mantle - Uplift Mighty Prep
... 1. How do we know what the inside of the Earth is made of? 2. What are the three basic layers of the Earth. 3. What layer do we live on? 4. What part makes up the bulk of the Earth’s mass? ...
... 1. How do we know what the inside of the Earth is made of? 2. What are the three basic layers of the Earth. 3. What layer do we live on? 4. What part makes up the bulk of the Earth’s mass? ...
Quiz 5
... B) 2 minutes, 15 seconds C) 3 minutes D) 4 minutes E) 5 minutes, 30 seconds 7. According to the figure above, what is the approximate S-P travel time? A) 1 minute, 45 seconds B) 2 minutes, 15 seconds C) 3 minutes, 15 seconds D) 0 minutes, 45 seconds E) cannot be determined ...
... B) 2 minutes, 15 seconds C) 3 minutes D) 4 minutes E) 5 minutes, 30 seconds 7. According to the figure above, what is the approximate S-P travel time? A) 1 minute, 45 seconds B) 2 minutes, 15 seconds C) 3 minutes, 15 seconds D) 0 minutes, 45 seconds E) cannot be determined ...
11 Test Review - The Planet Earth
... speed of onset – the rapidness of the storm, spatial dispersion – the most likely area to be affected, temporal spacing – how it occurs in time 3. Lithosphere – earth’s crust (soil, rocks, and minerals) Hydrosphere – earth’s water Atmosphere – the gases in the air Biosphere – all living things (plan ...
... speed of onset – the rapidness of the storm, spatial dispersion – the most likely area to be affected, temporal spacing – how it occurs in time 3. Lithosphere – earth’s crust (soil, rocks, and minerals) Hydrosphere – earth’s water Atmosphere – the gases in the air Biosphere – all living things (plan ...
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 ...
Earth
... the center—your oven only goes to about 600 degrees F). 3. It’s so hot that rock melts. Melted rock is called MAGMA. 4. 1,400 MILES THICK! ...
... the center—your oven only goes to about 600 degrees F). 3. It’s so hot that rock melts. Melted rock is called MAGMA. 4. 1,400 MILES THICK! ...
Chapter-2_PracticeTest
... a) The amount of gas dissolved in the magma increases. b) The pressure on the magma increases. c) The amount of gas dissolved in the magma decreases. d) The amount of water vapor in the air decreases. 13. Walking to school one day you feel the ground move in an up-and-down rolling motion. You ar ...
... a) The amount of gas dissolved in the magma increases. b) The pressure on the magma increases. c) The amount of gas dissolved in the magma decreases. d) The amount of water vapor in the air decreases. 13. Walking to school one day you feel the ground move in an up-and-down rolling motion. You ar ...
Factors Affecting Density
... – At great depths below Earth’s surface there is extremely high pressure from the overlying rocks. – Minerals are compressed ...
... – At great depths below Earth’s surface there is extremely high pressure from the overlying rocks. – Minerals are compressed ...
Name: June Proficiency Exam Study Guide 7th Grade Science
... List and describe the layers of the geosphere. Crust: thin outer layer, solid Mantle: thick, rocky middle layer-convection currents Outer Core: liquid iron and nickel Inner Core: solid, extreme heat and pressure ...
... List and describe the layers of the geosphere. Crust: thin outer layer, solid Mantle: thick, rocky middle layer-convection currents Outer Core: liquid iron and nickel Inner Core: solid, extreme heat and pressure ...
Introduction to Earthquakes EASA
... bulk of the lower mantle is termed the mesosphere and is stronger than the asthenosphere However, it does behave like a fluid over long time scales (convects) It is not clear if the whole mantle convects as one layer or two ...
... bulk of the lower mantle is termed the mesosphere and is stronger than the asthenosphere However, it does behave like a fluid over long time scales (convects) It is not clear if the whole mantle convects as one layer or two ...
Chapter 8 Test Review Notes
... boundary, and the rocks are old. The rocks are cold and dense. The greater density causes the seafloor to be deeper. As it plunges into a deep-sea trench, the seafloor reaches its greatest depths of anywhere in the ocean basin. ...
... boundary, and the rocks are old. The rocks are cold and dense. The greater density causes the seafloor to be deeper. As it plunges into a deep-sea trench, the seafloor reaches its greatest depths of anywhere in the ocean basin. ...
Sample High School Earth Science Unit Plan
... often recrystallized into new rock. Eventually, those new rocks may be brought to the surface by the forces that drive plate motions, and the rock cycle continues. EARTH'S HISTORY o The earth processes we see today, including erosion, movement of lithospheric plates, and changes in atmospheric compo ...
... often recrystallized into new rock. Eventually, those new rocks may be brought to the surface by the forces that drive plate motions, and the rock cycle continues. EARTH'S HISTORY o The earth processes we see today, including erosion, movement of lithospheric plates, and changes in atmospheric compo ...
Earthquakes
... An earthquake is ground movements that occur when blocks of rock in Earth move suddenly and release energy. Earthquakes occur along fault lines. ◦ Faults are breaks in Earth’s crust where blocks of rock slide past each other. ...
... An earthquake is ground movements that occur when blocks of rock in Earth move suddenly and release energy. Earthquakes occur along fault lines. ◦ Faults are breaks in Earth’s crust where blocks of rock slide past each other. ...
Science | Unit: Earth Science and Systems | Lesson 3: Spheres as
... __________ sphere on the planet. It is not a perfect sphere in that it is ________ at the equator (6,378 km) than at the poles (6,357 km). ...
... __________ sphere on the planet. It is not a perfect sphere in that it is ________ at the equator (6,378 km) than at the poles (6,357 km). ...
CH 5 Earth`s Phys Enviro
... Plate Tectonics- study of the processes by which the lithospheric plates move over the asthenosphere Plate Boundary- where 2 plates meet ...
... Plate Tectonics- study of the processes by which the lithospheric plates move over the asthenosphere Plate Boundary- where 2 plates meet ...
Ch._8__10_notes_plate_tectonics_and_earths_surface.pptx
... • Hot liquid weigh less and float above cooler liquids • When it rises to the top, it cools, and more hot liquid can rise above • This process is called convection • The mantle is not a liquid, but its rocks are so hot they ...
... • Hot liquid weigh less and float above cooler liquids • When it rises to the top, it cools, and more hot liquid can rise above • This process is called convection • The mantle is not a liquid, but its rocks are so hot they ...
Earth`s Interior (What`s down there below us?)
... From 100 to 200 km (60-120 miles) below the surface, the temperatures are above the melting point of the rock - even at the very high pressure at this ...
... From 100 to 200 km (60-120 miles) below the surface, the temperatures are above the melting point of the rock - even at the very high pressure at this ...
NASC 1100
... Most major earthquakes and volcanic eruption occur along plate boundaries. Plate tectonics carries rock from the mantle, transports it across the seafloor, and returns it back. New crust is spread through mid-ocean ridges. The old crust is returned back through trenches (subduction). ...
... Most major earthquakes and volcanic eruption occur along plate boundaries. Plate tectonics carries rock from the mantle, transports it across the seafloor, and returns it back. New crust is spread through mid-ocean ridges. The old crust is returned back through trenches (subduction). ...
Document
... A scale that rates earthquakes according to their intensity and how much damage they cause at a particular place ...
... A scale that rates earthquakes according to their intensity and how much damage they cause at a particular place ...
The Earth How the crust moves…
... • Identify and describe earth’s major geological processes. • Describe earth’s major geological hazards. ...
... • Identify and describe earth’s major geological processes. • Describe earth’s major geological hazards. ...
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.