Deforming the Earth`s Crust
... Rocks that are hot take up more space than cooler rocks ◦ As the lithosphere cools, it becomes denser and takes up less volume causing the crust to sink ...
... Rocks that are hot take up more space than cooler rocks ◦ As the lithosphere cools, it becomes denser and takes up less volume causing the crust to sink ...
Jeopardy - Effingham County Schools
... The lithosphere is broken into sections known as ……, which float on top of the athensophere ...
... The lithosphere is broken into sections known as ……, which float on top of the athensophere ...
Geology - ClassNet
... 33) __________ rocks form the bedrock of part of every province. 34) During the Paleozoic era, the vegetation in huge swamps produced __________ in "Nova ...
... 33) __________ rocks form the bedrock of part of every province. 34) During the Paleozoic era, the vegetation in huge swamps produced __________ in "Nova ...
Ch.2 Tectonics
... and overlying crust) The lithosphere overlies a weaker region in the mantle called the asthenosphere. The plates move relative to each other at a very slow but continuous rate and the rates ...
... and overlying crust) The lithosphere overlies a weaker region in the mantle called the asthenosphere. The plates move relative to each other at a very slow but continuous rate and the rates ...
1 - ClassNet
... 19) the bending of rock layers 20) movement along a crack or faults in the earth's crust 21) rock formed from the cooling of molten rock ...
... 19) the bending of rock layers 20) movement along a crack or faults in the earth's crust 21) rock formed from the cooling of molten rock ...
Changes in the Earth`s surface
... • They are moved slowly around by convection currents in the mantle • This has been happening for billions of years ...
... • They are moved slowly around by convection currents in the mantle • This has been happening for billions of years ...
NAME - Kcse Online
... (d) - The slopes of Fold Mountains which face the sun are warmer than those which face away from the sun. - The windward side slopes of Fold Mountains generally receive higher rainfall than the leeward slopes because of orographic effects. - Mountain slopes cause the developments of anabatic winds w ...
... (d) - The slopes of Fold Mountains which face the sun are warmer than those which face away from the sun. - The windward side slopes of Fold Mountains generally receive higher rainfall than the leeward slopes because of orographic effects. - Mountain slopes cause the developments of anabatic winds w ...
Great Idea: All matter above and beneath Earth`s surface moves in
... The biosphere is the net sum of all of the ecosystems on Earth. It is often referred to as the Earth’s life zone. In the most broad sense of the word, in biophysiology, biosphere is the global ecological system integrating all living beings and their relationships, including their interaction with ...
... The biosphere is the net sum of all of the ecosystems on Earth. It is often referred to as the Earth’s life zone. In the most broad sense of the word, in biophysiology, biosphere is the global ecological system integrating all living beings and their relationships, including their interaction with ...
Lower Mound Unit or Formation
... conformable succession of sedimentary rocks that typically represents a single shallowing upward cycle, bounded by marine flooding surfaces. A parasequence thus represents a single episode of sediment progradation (the seaward movement of shoreline), typically lasting 10’s to 100’s of thousands of y ...
... conformable succession of sedimentary rocks that typically represents a single shallowing upward cycle, bounded by marine flooding surfaces. A parasequence thus represents a single episode of sediment progradation (the seaward movement of shoreline), typically lasting 10’s to 100’s of thousands of y ...
Name____________________________
... the upper mantle. Plate Boundary: Place where two plates meet. Divergent Boundary: Place where two plates pull apart. Convergent Boundary: Place where two plates come together. Transform Boundary: Place where two plates slide past each other. Oceanic Crust: Dense crust formed by seafloor spreading a ...
... the upper mantle. Plate Boundary: Place where two plates meet. Divergent Boundary: Place where two plates pull apart. Convergent Boundary: Place where two plates come together. Transform Boundary: Place where two plates slide past each other. Oceanic Crust: Dense crust formed by seafloor spreading a ...
The Earth was extensively molten in the first 100 million years after
... The Earth was extensively molten in the first 100 million years after its formation. In that span of time, it acquired much of its present-day structure: the metallic core segregated and sank towards the center, while the mantle and crust separated at the surface. The primordial evolution of the man ...
... The Earth was extensively molten in the first 100 million years after its formation. In that span of time, it acquired much of its present-day structure: the metallic core segregated and sank towards the center, while the mantle and crust separated at the surface. The primordial evolution of the man ...
Study Guide
... Evidence: Matching fossils on coastlines of different continents Matching rock layers on coastlines of different continents Tropical plant fossils found in Greenland and Antarctica Continents “fit” together like puzzle pieces Plate tectonics: Earth’s lithosphere is broken into plates that move on th ...
... Evidence: Matching fossils on coastlines of different continents Matching rock layers on coastlines of different continents Tropical plant fossils found in Greenland and Antarctica Continents “fit” together like puzzle pieces Plate tectonics: Earth’s lithosphere is broken into plates that move on th ...
Oceanography 101 Linda Khandro, MAT Homework 2: Opening the
... America separated from Europe. By early in the Tertiary, spreading had stopped in the Labrador Sea. When spreading began in the Norwegian Sea, Greenland started to move away from Europe, along with North America, as part of the North American plate. ...
... America separated from Europe. By early in the Tertiary, spreading had stopped in the Labrador Sea. When spreading began in the Norwegian Sea, Greenland started to move away from Europe, along with North America, as part of the North American plate. ...
view as pdf - KITP Online
... Description of mass (re-)distribution(s) within a planet. High accuracy satellite data and pattern recognition- ...
... Description of mass (re-)distribution(s) within a planet. High accuracy satellite data and pattern recognition- ...
Plate Tectonics, Earthquakes, and Volcanoes Study Guide
... The earthquakes were felt over an area of at least 2 million square miles, from Canada to New Orleans. The earthquakes toppled chimneys as far away as Richmond, Virginia, and Cincinnati Ohio. The shaking rang church bells in Washington D.C. and in Boston 1,100 miles away. The land surface underwent ...
... The earthquakes were felt over an area of at least 2 million square miles, from Canada to New Orleans. The earthquakes toppled chimneys as far away as Richmond, Virginia, and Cincinnati Ohio. The shaking rang church bells in Washington D.C. and in Boston 1,100 miles away. The land surface underwent ...
Earth Science Essential Knowledge and Skills
... estuary – semi-isolated area of the ocean, which is diluted by freshwater drainage from the land ice cap – huge continental glaciers found in polar regions mid-ocean ridge – undersea mountain chain where new ocean floor is produced; a constructive (divergent) plate boundary ...
... estuary – semi-isolated area of the ocean, which is diluted by freshwater drainage from the land ice cap – huge continental glaciers found in polar regions mid-ocean ridge – undersea mountain chain where new ocean floor is produced; a constructive (divergent) plate boundary ...
Unit 3: Forces Within - Lemon Bay High School
... To play go here: jeopardylabs.com/play/unit-3-forces-within jeopardylabs.com/play/unit-3a-forces-within Date ________________ What type of boundary occurs where two plates move together, causing one plate to descend into the mantle beneath the other plate? ...
... To play go here: jeopardylabs.com/play/unit-3-forces-within jeopardylabs.com/play/unit-3a-forces-within Date ________________ What type of boundary occurs where two plates move together, causing one plate to descend into the mantle beneath the other plate? ...
Geology_101_Homework_2
... 2) What is the difference between ductile and brittle behavior for rocks? 3) There are two important brittle-ductile transitions in the upper 600 km of the Earth. In what layers or between which layers are they located? 4) Draw pictures of normal, reverse, and strike-slip faults using arrows to show ...
... 2) What is the difference between ductile and brittle behavior for rocks? 3) There are two important brittle-ductile transitions in the upper 600 km of the Earth. In what layers or between which layers are they located? 4) Draw pictures of normal, reverse, and strike-slip faults using arrows to show ...
Plate tectonics Assignment
... Geologists have gradually rejected the notion of a rigid Earth with fixed continents and ocean basins. Most now believe that the Earth’s crust is made up of about a dozen plates, which, for reasons not fully understood, move over the interior. Your task is to research some of the ideas that have led ...
... Geologists have gradually rejected the notion of a rigid Earth with fixed continents and ocean basins. Most now believe that the Earth’s crust is made up of about a dozen plates, which, for reasons not fully understood, move over the interior. Your task is to research some of the ideas that have led ...
Earthquake Notes
... Fault - A fracture in the earthʼs crust where there has already been some movement Focus - Point of origin of earthquakes where waves travel outward in all directions Crust - Outermost layer of the earth Mantle - A layer of earth that lies beneath the crust Lithosphere - Outer portion of the earth c ...
... Fault - A fracture in the earthʼs crust where there has already been some movement Focus - Point of origin of earthquakes where waves travel outward in all directions Crust - Outermost layer of the earth Mantle - A layer of earth that lies beneath the crust Lithosphere - Outer portion of the earth c ...
document
... On the Richter scale, a III level earthquake and a IV level earthquake were measured. How many times stronger was the IV compared to the III? [Question from ‘08 STAR test] ...
... On the Richter scale, a III level earthquake and a IV level earthquake were measured. How many times stronger was the IV compared to the III? [Question from ‘08 STAR test] ...
Geology of Planet Earth
... After answering the questions below and enter your final answers on Moodle. 1. What is the most likely geologic hazard in your part of the country? Is there more than one, if so what are they? 2. What are the three types of plate boundaries and where does each most commonly occur on the Earth? Circl ...
... After answering the questions below and enter your final answers on Moodle. 1. What is the most likely geologic hazard in your part of the country? Is there more than one, if so what are they? 2. What are the three types of plate boundaries and where does each most commonly occur on the Earth? Circl ...
Post-glacial rebound
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Post-glacial rebound (sometimes called continental rebound) is the rise of land masses that were depressed by the huge weight of ice sheets during the last glacial period, through a process known as isostatic depression. Post-glacial rebound and isostatic depression are different parts of a process known as either glacial isostasy, glacial isostatic adjustment, or glacioisostasy. Glacioisostasy is the solid Earth deformation associated with changes in ice mass distribution. The most obvious and direct affects of post-glacial rebound are readily apparent in northern Europe (especially Scotland, Estonia, Latvia, Fennoscandia, and northern Denmark), Siberia, Canada, the Great Lakes of Canada and the United States, the coastal region of the US state of Maine, parts of Patagonia, and Antarctica. However, through processes known as ocean siphoning and continental levering, the effects of post-glacial rebound on sea-level are felt globally far from the locations of current and former ice sheets.