
Lesson 3 For students of Geography, 2 course. Subject: THE EARTH
... The mid-ocean ridges can also be regarded as belts of frequent earthquakes. The shield areas of the continents, on the other hand, are much less affected. Earthquakes originate within the crust as well as the upper mantle, but most begin within 3 miles (5 km) of the surface. The point of origin is t ...
... The mid-ocean ridges can also be regarded as belts of frequent earthquakes. The shield areas of the continents, on the other hand, are much less affected. Earthquakes originate within the crust as well as the upper mantle, but most begin within 3 miles (5 km) of the surface. The point of origin is t ...
Earth Science Unit Review
... 32. Molecules in a solid are closer together, making contact more likely, which transfers thermal energy. 33. At sea level, there is a greater amount of atmosphere over the surface, but at high altitudes there is less atmosphere. 34. About 34ºC cooler 35. A biogeoclimatic zone is a region with a cer ...
... 32. Molecules in a solid are closer together, making contact more likely, which transfers thermal energy. 33. At sea level, there is a greater amount of atmosphere over the surface, but at high altitudes there is less atmosphere. 34. About 34ºC cooler 35. A biogeoclimatic zone is a region with a cer ...
Thinking Point - Dynamic Earth
... Working in groups pupils need to decide on a research question, come up with some predictions of what might happen and then design and carry out an experiment to test these. A great way to display the conclusions of their investigations is for each group to create a poster showing their scientific j ...
... Working in groups pupils need to decide on a research question, come up with some predictions of what might happen and then design and carry out an experiment to test these. A great way to display the conclusions of their investigations is for each group to create a poster showing their scientific j ...
The Earth - Humble ISD
... _______________ – soft layer of molten rock (magma) Crust – thin layer of rock on earth’s surface Continental Drift – __________________ first presented the theory. He claimed that in Earth’s early existence there was only one body of land, ______________. That supercontinent then slowly split and s ...
... _______________ – soft layer of molten rock (magma) Crust – thin layer of rock on earth’s surface Continental Drift – __________________ first presented the theory. He claimed that in Earth’s early existence there was only one body of land, ______________. That supercontinent then slowly split and s ...
Earth Science - WordPress.com
... shelf, continental slope, core, crust, deep-ocean basin, deep-ocean trench, Earth science, Earth system science, environment, geologic time scale, geology, geosphere, hydrosphere, hypothesis, inner core, interface, lithosphere, lithospheric plate, lower mantle, mantle, meteorology, model, nebular hy ...
... shelf, continental slope, core, crust, deep-ocean basin, deep-ocean trench, Earth science, Earth system science, environment, geologic time scale, geology, geosphere, hydrosphere, hypothesis, inner core, interface, lithosphere, lithospheric plate, lower mantle, mantle, meteorology, model, nebular hy ...
The Changing Face of the Planet new ppt
... spreading and a means of determining how the continents have moved When magma cools, grains of iron line up with the magnetic pole (like little compasses) Polarity reversals occur in parallel bands on opposite sides of the mid-ocean ridges During the past 4 million years, the magnetic poles have rev ...
... spreading and a means of determining how the continents have moved When magma cools, grains of iron line up with the magnetic pole (like little compasses) Polarity reversals occur in parallel bands on opposite sides of the mid-ocean ridges During the past 4 million years, the magnetic poles have rev ...
section - SCHOOLinSITES
... • A ________ is a break in the Earth’s crust along which Blocks of the crust __________ relative to each other ...
... • A ________ is a break in the Earth’s crust along which Blocks of the crust __________ relative to each other ...
9.2 – Sea Floor Spreading
... poles moveup to 50 miles (80 km) per day. (average of 25 miles per year) •In the last 150 years, the pole has wandered a total of about 685 miles •The last time the poles switched was 780,000 years ago, and it's happened about 400 times in 330 million years ...
... poles moveup to 50 miles (80 km) per day. (average of 25 miles per year) •In the last 150 years, the pole has wandered a total of about 685 miles •The last time the poles switched was 780,000 years ago, and it's happened about 400 times in 330 million years ...
Earthquakes, Mountains, and Volcanoes Review Puzzle What did
... 8. An opening in Earth’s crust through which magma, rock fragments, and gases erupt. __ __ __ __ __ __ __ 9. The most dangerous part of a volcanic eruption, due to its speed and temperature. Consists of a cloud of superhot dense gases and rock fragments. __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ ...
... 8. An opening in Earth’s crust through which magma, rock fragments, and gases erupt. __ __ __ __ __ __ __ 9. The most dangerous part of a volcanic eruption, due to its speed and temperature. Consists of a cloud of superhot dense gases and rock fragments. __ __ __ __ __ __ __ __ __ __ __ __ __ __ __ ...
forces of change
... The thickest layer. This layer is made up of hot, dense rock – silicon, aluminum, iron, magnesium, and oxygen. This layer rises, cools, sinks, warms up, rises, etc. The rocky shell that covers the earth’s surface. The shell is broken up into plates that move apart or ground together to push up mount ...
... The thickest layer. This layer is made up of hot, dense rock – silicon, aluminum, iron, magnesium, and oxygen. This layer rises, cools, sinks, warms up, rises, etc. The rocky shell that covers the earth’s surface. The shell is broken up into plates that move apart or ground together to push up mount ...
OUTDOOR SCIENCE SCHOOL VOC (#1 – Test)
... causes the rigid area of the crust to crack and form the lithospheric plates (b) asthenosphere – liquid, tar-like layer of the upper mantle below the lithosphere creating a convection current movement, which causes the plates to move (c) mesosphere – lower mantle, almost solid-like above the core (d ...
... causes the rigid area of the crust to crack and form the lithospheric plates (b) asthenosphere – liquid, tar-like layer of the upper mantle below the lithosphere creating a convection current movement, which causes the plates to move (c) mesosphere – lower mantle, almost solid-like above the core (d ...
Plate Tectonics – A Geologic Revolution
... • Magnetic inclination can be related to magnetic latitude. • If one can determine the magnetic inclination at some time in the past this information can be used to determine paleolatitude. • Magnetite becomes magnetic at 580oC (the Curie temperature). ...
... • Magnetic inclination can be related to magnetic latitude. • If one can determine the magnetic inclination at some time in the past this information can be used to determine paleolatitude. • Magnetite becomes magnetic at 580oC (the Curie temperature). ...
EQTip01 :: Final
... like the convective flow of water when heated in a beaker (Figure 2). The energy for the above circulations is derived from the heat produced from the incessant decay of radioactive elements in the rocks throughout the Earth’s interior. These convection currents result in a circulation of the earth’ ...
... like the convective flow of water when heated in a beaker (Figure 2). The energy for the above circulations is derived from the heat produced from the incessant decay of radioactive elements in the rocks throughout the Earth’s interior. These convection currents result in a circulation of the earth’ ...
Guided Reading on Sections 23.3 and 23.4
... 6. His hypothesis was that _____________ had fractured into a number of pieces, and that South America and ______________ had indeed once been joined together as part of a larger land mass. 7. He proposed that the geological boundary of each continent lay not at its ________________ but at the edge ...
... 6. His hypothesis was that _____________ had fractured into a number of pieces, and that South America and ______________ had indeed once been joined together as part of a larger land mass. 7. He proposed that the geological boundary of each continent lay not at its ________________ but at the edge ...
Answers to the study guide
... 9. How does the core create a magnetic field around the Earth? a. The solid inner core spins inside the liquid outer core creating a strong magnetic field that surrounds the Earth far out into space 10. Who proposed the theory of continental drift? a. Alfred Wegener 11. What is the theory of contine ...
... 9. How does the core create a magnetic field around the Earth? a. The solid inner core spins inside the liquid outer core creating a strong magnetic field that surrounds the Earth far out into space 10. Who proposed the theory of continental drift? a. Alfred Wegener 11. What is the theory of contine ...
Plate_Tectonics_Day_1
... Geologists discovered the Earth has three layersthe crust, the mantle, and the core. The oceanic crust beneath the ocean consists mostly of dense rock. Continental crust also consists of dense rock. The crust makes up the lithosphere. The asthenosphere is a soft layer that can bend like plasti ...
... Geologists discovered the Earth has three layersthe crust, the mantle, and the core. The oceanic crust beneath the ocean consists mostly of dense rock. Continental crust also consists of dense rock. The crust makes up the lithosphere. The asthenosphere is a soft layer that can bend like plasti ...
Layers of the Earth Notes - Howard Elementary School
... Earth’s Layers by Composition • Crust – Outermost layer – Thinnest layer – Composed mostly of oxygen, silicon, and aluminum – Two types • Oceanic (found under oceans; more dense) – Twice as much iron, calcium, and magnesium which are more dense minerals ...
... Earth’s Layers by Composition • Crust – Outermost layer – Thinnest layer – Composed mostly of oxygen, silicon, and aluminum – Two types • Oceanic (found under oceans; more dense) – Twice as much iron, calcium, and magnesium which are more dense minerals ...
Components of the Spheres
... GEOSPHERE Changes in the Geosphere are based on physical evidence such as rocks, fossils, and land forms Core- makes up 16% of the volume of the earth and 31% of mass. It is divided into 2 regions : Solid inner core and liquid outer core. Mantle- largest layer in the earth 82% of volume and 68% ...
... GEOSPHERE Changes in the Geosphere are based on physical evidence such as rocks, fossils, and land forms Core- makes up 16% of the volume of the earth and 31% of mass. It is divided into 2 regions : Solid inner core and liquid outer core. Mantle- largest layer in the earth 82% of volume and 68% ...
Geology Unit Study Guide
... 2. Who proposed the theory of continental drift? 3. Why was this theory not accepted? 4. What caused the tectonic plates to move? 5. What evidence did Wegener have that showed that Pangaea once existed? 6. How has technology aided in the support of continental drift? 7. What is the theory of plate t ...
... 2. Who proposed the theory of continental drift? 3. Why was this theory not accepted? 4. What caused the tectonic plates to move? 5. What evidence did Wegener have that showed that Pangaea once existed? 6. How has technology aided in the support of continental drift? 7. What is the theory of plate t ...
ppt
... As the Earth cooled the heavier, denser materials sank to the center and the lighter materials rose to the top. Because of this, the crust is made of the lightest materials (rock- basalts and granites) and the core consists of heavy metals (nickel and iron). ...
... As the Earth cooled the heavier, denser materials sank to the center and the lighter materials rose to the top. Because of this, the crust is made of the lightest materials (rock- basalts and granites) and the core consists of heavy metals (nickel and iron). ...
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.