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Alfred Lothar Wegener, 1880-1930
Alfred Lothar Wegener, 1880-1930

... Such an insight, to be accepted, would require large amounts of supporting evidence. Wegener found that large-scale geological features on separated continents often matched very closely when the continents were brought together. For example, the Appalachian mountains of eastern North America matche ...
Table of Contents - Mr. Tobin`s Earth Science Class
Table of Contents - Mr. Tobin`s Earth Science Class

... strain as the apply to rocks.  Students will be able to distinguish among the three types of movement of faults.  Students will be able to contrast three types of seismic waves. ...
Inside Earth Ch1 Jeopardy
Inside Earth Ch1 Jeopardy

... continuous process of sea-floor spreading. ...
File - Ms Hicks` Classes
File - Ms Hicks` Classes

... wave destroyed houses and flooded basements in Hot Springs Cove and Bamfield on the coast of Vancouver Island. • The wave travelled up Alberni Inlet and flooded town of Port Alberni. • Luckily, no one was killed, but damages caused by the wave totaled over $8 million. ...
Practice Exam #1 – Answer Key
Practice Exam #1 – Answer Key

Dynamic Planet Packet
Dynamic Planet Packet

... models that might be similar to the diagram on the left? ...
Semester 01 Syllabus/Study Guide Accelerated Earth Science
Semester 01 Syllabus/Study Guide Accelerated Earth Science

... 8. Distinguish and compare/contrast various similar items of the natural world based on physical characteristics. Mineral Rock Texture Grains Igneous rock Intrusive Extrusive Sediment Sedimentary rock Compaction Cementation Erosion Deposition Clastic rock Organic rock Chemical rock Metamorphic rock ...
earth dynamics - Index of /~pgres
earth dynamics - Index of /~pgres

... things that you will need to be aware of as you progress through it. However, it is really vital that you use this booklet in concert with the general School of GeoSciences “Handbook for Year 1 and Year 2 Courses” and with the Earth Dynamics Learn location on the School website – you should find all ...
Unit 3: Plate Tectonics Slideshow REGENTS
Unit 3: Plate Tectonics Slideshow REGENTS

... 2. Heat leftover from Earth’s formation and produced by radioactive decay creates DENSITY differences in the mantle. 3. This causes the fluid mantle to flow. 4. The flow of mantle material pulls on the crust above it…like a leaf on a stream ...
Earthquakes - Library Video Company
Earthquakes - Library Video Company

Geology and Nonrenewable Mineral Resources
Geology and Nonrenewable Mineral Resources

... Tectonic plates have rearranged the earth’s continents and ocean basins over millions of years like pieces of a gigantic jigsaw puzzle. The plates have three types of boundaries. Natural hazards such as earthquakes and volcanoes are likely to be found at plate boundaries. ...
GEO/OC 103 Exploring the Deep… Lab 2
GEO/OC 103 Exploring the Deep… Lab 2

... cooled enough for water to accumulate, forming the early oceans. Scientists think that this is when the crust began to differentiate into two types — continental and oceanic crust — because the process that forms granite, the most common type of continental rock, requires the presence of water. The e ...
Sea-Floor Spreading - Madison County Schools
Sea-Floor Spreading - Madison County Schools

... able to look into a rift valley and examine something called pillow lava, which is a special type of solid rock that only forms on the ocean floor when magma cools very rapidly. This proved that new molten material was being added to the ocean floor at these ridges. ...
Earth Structure
Earth Structure

... • 1963 – J. Tuzo Wilson observed that some volcanoes exist far from plate boundaries – He theorized that hot spots are small melting areas within the mantel where thermal plumes cause magma columns to push up through the crust (forming volcanoes) •Hot spots can occur at fault lines although most for ...
File
File

... 1. Depletion time for a resource depends on how long it takes to use up a certain proportion (usually 80%) at a given rate of use. 2. Depletion time is extended by recycling, reusing, and reducing consumption of a given resource. 3. New discoveries of a resource extend the depletion time. 4. The dem ...
Crust
Crust

... • Geophysical surveys: seismic, gravity, magnetic, electrical, geodesy – Acquisition: land, air, sea and satellite – Geological surveys: fieldwork, boreholes, mines ...
2. Plate tectonics
2. Plate tectonics

... Plate Tectonics: a unifying View of Earth Plate Tectonics —  Compelling model of dynamic Earth —  Explains many of Earth’s large-scale surface features and related ...
PowerPoint- Ocean Floor Features
PowerPoint- Ocean Floor Features

... (abyssal hills) less than 1 kilometer above the deep ocean floor ...
LAYERS OF THE EARTH MODEL
LAYERS OF THE EARTH MODEL

... Size of the layers are proportional in relation to each other (i.e. crust is thinnest, mantle is thickest, etc) Element Composition of all layers included Temperature of all layers included Size of all layers included Structure is neat and attractive Use of materials is creative ...
for true or “F” - University of South Alabama
for true or “F” - University of South Alabama

... 2. (T F) The fundamental structure of silicate minerals is built upon the silicon-oxygen tetrahedron (SiO4). 3. (T F) After a theory has survived much scientific scrutiny, it may be elevated to hypothesis status. 4. (T F) Convergent plate tectonic boundaries are located where plates move toward one ...
Shake Table
Shake Table

... broken up into several pieces, known as plates. Convection currents in the liquid mantle pull the plates, causing them to move against one another (plate tectonics). Most earthquakes occur where plates come together (plate boundaries). The state of California spans over 2 plates: the North American ...
CHAPTER 3
CHAPTER 3

... Related or supporting concepts: - Along convergent boundaries where at least one of the plate edges is oceanic, a trench will form and oceanic lithosphere will be subducted into the mantle. - Where two continental margins converge there will be a buckling of the crust and formation of a mountain ran ...
Volcanic Hot Spots
Volcanic Hot Spots

... Volcanic Hot Spots 1. Where do most volcanoes form? ...
1 Plate Tectonics Review w
1 Plate Tectonics Review w

... all caused by the same process. Subduction Zone same process as Andes ...
An overview of mass movement
An overview of mass movement

... The term mass wasting (sometimes called mass movement) encompasses a broad array of processes whereby earth material is transported down a slope by the force of gravity. It is related closely to weathering, which is the breakdown of minerals or rocks at or near Earth's surface through physical, chem ...
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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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