 
									
								
									Convergent boundary
									
... Earth is probably not built of uniform layers, it is likely mixed somewhat by convection ...
                        	... Earth is probably not built of uniform layers, it is likely mixed somewhat by convection ...
									hot, less dense material is forced upward by the surrounding cooler
									
... The plates can move in opposite directions  The plates can also move in the same direction, but at different rates ...
                        	... The plates can move in opposite directions  The plates can also move in the same direction, but at different rates ...
									Geology The difference between rocks and minerals
									
... 1. First make the 'cone' of the baking soda volcano. Mix 6 cups flour, 2 cups salt, 4 tablespoons cooking oil, and 2 cups of water. The resulting mixture should be smooth and firm (more water may be added if needed). 2. Stand a soda bottle in the baking pan and mold the dough around it into a volca ...
                        	... 1. First make the 'cone' of the baking soda volcano. Mix 6 cups flour, 2 cups salt, 4 tablespoons cooking oil, and 2 cups of water. The resulting mixture should be smooth and firm (more water may be added if needed). 2. Stand a soda bottle in the baking pan and mold the dough around it into a volca ...
									APES Unit 2 – Review Sheet
									
... i. Density – most dense in center & least dense at surface ii. Composition – core = metal; mantle & crust = rock iii. Source of heat – radioactive decay of U and Pt (fission) c. Sequence of layers – crust, lithosphere, asthenosphere (upper mantle), mantle, outer core, and inner core. 3. List Wegener ...
                        	... i. Density – most dense in center & least dense at surface ii. Composition – core = metal; mantle & crust = rock iii. Source of heat – radioactive decay of U and Pt (fission) c. Sequence of layers – crust, lithosphere, asthenosphere (upper mantle), mantle, outer core, and inner core. 3. List Wegener ...
									Earths Layer Model
									
... Students will learn about the earth’s layers and make a model. They will explore the layers of earth through an interactive board where they can test their knowledge. Then they will do an activity where they make a 3D model of the earth’s layers with a half of a foam ball. Students will color code e ...
                        	... Students will learn about the earth’s layers and make a model. They will explore the layers of earth through an interactive board where they can test their knowledge. Then they will do an activity where they make a 3D model of the earth’s layers with a half of a foam ball. Students will color code e ...
									Our Haven, Planet Earth
									
... The information we have concerning the composition of the stars, planets, their satellites (or moons) and comets has been obtained from astronomical observations conducted from Earth and, more recently, from observations obtained by spacecraft launched from Earth to explore our galaxy. The astronomi ...
                        	... The information we have concerning the composition of the stars, planets, their satellites (or moons) and comets has been obtained from astronomical observations conducted from Earth and, more recently, from observations obtained by spacecraft launched from Earth to explore our galaxy. The astronomi ...
									Word - State of New Jersey
									
... temperatures and density in these investigations so that students understand the cycling of matter due to the outward flow of energy from Earth’s interior and the gravitational movement of denser materials toward the interior. Further discussion of this topic should emphasize how areas of tension ov ...
                        	... temperatures and density in these investigations so that students understand the cycling of matter due to the outward flow of energy from Earth’s interior and the gravitational movement of denser materials toward the interior. Further discussion of this topic should emphasize how areas of tension ov ...
									Ch 8 Archean
									
...  Also, ultramafic extrusive igneous rocks were more common due to the higher temperatures ...
                        	...  Also, ultramafic extrusive igneous rocks were more common due to the higher temperatures ...
									Expedition Worksheet
									
... appeared that the oceanic lithosphere should be older with greater distance from the center of the mid-ocean ridge where it first formed By matching the reversal history to the magnetic patterns under the sea, and assuming seafloor spreading, the age of a particular piece of oceanic lithosphere coul ...
                        	... appeared that the oceanic lithosphere should be older with greater distance from the center of the mid-ocean ridge where it first formed By matching the reversal history to the magnetic patterns under the sea, and assuming seafloor spreading, the age of a particular piece of oceanic lithosphere coul ...
									Grid phenomenon, alignment of formations, ordered
									
... As the basic mechanism controlling a ordering in redistribution of various formations of celestial bodies the mechanism of the forced relative swing and displacements of the basic shells of a planet (satellite) along the certain primary radial directions and the mechanism of excitation of elastic wa ...
                        	... As the basic mechanism controlling a ordering in redistribution of various formations of celestial bodies the mechanism of the forced relative swing and displacements of the basic shells of a planet (satellite) along the certain primary radial directions and the mechanism of excitation of elastic wa ...
									Document
									
... fluid dynamical ones. With the advent of more powerful supercomputers major advances have been made in recent years. ...
                        	... fluid dynamical ones. With the advent of more powerful supercomputers major advances have been made in recent years. ...
									22 questions - ReviewEarthScience.com
									
... shallow-water fossils found at great ocean depths marine fossils found at high elevations above sea level younger fossils above older fossils in layers of rock marine fossils found in horizontal sedimentary layers ...
                        	... shallow-water fossils found at great ocean depths marine fossils found at high elevations above sea level younger fossils above older fossils in layers of rock marine fossils found in horizontal sedimentary layers ...
									ROCKS
									
... were formed when lava cooled quickly above ground. You can see where little pockets of air had been. This rock is so light, that many pumice rocks will actually float in water. Pumice is actually a kind of glass and not a mixture of minerals. Because this rock is so light, it is used quite often as ...
                        	... were formed when lava cooled quickly above ground. You can see where little pockets of air had been. This rock is so light, that many pumice rocks will actually float in water. Pumice is actually a kind of glass and not a mixture of minerals. Because this rock is so light, it is used quite often as ...
									Case of the Split Personality Lab #20
									
... Case of the Split Personality Lab #20 Objective: Use a model to simulate the physical properties of the asthenosphere and the movement within it. ...
                        	... Case of the Split Personality Lab #20 Objective: Use a model to simulate the physical properties of the asthenosphere and the movement within it. ...
									see powerpoint
									
... The process by which new oceanic crust forms at mid-ocean ridges as tectonic plates are pulled away from each other. ...
                        	... The process by which new oceanic crust forms at mid-ocean ridges as tectonic plates are pulled away from each other. ...
									Gouiza et al - NSERC
									
... and metamorphosed Archean and Paleoproterozoic rocks of the Hearne and Rae Provinces host unconformity-type uranium deposits which are spatially associated with faults that cut the unconformity between the unmetametamorphosed basin-fill sedimentary rocks and the underlying metamorphic basement rocks ...
                        	... and metamorphosed Archean and Paleoproterozoic rocks of the Hearne and Rae Provinces host unconformity-type uranium deposits which are spatially associated with faults that cut the unconformity between the unmetametamorphosed basin-fill sedimentary rocks and the underlying metamorphic basement rocks ...
									What have we learned?
									
... • Electric currents in the liquid outer core generate a magnetic field • This magnetic field produces a magnetosphere that surrounds the Earth and blocks the solar wind from hitting the atmosphere • Most of the particles of the solar wind are deflected around the Earth by the magnetosphere. ...
                        	... • Electric currents in the liquid outer core generate a magnetic field • This magnetic field produces a magnetosphere that surrounds the Earth and blocks the solar wind from hitting the atmosphere • Most of the particles of the solar wind are deflected around the Earth by the magnetosphere. ...
									01 - 6th Grade Science with Mrs. Harlow
									
... Rain, flash floods, and mudslides occur in places where there is normally little rain and droughts in areas that are used to a lot of rain. 19. In what direction does an undertow flow? This subsurface current pulls objects straight out to sea in the opposite direction of the waves. 20. How does an e ...
                        	... Rain, flash floods, and mudslides occur in places where there is normally little rain and droughts in areas that are used to a lot of rain. 19. In what direction does an undertow flow? This subsurface current pulls objects straight out to sea in the opposite direction of the waves. 20. How does an e ...
									Semester 1 Course Review
									
... 1. How do seismic waves provide a detailed picture of Earth’s interior? 2. What are the names of the internal layers of the Earth and what is the composition of each layer? 3. How does the outer core produce the Earth’s magnetic field? 4. How is heat transferred from the core to the crust? 5. Who co ...
                        	... 1. How do seismic waves provide a detailed picture of Earth’s interior? 2. What are the names of the internal layers of the Earth and what is the composition of each layer? 3. How does the outer core produce the Earth’s magnetic field? 4. How is heat transferred from the core to the crust? 5. Who co ...
									Dissolution-precipitation creep at mid
									
... The enrichment of Ca in Plag2 could reflect either a difference in the PT conditions compared to the growth of Plag1 or a possible metasomatic event characterized by an influx of a Ca-rich fluid, as suggested by the presence of intergranular calcite crystals as well as discrete calcite veins. The X- ...
                        	... The enrichment of Ca in Plag2 could reflect either a difference in the PT conditions compared to the growth of Plag1 or a possible metasomatic event characterized by an influx of a Ca-rich fluid, as suggested by the presence of intergranular calcite crystals as well as discrete calcite veins. The X- ...
									First Hour Exam Answers
									
... of continental margins, that support the combined theories of continental drift and plate tectonics, and indicate how each line of evidence supports these concepts. Avoid circular reasoning (i.e., don't use plate tectonics as evidence for plate tectonics!). (10 points: 4-3-3) (1) Identical plant and ...
                        	... of continental margins, that support the combined theories of continental drift and plate tectonics, and indicate how each line of evidence supports these concepts. Avoid circular reasoning (i.e., don't use plate tectonics as evidence for plate tectonics!). (10 points: 4-3-3) (1) Identical plant and ...
Geophysics
 
                        Geophysics /dʒiːoʊfɪzɪks/ is a subject of natural science concerned with the physical processes and physical properties of the Earth and its surrounding space environment, and the use of quantitative methods for their analysis. The term geophysics sometimes refers only to the geological applications: Earth's shape; its gravitational and magnetic fields; its internal structure and composition; its dynamics and their surface expression in plate tectonics, the generation of magmas, volcanism and rock formation. However, modern geophysics organizations use a broader definition that includes the water cycle including snow and ice; fluid dynamics of the oceans and the atmosphere; electricity and magnetism in the ionosphere and magnetosphere and solar-terrestrial relations; and analogous problems associated with the Moon and other planets.Although geophysics was only recognized as a separate discipline in the 19th century, its origins go back to ancient times. The first magnetic compasses were made from lodestones, while more modern magnetic compasses played an important role in the history of navigation. The first seismic instrument was built in 132 BC. Isaac Newton applied his theory of mechanics to the tides and the precession of the equinox; and instruments were developed to measure the Earth's shape, density and gravity field, as well as the components of the water cycle. In the 20th century, geophysical methods were developed for remote exploration of the solid Earth and the ocean, and geophysics played an essential role in the development of the theory of plate tectonics.Geophysics is applied to societal needs, such as mineral resources, mitigation of natural hazards and environmental protection. Geophysical survey data are used to analyze potential petroleum reservoirs and mineral deposits, locate groundwater, find archaeological relics, determine the thickness of glaciers and soils, and assess sites for environmental remediation.
 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									 
									