Plate Tectonics
... tectonics is responsible for the formation of the most spectacular natural features on Earth, such as mountain belts, volcanoes, rift valleys, hot springs and mid-ocean ridges and also for the dramatic impacts of earthquakes. ...
... tectonics is responsible for the formation of the most spectacular natural features on Earth, such as mountain belts, volcanoes, rift valleys, hot springs and mid-ocean ridges and also for the dramatic impacts of earthquakes. ...
The Outer Core - Geography1000
... • Beneath continents the thickness averages more than 5 times that much • The base of the Crust is a change in mineral composition, called • Mohorovicic discontinuity (or Moho) ...
... • Beneath continents the thickness averages more than 5 times that much • The base of the Crust is a change in mineral composition, called • Mohorovicic discontinuity (or Moho) ...
KEY for Tectonics Study Guide #1
... Use this “key” to check the answers on your study guide. Remember, answers do not need to match word-for-word, but the ideas should be the same. Your answer should have the same level of detail that the key shows, too. Goal 1: Describe the Shrinking Earth Theory. Explain how new ideas and technology ...
... Use this “key” to check the answers on your study guide. Remember, answers do not need to match word-for-word, but the ideas should be the same. Your answer should have the same level of detail that the key shows, too. Goal 1: Describe the Shrinking Earth Theory. Explain how new ideas and technology ...
volcanoes - Etiwanda E
... Tectonic Plates Tectonic plates are made of either oceanic or continental crust and the very top part of the mantle, a layer of rock inside the earth. ...
... Tectonic Plates Tectonic plates are made of either oceanic or continental crust and the very top part of the mantle, a layer of rock inside the earth. ...
Name - Quia
... Name ___________________________ Inside Earth – CRT # 1 Review Chapter 1 Section 1 – Earth’s Interior The Science of Geology (page 17-18) Who are the scientists who study the forces that make and shape planet Earth? ...
... Name ___________________________ Inside Earth – CRT # 1 Review Chapter 1 Section 1 – Earth’s Interior The Science of Geology (page 17-18) Who are the scientists who study the forces that make and shape planet Earth? ...
1-Unit4Part1EarthsInterior
... • Outermost layer • Rigid and thin compared to the other two • Ranges from 0 to 100 km thickness – Oceanic Crust • Beneath the ocean – about 5 km thickness ...
... • Outermost layer • Rigid and thin compared to the other two • Ranges from 0 to 100 km thickness – Oceanic Crust • Beneath the ocean – about 5 km thickness ...
No Slide Title
... Collide with other particles and sets them in motion. Not an efficient way to move heat in the Earth. Rock is a very POOR conductor of heat. ...
... Collide with other particles and sets them in motion. Not an efficient way to move heat in the Earth. Rock is a very POOR conductor of heat. ...
early-earth1 - WordPress.com
... • Our galaxy was formed - _________ billion years ago • Our Universe was formed - ________ billion years ago • Life on earth began _______ billion years ago • Human life began _________ years ago – the last _____ _________________ of the cosmic calendar. ...
... • Our galaxy was formed - _________ billion years ago • Our Universe was formed - ________ billion years ago • Life on earth began _______ billion years ago • Human life began _________ years ago – the last _____ _________________ of the cosmic calendar. ...
Geology Study Guide
... 1. Earth’s rigid outer layers make up the inner core outer core lithosphere mantle. 2. To learn the structure of earth’s interior geologists study the magnetic field the luster of minerals sedimentary rocks seismic waves. 3. An example of an igneous rock is gneiss basalt marble limestone. 4. The con ...
... 1. Earth’s rigid outer layers make up the inner core outer core lithosphere mantle. 2. To learn the structure of earth’s interior geologists study the magnetic field the luster of minerals sedimentary rocks seismic waves. 3. An example of an igneous rock is gneiss basalt marble limestone. 4. The con ...
Section 1
... • Temperature inside Earth increases as depth increases. • Beneath earth surface rock is cool, but 20 meters down the rock starts to get warmer. • For every 40 meters down , the temperature increases 1 Celsius degree. • The high temperatures inside Earth are the results of great rock pressure, energ ...
... • Temperature inside Earth increases as depth increases. • Beneath earth surface rock is cool, but 20 meters down the rock starts to get warmer. • For every 40 meters down , the temperature increases 1 Celsius degree. • The high temperatures inside Earth are the results of great rock pressure, energ ...
Due: Tuesday February 1
... 5. What happens to pressure and temperature as you down into the earth? ...
... 5. What happens to pressure and temperature as you down into the earth? ...
the earth`s spheres
... Transform boundaries -- where crust is neither produced nor destroyed as the plates slide horizontally past each other. ...
... Transform boundaries -- where crust is neither produced nor destroyed as the plates slide horizontally past each other. ...
Plate Tectonics Picture Study Guide File
... Why do we not notice Continental Drift: They only drift one to four centimeters per year so we will not observe through our life. 200 Million Years Ago 135 Million Years Ago 65 Million Years Ago ...
... Why do we not notice Continental Drift: They only drift one to four centimeters per year so we will not observe through our life. 200 Million Years Ago 135 Million Years Ago 65 Million Years Ago ...
Unit 3 Review Questions
... 14. A break or crack in Earth’s crust is called a ________________. 15. What type of landform results from convergent plate boundary movement? _________ 16. What type of plate boundary movement would be associated with compression? ______________________ ...
... 14. A break or crack in Earth’s crust is called a ________________. 15. What type of landform results from convergent plate boundary movement? _________ 16. What type of plate boundary movement would be associated with compression? ______________________ ...
Which type of heat transfer is taking place?
... Earth that we live on, the outermost layer called the crust. It is made up of loose material, like rocks, soil, and seabed. The crust is about five miles deep beneath the oceans and about twenty-five miles thick below the continents. Beyond the crust is the mantle. The mantle extends approximately 1 ...
... Earth that we live on, the outermost layer called the crust. It is made up of loose material, like rocks, soil, and seabed. The crust is about five miles deep beneath the oceans and about twenty-five miles thick below the continents. Beyond the crust is the mantle. The mantle extends approximately 1 ...
Science Test Study Guide
... The solar system is made up of the Sun and all the objects that orbit it. Our Sun is a star. The Moon is a satellite of the Earth. There are eight planets that circle the sun: Mercury, Venus, Earth, Mars, Jupiter, Saturn, Uranus, and Neptune. All the planets orbit the Sun. The inner planets are the ...
... The solar system is made up of the Sun and all the objects that orbit it. Our Sun is a star. The Moon is a satellite of the Earth. There are eight planets that circle the sun: Mercury, Venus, Earth, Mars, Jupiter, Saturn, Uranus, and Neptune. All the planets orbit the Sun. The inner planets are the ...
Earth Science Vocabulary Chapter 9: Plate Tectonics Section 9.1
... Paleomagnetism- the study of changes in Earth’s magnetic field, as shown by patterns of magnetism in rocks that have formed over time Normal Polarity- a magnetic field that is the same as that which exists at present Reverse Polarity- a magnetic field opposite to that which exist at present Hot Spot ...
... Paleomagnetism- the study of changes in Earth’s magnetic field, as shown by patterns of magnetism in rocks that have formed over time Normal Polarity- a magnetic field that is the same as that which exists at present Reverse Polarity- a magnetic field opposite to that which exist at present Hot Spot ...
Constructive and Destructive Landforms
... Running water-rivers form canyons Groundwater-underground water forms caves/caverns Glaciers-rocks are carried under a glacier. Wind-rock particles are blown Ocean currents-sand is moved along a beach by waves. ...
... Running water-rivers form canyons Groundwater-underground water forms caves/caverns Glaciers-rocks are carried under a glacier. Wind-rock particles are blown Ocean currents-sand is moved along a beach by waves. ...
Inside the Earth
... – The center of the Earth’s core is hotter than the surface of the sun. The temperature of Earth’s inner core reaches 6000 °C whereas the surface of the sun is roughly 5500 °C. • The sun’s core, however, is 15,000,000 °C ...
... – The center of the Earth’s core is hotter than the surface of the sun. The temperature of Earth’s inner core reaches 6000 °C whereas the surface of the sun is roughly 5500 °C. • The sun’s core, however, is 15,000,000 °C ...
Ch. 4 Plate Tectonics This is a satellite image of the San Francisco
... core force the solid inner core to spin at a slightly faster rate than the rest of the planet. These currents in the outer core also create Earth's magnetic field, which causes the planet to act like a giant bar magnet. ...
... core force the solid inner core to spin at a slightly faster rate than the rest of the planet. These currents in the outer core also create Earth's magnetic field, which causes the planet to act like a giant bar magnet. ...
DRAFT Expectation: Interactions of Earth`s Systems
... the system achieves a new state of equilibrium with very different conditions or; o it may fail to achieve any type of equilibrium. ...
... the system achieves a new state of equilibrium with very different conditions or; o it may fail to achieve any type of equilibrium. ...
The science of Geology
... Parts of the Earth system are linked Characterized by processes that ...
... Parts of the Earth system are linked Characterized by processes that ...
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.