Sample 5.3.B.2 Complete
... presentation below by drawing a sixth map showing how the continents might look 100 million years from now. Students must consider that the earth’s lithosphere is made up of moving plates and must take into account the directions in which major plates are moving. (5.4.6.D.1) ...
... presentation below by drawing a sixth map showing how the continents might look 100 million years from now. Students must consider that the earth’s lithosphere is made up of moving plates and must take into account the directions in which major plates are moving. (5.4.6.D.1) ...
Earths Layers
... Uneven heating causes material in the mantle to constantly and slowly rise & fall in convection currents. Convection Current: process by which hot fluid rises to the surface, and then sinks again, like soup being heated in a saucepan ...
... Uneven heating causes material in the mantle to constantly and slowly rise & fall in convection currents. Convection Current: process by which hot fluid rises to the surface, and then sinks again, like soup being heated in a saucepan ...
Chapter 5 - Mrs. Wiley`s Environmental Science Site
... Describe igneous rocks and tell how they are formed. Igneous rocks can be fine or coarse-grained. They are formed when magma or lava cools. Describe metamorphic rocks and tell how they are formed. Metamorphic rocks form when parent rocks are heated, squeezed, or exposed to hot liquids. They do not m ...
... Describe igneous rocks and tell how they are formed. Igneous rocks can be fine or coarse-grained. They are formed when magma or lava cools. Describe metamorphic rocks and tell how they are formed. Metamorphic rocks form when parent rocks are heated, squeezed, or exposed to hot liquids. They do not m ...
Earth`s Interior - Poster Project
... Must include a scale drawing of the Earth’s layers including a closer look at the layers near the Earth’s surface (Should be about 5 inches in diameter.) Must include a cutout, which shows the layers up close. ...
... Must include a scale drawing of the Earth’s layers including a closer look at the layers near the Earth’s surface (Should be about 5 inches in diameter.) Must include a cutout, which shows the layers up close. ...
Earth`s Crust
... Plate tectonic – theory that Earth’s crust and part of the upper mantle are broken into sections ...
... Plate tectonic – theory that Earth’s crust and part of the upper mantle are broken into sections ...
EARTH-2
... layers the crust is much thinner. It floats upon the softer, denser mantle. The crust is made up of solid material but this material is not the same everywhere. There is an Oceanic crust and a Continental crust. The first one is about 4-7 miles (6-11 km) thick and mainly consists of heavy rocks, lik ...
... layers the crust is much thinner. It floats upon the softer, denser mantle. The crust is made up of solid material but this material is not the same everywhere. There is an Oceanic crust and a Continental crust. The first one is about 4-7 miles (6-11 km) thick and mainly consists of heavy rocks, lik ...
Lesson 5: Intro to Magnet
... You should know that we human have known about magnets for thousands of years and we have been using them practically, as compasses, for almost as long. However, we did not know that there is a link between magnet and electricity until recently. We've only really learned how magnetism works in the l ...
... You should know that we human have known about magnets for thousands of years and we have been using them practically, as compasses, for almost as long. However, we did not know that there is a link between magnet and electricity until recently. We've only really learned how magnetism works in the l ...
Earth Layers and Continental Drift
... 1. Direct evidence from rock samples (drilled from deep inside Earth) 2. Indirect evidence from seismic waves (produced by earthquakes; speed gives clues to the material) ...
... 1. Direct evidence from rock samples (drilled from deep inside Earth) 2. Indirect evidence from seismic waves (produced by earthquakes; speed gives clues to the material) ...
Origin of the Universe
... The revolution begins • During the 1940s and 1950s technological advances permitted mapping of the ocean floor. Hess was captain of a minesweeper with sonar. Left it on all WWII. • Seafloor spreading hypothesis was proposed by Harry Hess in the early 1960s. http://www.amnh.org/education/resources/rf ...
... The revolution begins • During the 1940s and 1950s technological advances permitted mapping of the ocean floor. Hess was captain of a minesweeper with sonar. Left it on all WWII. • Seafloor spreading hypothesis was proposed by Harry Hess in the early 1960s. http://www.amnh.org/education/resources/rf ...
Vocab-Chapter 7 - Wachter Middle School
... ____________________________ 8. The layer of the Earth between the crust and the core. ____________________________ 9. Literally, the “middle sphere”-the strong, lower part of the mantle between the asthenosphere and the outer core. ____________________________ 10. The process by which new oceanic l ...
... ____________________________ 8. The layer of the Earth between the crust and the core. ____________________________ 9. Literally, the “middle sphere”-the strong, lower part of the mantle between the asthenosphere and the outer core. ____________________________ 10. The process by which new oceanic l ...
Basic Structure of the Earth
... studying seismic (earthquake) waves and volcanic rocks • Deepest well ever drilled was only 12 km deep • The crust is only 1% of earth’s mass • The mantle is about 65% of earth’s mass • The core is about 34% of earth’s mass • Pressure at the center of the earth is about ...
... studying seismic (earthquake) waves and volcanic rocks • Deepest well ever drilled was only 12 km deep • The crust is only 1% of earth’s mass • The mantle is about 65% of earth’s mass • The core is about 34% of earth’s mass • Pressure at the center of the earth is about ...
The Earth - Indiana University Astronomy
... Differentiation occurs in a mixture of heavy and light materials if these materials are liquid for a long enough time The Earth must have been almost entirely liquid in the past ...
... Differentiation occurs in a mixture of heavy and light materials if these materials are liquid for a long enough time The Earth must have been almost entirely liquid in the past ...
Earth Space Science Week8
... transferred through Earth's system. SC.6.E.7.4 (AA) Differentiate and show interactions among the geosphere, hydrosphere, cryosphere, atmosphere, and biosphere. SC.7.E.6.1 Describe the layers of the solid Earth, including the lithosphere, the hot convecting mantle, and the dense metallic liquid and ...
... transferred through Earth's system. SC.6.E.7.4 (AA) Differentiate and show interactions among the geosphere, hydrosphere, cryosphere, atmosphere, and biosphere. SC.7.E.6.1 Describe the layers of the solid Earth, including the lithosphere, the hot convecting mantle, and the dense metallic liquid and ...
MS Word
... everything that is covered in class so this practice test is not all-inclusive of topics to be tested. Check the review sheet (separate link) for a more complete list! Note: there may be formatting gaps in the practice quiz below. Ignore question numbers – and check back for the answer key at a late ...
... everything that is covered in class so this practice test is not all-inclusive of topics to be tested. Check the review sheet (separate link) for a more complete list! Note: there may be formatting gaps in the practice quiz below. Ignore question numbers – and check back for the answer key at a late ...
unit 4 physics index book 1 — electric power
... AREA OF STUDY: ELECTRIC POWER MAGNETIC FIELDS A magnetic field can be thought of as a region in which magnetic forces exist. Such a field exists, for example, around a permanent magnet. Note that the magnetic field lines come out of the north pole of a magnet, and go into a south pole. ...
... AREA OF STUDY: ELECTRIC POWER MAGNETIC FIELDS A magnetic field can be thought of as a region in which magnetic forces exist. Such a field exists, for example, around a permanent magnet. Note that the magnetic field lines come out of the north pole of a magnet, and go into a south pole. ...
Structure of the Earth Crust
... ride atop of the plates and constantly pull apart, collide, and grind against one another at plate boundaries ...
... ride atop of the plates and constantly pull apart, collide, and grind against one another at plate boundaries ...
The Changing Earth 1.3
... You learned earlier that the sea floor is younger near a mid-ocean ridge and older farther away. As scientists continued to study the sea-floor rock, they made a surprising discovery about Earth's magnetic field. To understand Earth's magnetic field, you can compare the planet to a bar magnet, whic ...
... You learned earlier that the sea floor is younger near a mid-ocean ridge and older farther away. As scientists continued to study the sea-floor rock, they made a surprising discovery about Earth's magnetic field. To understand Earth's magnetic field, you can compare the planet to a bar magnet, whic ...
Uniformitarianism and earth layers
... were “mineral freaks”, and effects of the flood were seen everywhere. Uniformitarianism’s main idea was that of gradual forces gave rise to all order we see today. Mountains uplifted by gradually occurring natural forces, leading to the term gradualism. ...
... were “mineral freaks”, and effects of the flood were seen everywhere. Uniformitarianism’s main idea was that of gradual forces gave rise to all order we see today. Mountains uplifted by gradually occurring natural forces, leading to the term gradualism. ...
Key Ideas
... combining with other elements to form compounds, and is also being used by respiratory life. Despite this, the amount of oxygen in our atmosphere is not decreasing because it is being replenished by A. B. C. D. ...
... combining with other elements to form compounds, and is also being used by respiratory life. Despite this, the amount of oxygen in our atmosphere is not decreasing because it is being replenished by A. B. C. D. ...
Plate Tectonics Crossword
... _____________ boundaries occur where plates grind past each other without destroying the lithosphere. ...
... _____________ boundaries occur where plates grind past each other without destroying the lithosphere. ...
Geosphere!
... The Earth is described as a system since it also has connecting ‘parts’ that make up its ‘whole.’ ...
... The Earth is described as a system since it also has connecting ‘parts’ that make up its ‘whole.’ ...
History of geomagnetism
The history of geomagnetism is concerned with the history of the study of Earth's magnetic field. It encompasses the history of navigation using compasses, studies of the prehistoric magnetic field (archeomagnetism and paleomagnetism), and applications to plate tectonics.Magnetism has been known since prehistory, but knowledge of the Earth's field developed slowly. The horizontal direction of the Earth's field was first measured in the fourth century BC but the vertical direction was not measured until 1544 AD and the intensity was first measured in 1791. At first, compasses were thought to point towards locations in the heavens, then towards magnetic mountains. A modern experimental approach to understanding the Earth's field began with de Magnete, a book published by William Gilbert in 1600. His experiments with a magnetic model of the Earth convinced him that the Earth itself is a large magnet.