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REVISED EXAM 3 STUDY GUIDE – PHYSICAL GEOGRAPHY
REVISED EXAM 3 STUDY GUIDE – PHYSICAL GEOGRAPHY

... a. Along the mid-ocean ridges b. Around the Pacific Ring of Fire c. In California d. In the Appalachians ...
information about earth`s layers
information about earth`s layers

... outer core is made of iron and is very dense. Scientists hypothesize that the circulation of the outer core causes the magnetic field around the earth. It is believed to be circulating in the counter-clockwise direction giving us the north pole in its present location. It switches about every millio ...
Journey to the Center of the Earth
Journey to the Center of the Earth

... (under the continents). The crust encompasses the brittle and shifting continental plates; it becomes scarred with mountains when the plates grind together or with deep ocean basins when the plates pull apart. The Mantle This deep layer of warm rock accounts for two-thirds of the mass of our planet. ...
Catastrophic Events
Catastrophic Events

...  I understand earthquake waves help scientists to construct hypotheses about the structure of the earth’s interior.  I understand the earth has layers, including a crust, a mantle, and a core; the core is divided into a liquid outer core and a solid inner core.  I understand the crust and rigid p ...
now and ice cores from antarctica , greenland and high altitude
now and ice cores from antarctica , greenland and high altitude

... ) 20.2 , thanks to the extensive study of deep ice cores drilled at Vostok , Dome C and Dome F in central East Antarctica . For Greenland , available data cover the past 100 000 years , thanks to the analysis of the GRIP and GISP 2 ice cores drilled at Summit in central Greenland . They show a succe ...
UNit 2 earth science quiz
UNit 2 earth science quiz

... Alfred Wegner’s theory that the continents must have been together at one time in Earth’s history and thus have the ability to move (drift) A opening in the oceanic crust where molten materials from the mantle escape A plate boundary at which plates move toward each other and collide A long, narrow, ...
Science Background Information
Science Background Information

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Midterm 1, Winter 2012 with answers
Midterm 1, Winter 2012 with answers

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... Earth, and how do we know all of this “stuff” without having been there? The center of the Earth is too hot and too high of a pressure. We know about the inside of the Earth because of Seismological Studies. 41. Why is it so hot in the middle of the Earth? Left over heat from the formation of the so ...
Physical Science - Harrison County Schools
Physical Science - Harrison County Schools

... chemical properties of a substance cause it to react in predictable ways with other substances to form compounds with different characteristic properties. In chemical reactions, the total mass is conserved. Substances are often classified into groups if they react in similar ways. The patterns that ...
Plate Tectonics A . Alfred Wegner 1. Continental drift hypothesis a
Plate Tectonics A . Alfred Wegner 1. Continental drift hypothesis a

... b. occurs where a slab of the ocean floor is displaced vertically along a fault  c. can also occur when the vibration of a quake sets an underwater landslide  into motion  d. although tsunamis travel very rapidly, there is sufficient time to evacuate  all but the area closest to the epicenter  ...
Earth Systems
Earth Systems

...  Because of the heat, the metals are molten and flow like a thick liquid. ...
Magma ocean influence on early atmosphere composition and mass
Magma ocean influence on early atmosphere composition and mass

How did plate tectonics emerge on Earth?
How did plate tectonics emerge on Earth?

... The lithosphere1, the Earth's outermost mobile layer, is divided into a small number of rigid plates that move over the asthenosphere, the part of the Earth's mantle located immediately beneath it. This system is responsible for geological phenomena such as earthquakes and volcanic activity. It also ...
Chapter 10 Section 3
Chapter 10 Section 3

... mantle that transfers heat in Earth's interior and is the driving force for plate tectonics. It is also known as the cycle of heating, rising, and cooling. ...
Ocean Basin Physiography
Ocean Basin Physiography

... example of this kind of activity was provided during the Grand Banks Earthquake off Newfoundland on November 19, 1929 (Figures 5 and 6). Slumping and turbidity currents triggered by the earthquake resulted in breakage of 13 trans-Atlantic telephone and telegraph cables over a period of about 12 hour ...
Physical Jeopardy Review Game2.0
Physical Jeopardy Review Game2.0

... • Added credits and instructions. • Replaced WordArt with title text (for ease of typing). Also altered the text content. ...
Gondwana - The Great Supercontinent
Gondwana - The Great Supercontinent

... supercontinent. The most successful was the myrtle or southern beech (Nothofagus) which provides arguably the strongest evidence for the Gondwanan landmass. There are about 40 living species left today distributed across a number of land masses- three species in Australia, nine in Chile and Patagoni ...
EARTH SCIENCE PRACTICE OGT QUESTIONS
EARTH SCIENCE PRACTICE OGT QUESTIONS

... By studying folds and faults in rocks, scientists can determine the… A. B. C. D. ...
Earth History Benchmark Study Guide 2014 Sedimentary Rocks
Earth History Benchmark Study Guide 2014 Sedimentary Rocks

... more dense oceanic plates under less dense continental plates. Volcanoes occur when water from the ocean is pulled under the less dense continental plate and creates pressure in the magma in the mantle under the continental crust. This pressure builds up forcing the magma towards the surface, eventu ...
Astronomy Test - The Summer Science Safari Summer Camp
Astronomy Test - The Summer Science Safari Summer Camp

... 71. The era we now live in is the _Cenozoic________ Era. 72. At the end of the Paleozoic Era, extinction of many organisms occurred. What caused this to happen? Pangaea formed, climate changed 73. Scientist divide geologic time into eras based on major changes 74. During which era did the greatest e ...
Plate Tectonics
Plate Tectonics

... Fossils, rocks, glaciers, and the bottom of the ocean all revealed a past that did not reflect the current conditions on earth. But what did that mean? Let’s review what scientists found and then look at their conclusion. ...
12 Introduction to the Geology of the Terrestrial
12 Introduction to the Geology of the Terrestrial

... due to a variety of processes. Here we will be concerned with the two main erosion processes due to the presence of an atmosphere: wind erosion, and water erosion. With daytime temperatures above 700o F, both Mercury and Venus are too hot to have liquid water on their surfaces. In addition, Mercury ...
Iceland`s Geothermal Energy - National Geographic Society
Iceland`s Geothermal Energy - National Geographic Society

... In the photos, it appears that smoke is being forced out of the vents in the power plant. What material is in this smoke? The exhaust is steam. Steam is being released into the atmosphere from the large vents on the top of the plant. Steam, which is composed of water particles, has little impact on ...
Word Bank Crust Inner core Mantle Outer Core Lithosphere
Word Bank Crust Inner core Mantle Outer Core Lithosphere

... 1. Where are Earth’s tectonic plates located? A. They float just below the crust. B. They float on top of the inner core. C. They float on top of the lower mantle D. They float on the atmosphere 2. Most of Earth’s mass is in the A. crust. B. mantle. ...
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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.
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