Lesson 3
... The focus is the place where the earthquake began. The point on the surface directly above the focus is the epicenter. 3. With regard to the model showing the blocks moving up and down, emphasize that this movement shows a waterfall forming and falling rocks and trees. Have students discuss how the ...
... The focus is the place where the earthquake began. The point on the surface directly above the focus is the epicenter. 3. With regard to the model showing the blocks moving up and down, emphasize that this movement shows a waterfall forming and falling rocks and trees. Have students discuss how the ...
Crust - www .alexandria .k12 .mn .us
... different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and has the ability to flow. The outer core and inner core are even hotter with pressures so great you would be squeezed into a ball smaller than a marble if you wer ...
... different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and has the ability to flow. The outer core and inner core are even hotter with pressures so great you would be squeezed into a ball smaller than a marble if you wer ...
The Layers of the Earth
... different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and has the ability to flow. The outer core and inner core are even hotter with pressures so great you would be squeezed into a ball smaller than a marble if you wer ...
... different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and has the ability to flow. The outer core and inner core are even hotter with pressures so great you would be squeezed into a ball smaller than a marble if you wer ...
walpolebms.ss5.sharpschool.com
... Show what happens to temperature as you move closer to the earth’s core. Show what happens to density as you move towards the earth’s core. ...
... Show what happens to temperature as you move closer to the earth’s core. Show what happens to density as you move towards the earth’s core. ...
Earth’s Interior PowerPoint - Marcia's Science Teaching
... different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and has the ability to flow. The outer core and inner core are even hotter with pressures so great you would be squeezed into a ball smaller than a marble if you wer ...
... different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and has the ability to flow. The outer core and inner core are even hotter with pressures so great you would be squeezed into a ball smaller than a marble if you wer ...
1 - TeacherWeb
... 30. Which of the following statements is the best summary of the rock cycle? a. Rock deep below ground rise to the surface, are moved back underground, then rise to the surface again. b. Igneous rock and sedimentary rock change to metamorphic rock. c. The rock cycle has a single pathway from one ty ...
... 30. Which of the following statements is the best summary of the rock cycle? a. Rock deep below ground rise to the surface, are moved back underground, then rise to the surface again. b. Igneous rock and sedimentary rock change to metamorphic rock. c. The rock cycle has a single pathway from one ty ...
8.1 Earth has several layers
... • Tectonic plates rest on the asthenosphere (layer of soft, hot rock) • Convection currents within Earth helps to move the plates • convection—the transfer of heat by the movement of a material • convection current—a motion that transfers heat energy to a material • Moves very slowly, a few centimet ...
... • Tectonic plates rest on the asthenosphere (layer of soft, hot rock) • Convection currents within Earth helps to move the plates • convection—the transfer of heat by the movement of a material • convection current—a motion that transfers heat energy to a material • Moves very slowly, a few centimet ...
Seismic Waves Webquest - Dublin City Schools Dashboard
... 1. Go to http://aspire.cosmic-‐ray.org/Labs/SeismicWaves/ you can also access this website in the resources section of this lesson. 2. Spend 1-‐2 minutes playing with the Mighty Wave Make ...
... 1. Go to http://aspire.cosmic-‐ray.org/Labs/SeismicWaves/ you can also access this website in the resources section of this lesson. 2. Spend 1-‐2 minutes playing with the Mighty Wave Make ...
Earth`s Interior
... QuickTime™ and a Sorenson Video 3 decompressor are needed to see this picture. ...
... QuickTime™ and a Sorenson Video 3 decompressor are needed to see this picture. ...
Crust - MentorMob
... different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and has the ability to flow. The outer core and inner core are even hotter with pressures so great you would be squeezed into a ball smaller than a marble if you wer ...
... different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and has the ability to flow. The outer core and inner core are even hotter with pressures so great you would be squeezed into a ball smaller than a marble if you wer ...
Earth,Notes,RevQs,Ch1
... 3. They believed Earth to be a very young planet. Accepting such a brief geologic history forced them to explain Earth's evolution in terms of many, rapid, short-term, catastrophic events. Stupendous natural features like the Grand Canyon, mountain ranges, the polar ice caps, the oceans, etc., had t ...
... 3. They believed Earth to be a very young planet. Accepting such a brief geologic history forced them to explain Earth's evolution in terms of many, rapid, short-term, catastrophic events. Stupendous natural features like the Grand Canyon, mountain ranges, the polar ice caps, the oceans, etc., had t ...
Name - Cedar Hill ISD
... 15. The oceanic plate is SUBDUCTED below the continental plate in a convergent boundary because the oceanic plate is MORE dense then the continental plate. When this happens, the oceanic plate returns to the MANTLE. 16. Why does subduction not occur when two continental plates converge? THEY ARE THE ...
... 15. The oceanic plate is SUBDUCTED below the continental plate in a convergent boundary because the oceanic plate is MORE dense then the continental plate. When this happens, the oceanic plate returns to the MANTLE. 16. Why does subduction not occur when two continental plates converge? THEY ARE THE ...
UNIT 5 PLANET EARTH
... Carbonaceous film- a type of fossil found in sedimentary rock when organic materials are compressed Original remains- fossils Trace fossils- evidence of animal activity TOPIC 9 GEOGRAPHIC TIME Principle of superposition- geological theory older rock will be layered on bottom Strata- sedimentary laye ...
... Carbonaceous film- a type of fossil found in sedimentary rock when organic materials are compressed Original remains- fossils Trace fossils- evidence of animal activity TOPIC 9 GEOGRAPHIC TIME Principle of superposition- geological theory older rock will be layered on bottom Strata- sedimentary laye ...
- IMSA Digital Commons
... The Earth’s magnetic field is produced because the Earth’s core has certain properties. The core is … • Electrically conductive (it is made of metal) ...
... The Earth’s magnetic field is produced because the Earth’s core has certain properties. The core is … • Electrically conductive (it is made of metal) ...
Plate Tectonics Study Guide (Chapter 13 Lesson 1) Challenge Date
... 7. Compare oceanic and continental crust. Which is thicker? Which is denser? 8. Describe the different types of plate boundaries in terms of how plates move and features that form (e.g. volcanoes, trenches, mid-ocean ridges, rift valleys, earthquakes, mountains). Be able to recognize diagrams of eac ...
... 7. Compare oceanic and continental crust. Which is thicker? Which is denser? 8. Describe the different types of plate boundaries in terms of how plates move and features that form (e.g. volcanoes, trenches, mid-ocean ridges, rift valleys, earthquakes, mountains). Be able to recognize diagrams of eac ...
Earth`sInterior
... • Like a bar magnet, the Earth has two magnetic poles. The lines of force of the Earth’s magnetic field extend between the North Magnetic Pole and the South Magnetic Pole. • The source may be the liquid iron in the Earth’s outer core. Because iron is a good conductor, scientists hypothesize that mot ...
... • Like a bar magnet, the Earth has two magnetic poles. The lines of force of the Earth’s magnetic field extend between the North Magnetic Pole and the South Magnetic Pole. • The source may be the liquid iron in the Earth’s outer core. Because iron is a good conductor, scientists hypothesize that mot ...
Unit 3 Geology - Manatee School For the Arts / Homepage
... Geology of the Ocean, Water, Waves, and Tides MRS. STAHL MARINE BIOLOGY ...
... Geology of the Ocean, Water, Waves, and Tides MRS. STAHL MARINE BIOLOGY ...
Chapter2StructureofAtmosphere
... Meteorology – the study of the atmosphere and the processes that cause weather Climate – weather conditions at some place averaged over a specific time period Climatology – the study of the climate ...
... Meteorology – the study of the atmosphere and the processes that cause weather Climate – weather conditions at some place averaged over a specific time period Climatology – the study of the climate ...
The Dynamic Earth
... asthenosphere is the layer beneath the lithosphere. The asthenosphere is a plastic, solid layer of the mantle made of rock that flows very slowly and allows tectonic plates to move on top of it. Beneath the asthenosphere is the mesosphere, the lower part of the mantle. The Earth’s outer core is a de ...
... asthenosphere is the layer beneath the lithosphere. The asthenosphere is a plastic, solid layer of the mantle made of rock that flows very slowly and allows tectonic plates to move on top of it. Beneath the asthenosphere is the mesosphere, the lower part of the mantle. The Earth’s outer core is a de ...
Inside the Earth
... Calculate the Speed of an object traveling 120 miles in 3 hours. Next, calculate the time it would take the object to get 240 miles if it traveled at that same speed. Show your work!!!! ...
... Calculate the Speed of an object traveling 120 miles in 3 hours. Next, calculate the time it would take the object to get 240 miles if it traveled at that same speed. Show your work!!!! ...
Earth`s Layers Lesson Plan - elementaryscienceteachers
... the Earth's layers and explain what makes up the layers. Ask the students what it would be like to actually see the different layers. (The teacher may choose to use a peach to demonstrate the layers of the Earth.) Engage the students by telling them that they will be getting a chance to eat the diff ...
... the Earth's layers and explain what makes up the layers. Ask the students what it would be like to actually see the different layers. (The teacher may choose to use a peach to demonstrate the layers of the Earth.) Engage the students by telling them that they will be getting a chance to eat the diff ...
LAYERS OF THE EARTH
... of the mantle, made up of solid rock. Includes the Earth’s plates. Asthenosphere- includes the rest of the Mantle that is made up of magma which is solid and liquid rock. Where the mantle’s circulation takes place. ...
... of the mantle, made up of solid rock. Includes the Earth’s plates. Asthenosphere- includes the rest of the Mantle that is made up of magma which is solid and liquid rock. Where the mantle’s circulation takes place. ...
Nature
Nature, in the broadest sense, is the natural, physical, or material world or universe. ""Nature"" can refer to the phenomena of the physical world, and also to life in general. The study of nature is a large part of science. Although humans are part of nature, human activity is often understood as a separate category from other natural phenomena.The word nature is derived from the Latin word natura, or ""essential qualities, innate disposition"", and in ancient times, literally meant ""birth"". Natura is a Latin translation of the Greek word physis (φύσις), which originally related to the intrinsic characteristics that plants, animals, and other features of the world develop of their own accord. The concept of nature as a whole, the physical universe, is one of several expansions of the original notion; it began with certain core applications of the word φύσις by pre-Socratic philosophers, and has steadily gained currency ever since. This usage continued during the advent of modern scientific method in the last several centuries.Within the various uses of the word today, ""nature"" often refers to geology and wildlife. Nature can refer to the general realm of living plants and animals, and in some cases to the processes associated with inanimate objects – the way that particular types of things exist and change of their own accord, such as the weather and geology of the Earth. It is often taken to mean the ""natural environment"" or wilderness–wild animals, rocks, forest, and in general those things that have not been substantially altered by human intervention, or which persist despite human intervention. For example, manufactured objects and human interaction generally are not considered part of nature, unless qualified as, for example, ""human nature"" or ""the whole of nature"". This more traditional concept of natural things which can still be found today implies a distinction between the natural and the artificial, with the artificial being understood as that which has been brought into being by a human consciousness or a human mind. Depending on the particular context, the term ""natural"" might also be distinguished from the unnatural or the supernatural.