equator; - water depths from 2 to 30m because they need light to allow the algae (zooxanthellae) to photosynthesise in the coral - warm waters where the water temperature does not fall below 17°C nor exceeds 34˚S with the optimum temperature bein ...
... - a zone extending from Latitudes 30°N to 30°S of the equator; - water depths from 2 to 30m because they need light to allow the algae (zooxanthellae) to photosynthesise in the coral - warm waters where the water temperature does not fall below 17°C nor exceeds 34˚S with the optimum temperature bein ...
Quaternary Climate Change and Geomorphology
... Periglacial zones- areas lying in the foreland of the glaciers, areas that were never covered by ice, but received extensive modification by erosional/depositional processes of meltwater. As well as sites of cold climate weathering/mass wasting processes (freeze/thaw, and permafrost conditions) (a) ...
... Periglacial zones- areas lying in the foreland of the glaciers, areas that were never covered by ice, but received extensive modification by erosional/depositional processes of meltwater. As well as sites of cold climate weathering/mass wasting processes (freeze/thaw, and permafrost conditions) (a) ...
Weathering and Erosion
... True or False: The Earth’s surface has stayed the same for thousands of years. Think about the statement in the box above. Do you think it is a true statement or a false statement? Circle True or False on Journal Jam #10. ...
... True or False: The Earth’s surface has stayed the same for thousands of years. Think about the statement in the box above. Do you think it is a true statement or a false statement? Circle True or False on Journal Jam #10. ...
earth science 140 - College of DuPage
... temperature (SST). Also relate the angles of solar energy receipt to the patterns of light distribution with increasing depth that you learned in the previous unit. ...
... temperature (SST). Also relate the angles of solar energy receipt to the patterns of light distribution with increasing depth that you learned in the previous unit. ...
Plate Tectonics Visual Glossary and Atlas
... • Incorporate the definitions contained in the glossary into written evidence. • Visualize data in 3D that is traditionally represented in 2D. ...
... • Incorporate the definitions contained in the glossary into written evidence. • Visualize data in 3D that is traditionally represented in 2D. ...
Sources of Precipitation Over Equatorial Central Africa
... Equatorial Central Africa (hereafter referred to as ECA) is a major global convective region that plays a large role in the global circulation. Additionally, ECA is climatically important due to its extensive rainforest; second largest in the world after the Amazon. Many of the farmers in the area d ...
... Equatorial Central Africa (hereafter referred to as ECA) is a major global convective region that plays a large role in the global circulation. Additionally, ECA is climatically important due to its extensive rainforest; second largest in the world after the Amazon. Many of the farmers in the area d ...
tectonic plates.
... plates are moving away from one another. • The rising current pushes up on the bottom of the lithosphere, lifting it and flowing laterally beneath it. This lateral flow causes the plate material above to be dragged along in the direction of flow. • At the crest of the uplift, the overlying plate is ...
... plates are moving away from one another. • The rising current pushes up on the bottom of the lithosphere, lifting it and flowing laterally beneath it. This lateral flow causes the plate material above to be dragged along in the direction of flow. • At the crest of the uplift, the overlying plate is ...
Version 1
... With offset in the new LOMROG II 2009 hydrographic dataset, a systematic comparison of halocline strength and Atlantic Layer properties with post 1991 cruise data is performed. This recent evolution is referenced to the climatological hydrography of the Arctic Ocean using the PHC 3.0 climatological ...
... With offset in the new LOMROG II 2009 hydrographic dataset, a systematic comparison of halocline strength and Atlantic Layer properties with post 1991 cruise data is performed. This recent evolution is referenced to the climatological hydrography of the Arctic Ocean using the PHC 3.0 climatological ...
What is plate tectonics?
... the temperatures there are adequate to melt the iron-nickel alloy. However, the inner core is a solid even though its temperature is higher than the outer core. Here, tremendous pressure, produced by the weight of the overlying rocks is strong enough to crowd the atoms tightly together and prevents ...
... the temperatures there are adequate to melt the iron-nickel alloy. However, the inner core is a solid even though its temperature is higher than the outer core. Here, tremendous pressure, produced by the weight of the overlying rocks is strong enough to crowd the atoms tightly together and prevents ...
1 Mapping in the Arctic Ocean in Support of a Potential Extended
... in the vicinity of 82° N and 162° W. Surveying continued east to follow the morphologic expression of the base of the slope until approximately 150° W where the character of the base of the slope changed and the surveying switched to a reconnaissance mode. This mode of survey continued until the eas ...
... in the vicinity of 82° N and 162° W. Surveying continued east to follow the morphologic expression of the base of the slope until approximately 150° W where the character of the base of the slope changed and the surveying switched to a reconnaissance mode. This mode of survey continued until the eas ...
Gordon_S_Atl_Ventilation_DSR81.pdf
... water characteristics of North Atlantic Deep Water and Antarctic Bottom Water (Wt~sL 1935; REID et al., 1977). The North Atlantic Deep Water characteristic high salinity is surprisingly coherent with the intensity of the thermocline signal, though Antarctic Bottom Water is not coherent. Thus, the po ...
... water characteristics of North Atlantic Deep Water and Antarctic Bottom Water (Wt~sL 1935; REID et al., 1977). The North Atlantic Deep Water characteristic high salinity is surprisingly coherent with the intensity of the thermocline signal, though Antarctic Bottom Water is not coherent. Thus, the po ...
GEOLOGY FOR MINING ENGINEERS
... the atmosphere; and frozen in glaciers. It also includes ground water present in soil and rock to a depth of at least 2 kilometers. The atmosphere is a mixture of gases, mostly nitrogen and oxygen. It is held to the Earth by gravity and thins rapidly with altitude. Ninety‐nine percent is concentrat ...
... the atmosphere; and frozen in glaciers. It also includes ground water present in soil and rock to a depth of at least 2 kilometers. The atmosphere is a mixture of gases, mostly nitrogen and oxygen. It is held to the Earth by gravity and thins rapidly with altitude. Ninety‐nine percent is concentrat ...
Continental erosion and the Cenozoic rise of marine diatoms
... northward, intermediate waters feed low-latitude ecosystems, yet, in this ocean configuration, the Southern Ocean acts as a trap for H4SiO4 (25). The Antarctic Bottom Water (AABW) circulation cell is closed by AABW mixing into North Atlantic Depth Water (NADW). The dissolution of sinking opal from p ...
... northward, intermediate waters feed low-latitude ecosystems, yet, in this ocean configuration, the Southern Ocean acts as a trap for H4SiO4 (25). The Antarctic Bottom Water (AABW) circulation cell is closed by AABW mixing into North Atlantic Depth Water (NADW). The dissolution of sinking opal from p ...
Sample Exam Geology
... d. northward movement of India into Eurasia 61. Pull-apart zones are generally associated with a ____________ plate boundary. a. transform b. divergent c. convergent d. all plate boundaries 62. A very long-lived magma source located deep in the mantle is called a ____________. a. magma welt b. basal ...
... d. northward movement of India into Eurasia 61. Pull-apart zones are generally associated with a ____________ plate boundary. a. transform b. divergent c. convergent d. all plate boundaries 62. A very long-lived magma source located deep in the mantle is called a ____________. a. magma welt b. basal ...
Ecological values of the 12 miles zone of Bonaire
... allow photosynthesis. It is therefore also called the photic or sunlight zone. It extends from the surface to 200 meters. The part of this zone above the drop-off of the continental shelf is called the neritic zone, the part beyond the shelf break is the oceanic zone. ...
... allow photosynthesis. It is therefore also called the photic or sunlight zone. It extends from the surface to 200 meters. The part of this zone above the drop-off of the continental shelf is called the neritic zone, the part beyond the shelf break is the oceanic zone. ...
lecture notes
... Sand is easily erosed because it is small and not cohesive As energy decreases, particles are deposited according to size (weight) with the largest first and smallest last More energy is required to erode than transport a particle Sedimentation in the ocean ...
... Sand is easily erosed because it is small and not cohesive As energy decreases, particles are deposited according to size (weight) with the largest first and smallest last More energy is required to erode than transport a particle Sedimentation in the ocean ...
Intro to plate tectonics
... America, two far away places. Mesosaurus was a freshwater animal, and could not have crossed the Atlantic Ocean, this indicates that the two continents used to be joined together. • Marsupials are only found in Australia because it drifted away from the main supercontinent before the predators that ...
... America, two far away places. Mesosaurus was a freshwater animal, and could not have crossed the Atlantic Ocean, this indicates that the two continents used to be joined together. • Marsupials are only found in Australia because it drifted away from the main supercontinent before the predators that ...
The Earth`s structure
... of hot mantle material) located right underneath where Iceland has formed. This would mean that more material would be erupted in the Iceland area compared with if there was just the divergent boundary without the plume underneath it. ...
... of hot mantle material) located right underneath where Iceland has formed. This would mean that more material would be erupted in the Iceland area compared with if there was just the divergent boundary without the plume underneath it. ...
CHAPTER 3
... between continents. These included: a. the distribution of fossils, b. patterns of major geologic features such as faults and mountain ranges, and c. the locations of distinctive rock formations. - Edward Suess, an Austrian geologist, suggested that the Southern Hemisphere continents had once been j ...
... between continents. These included: a. the distribution of fossils, b. patterns of major geologic features such as faults and mountain ranges, and c. the locations of distinctive rock formations. - Edward Suess, an Austrian geologist, suggested that the Southern Hemisphere continents had once been j ...
The Mysterious Planet Earth - Japan Agency for Marine
... Where two plates of oceanic crust collide the colder, older plate is forced to subduct and takes water in the rocks down into the mantle. Because mantle material melts at a lower temperature if water is present, molten rock is generated. This rises buoyantly and accretes to the oceanic crust that is ...
... Where two plates of oceanic crust collide the colder, older plate is forced to subduct and takes water in the rocks down into the mantle. Because mantle material melts at a lower temperature if water is present, molten rock is generated. This rises buoyantly and accretes to the oceanic crust that is ...
Our Australia - One Place, Many Stories: Oceans
... The Leeuwin Current runs south along the west coast of Australia, around the south-west corner, and all the way across the Great Australian Bight to Tasmania. Originating in the Indian Ocean, it is the longest coastal current in the world, travelling for about 5000 kilometres along a pathway less th ...
... The Leeuwin Current runs south along the west coast of Australia, around the south-west corner, and all the way across the Great Australian Bight to Tasmania. Originating in the Indian Ocean, it is the longest coastal current in the world, travelling for about 5000 kilometres along a pathway less th ...
CLS Optical Metrology Facility - Overview
... the length of the surface. Typically three tangential and three sagittal slope profiles are acquired for a complete measurement of an optical surface. The FI measures the height map of the optical surface component. The radius of curvature and slope error can then be calculated from this surface hei ...
... the length of the surface. Typically three tangential and three sagittal slope profiles are acquired for a complete measurement of an optical surface. The FI measures the height map of the optical surface component. The radius of curvature and slope error can then be calculated from this surface hei ...
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.