Unit VI: Circulation of the Solid Earth
... a. Divergent Margins: where Earth’s lithosphere is being pulled apart. b. Convergent Margins: where two plates are forced together (subduction/collision). c. Transform Margins: Where two plates slide past each other. Examples? Southern California and the San Andreas fault ...
... a. Divergent Margins: where Earth’s lithosphere is being pulled apart. b. Convergent Margins: where two plates are forced together (subduction/collision). c. Transform Margins: Where two plates slide past each other. Examples? Southern California and the San Andreas fault ...
Volcanoes
... Dike: Magma that cuts across preexisting rock Laccolith: small pool of magma that collects just under Earth’s surface Pluton: Intrusive igneous rocks formed by converging plates Sill: Pool of solidified magma in between rock layers Stock: Small batholith ...
... Dike: Magma that cuts across preexisting rock Laccolith: small pool of magma that collects just under Earth’s surface Pluton: Intrusive igneous rocks formed by converging plates Sill: Pool of solidified magma in between rock layers Stock: Small batholith ...
The Geology of North America as Illustrated by Native American
... Then the healer told his assistants to dig a large circular trench around the roots of the tree. They dug so far that the woman, the tree, and the earth clinging to its roots fell from the sky. For this reason the woman is called Woman-Who-Fell-From-theSky. The swans saw the woman falling from the s ...
... Then the healer told his assistants to dig a large circular trench around the roots of the tree. They dug so far that the woman, the tree, and the earth clinging to its roots fell from the sky. For this reason the woman is called Woman-Who-Fell-From-theSky. The swans saw the woman falling from the s ...
Earth`s Composition
... really easy to bend, and the silly putty will take the shape of its container over time. Because of this property, the asthenosphere is classified differently than the lithosphere. The lower mantle is also known as the mesophere. The average temperature of this layer is about 2000ºC. It is the botto ...
... really easy to bend, and the silly putty will take the shape of its container over time. Because of this property, the asthenosphere is classified differently than the lithosphere. The lower mantle is also known as the mesophere. The average temperature of this layer is about 2000ºC. It is the botto ...
PowerPoint - Science A 2 Z
... Are learning what the interior of the Earth is made of/how it’s arranged. Are learning the geological history of the Earth. ...
... Are learning what the interior of the Earth is made of/how it’s arranged. Are learning the geological history of the Earth. ...
The Earth As A System
... producers and other consumers. • Decomposers – Bacteria and fungi that break down detritus to make nutrients available to plants again. ...
... producers and other consumers. • Decomposers – Bacteria and fungi that break down detritus to make nutrients available to plants again. ...
Notes class_5_6_7
... of continents. This material may be new rock material added by subduction, island arcs developed away from the continents or fragments of old continents. ...
... of continents. This material may be new rock material added by subduction, island arcs developed away from the continents or fragments of old continents. ...
OCN 201: Plate Tectonics II
... – Continental crust probably formed by a second stage of melting… – Water driven off subducting oceanic crust at depth is added to mantle wedge overriding the downgoing plate lowers melting point, mantle melts with different composition, produces andesitic magma which rises to form volcanic arc ...
... – Continental crust probably formed by a second stage of melting… – Water driven off subducting oceanic crust at depth is added to mantle wedge overriding the downgoing plate lowers melting point, mantle melts with different composition, produces andesitic magma which rises to form volcanic arc ...
17.3-homework - Maples Elementary School
... Name __________________________________________________________________________ Date_________________________________ Hour__________________ 17.3 Theory of Plate Tectonics __________1. Which theory states that Earth’s crust and rigid upper mantle move in different directions and at different rates o ...
... Name __________________________________________________________________________ Date_________________________________ Hour__________________ 17.3 Theory of Plate Tectonics __________1. Which theory states that Earth’s crust and rigid upper mantle move in different directions and at different rates o ...
File
... watch the convection currents move in the liquid. When the convection currents flow in the asthenosphere they also move the crust. The crust gets a free ride with these currents, like the cork in this illustration http://www.absorblearning.com/media/attachment.a ...
... watch the convection currents move in the liquid. When the convection currents flow in the asthenosphere they also move the crust. The crust gets a free ride with these currents, like the cork in this illustration http://www.absorblearning.com/media/attachment.a ...
Soils NR 200
... The surface mantel is named in the normal way (e.g. as a Regosol, Andosol or Arenosol) and the buried soil would be classified with a prefix qualifier `thapto-`. If the surface mantle is less than 50 cm thick, it is ignored in the soil name but the soil may be marked on the soil map by a phase indic ...
... The surface mantel is named in the normal way (e.g. as a Regosol, Andosol or Arenosol) and the buried soil would be classified with a prefix qualifier `thapto-`. If the surface mantle is less than 50 cm thick, it is ignored in the soil name but the soil may be marked on the soil map by a phase indic ...
Layers of the Earth
... Writing Prompts Choose two of Earth’s layers that are next to each other and provide the following: the name of each layer, the relative positions of each (which one is above which one), and the basic characteristics of both layers. Essential Questions 1. What properties are utilized to identify and ...
... Writing Prompts Choose two of Earth’s layers that are next to each other and provide the following: the name of each layer, the relative positions of each (which one is above which one), and the basic characteristics of both layers. Essential Questions 1. What properties are utilized to identify and ...
Video: Planet Earth, The Living Machine
... plates were pulling apart here, forming the fault zone. Compressional forces now make this one of the most dangerous fault zones. ...
... plates were pulling apart here, forming the fault zone. Compressional forces now make this one of the most dangerous fault zones. ...
Video: Planet Earth, The Living Machine
... plates were pulling apart here, forming the fault zone. Compressional forces now make this one of the most dangerous fault zones. ...
... plates were pulling apart here, forming the fault zone. Compressional forces now make this one of the most dangerous fault zones. ...
Lecture Notes on Convection and Plate Tectonics
... II. Convection in Earth's Mantle A. Environmental Conditions in Earth's Interior 1. As you go deeper into Earth's interior, the temperature continually 2. Will this type of temperature distribution encourage convection? 3. What are the sources of heat in Earth's interior? a. b. ...
... II. Convection in Earth's Mantle A. Environmental Conditions in Earth's Interior 1. As you go deeper into Earth's interior, the temperature continually 2. Will this type of temperature distribution encourage convection? 3. What are the sources of heat in Earth's interior? a. b. ...
Scaling the Earth`s Interior A wedge of Earth
... layer, relatively speaking, consists of huge plates that migrate over the surface of the globe. The lower portion of this layer, though solid is still considered part of the mantle. Firmly joined above to this lower portion of plate, is the layer we live on, the crust. The crust is the thinnest, mos ...
... layer, relatively speaking, consists of huge plates that migrate over the surface of the globe. The lower portion of this layer, though solid is still considered part of the mantle. Firmly joined above to this lower portion of plate, is the layer we live on, the crust. The crust is the thinnest, mos ...
South Carolina Sample Questions 8th Grade Science
... Caroline tested the rate of evaporation for 4 liquids by placing 100 mL of each liquid into separate Petri dishes. She waited 24 hours before measuring the amount of liquid left in each dish. The results are shown in the table. ...
... Caroline tested the rate of evaporation for 4 liquids by placing 100 mL of each liquid into separate Petri dishes. She waited 24 hours before measuring the amount of liquid left in each dish. The results are shown in the table. ...
Chapter 6 Plate Tectonics
... southern Africa, South America, India and Australia Large coal deposits were formed from tropical swamps in both N. America and Europe at the same time ...
... southern Africa, South America, India and Australia Large coal deposits were formed from tropical swamps in both N. America and Europe at the same time ...
C3 Chemicals in our Lives Revision ppt
... C3 Journey through Time LO: to explain how Britain came into existence as continents, how different climates Britain has experienced and magnetic clues that geologists use to track continents ...
... C3 Journey through Time LO: to explain how Britain came into existence as continents, how different climates Britain has experienced and magnetic clues that geologists use to track continents ...
TECTONIC PLATES
... The locations of volcanoes can also help identify the locations of plate boundaries. Some volcanoes form when plate motions generate magma that erupts on Earth’s surface. For example, the Pacific Ring of Fire is a zone of active volcanoes that encircles the Pacific Ocean. This zone is also one of Ea ...
... The locations of volcanoes can also help identify the locations of plate boundaries. Some volcanoes form when plate motions generate magma that erupts on Earth’s surface. For example, the Pacific Ring of Fire is a zone of active volcanoes that encircles the Pacific Ocean. This zone is also one of Ea ...
Earth`s Layers Lesson Plan - elementaryscienceteachers
... Vocabulary: crust, mantle, inner core, outer core, describe Bloom’s: Remembering Understanding Applying Analyzing Evaluation Creating Questions: How many layers does the Earth have? Tell me the names of the layers of the Earth? Describe what the crust looks like. Describe what the mantle is. ...
... Vocabulary: crust, mantle, inner core, outer core, describe Bloom’s: Remembering Understanding Applying Analyzing Evaluation Creating Questions: How many layers does the Earth have? Tell me the names of the layers of the Earth? Describe what the crust looks like. Describe what the mantle is. ...
Geology
Geology (from the Greek γῆ, gē, i.e. ""earth"" and -λoγία, -logia, i.e. ""study of, discourse"") is an earth science comprising the study of solid Earth, the rocks of which it is composed, and the processes by which they change. Geology can also refer generally to the study of the solid features of any celestial body (such as the geology of the Moon or Mars).Geology gives insight into the history of the Earth by providing the primary evidence for plate tectonics, the evolutionary history of life, and past climates. Geology is important for mineral and hydrocarbon exploration and exploitation, evaluating water resources, understanding of natural hazards, the remediation of environmental problems, and for providing insights into past climate change. Geology also plays a role in geotechnical engineering and is a major academic discipline.