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Layers of Earth Notes
Layers of Earth Notes

KS3 Russia
KS3 Russia

... Mountains (in the USA), the Ural Mountains formed about 300 million years ago, near the end of the Carboniferous period, when the first reptiles were evolving. This was when the tectonic plates began to form the supercontinent of Pangaea. When the western Siberia plate smashed into the Baltica and N ...
msword - rgs.org
msword - rgs.org

... Mountains (in the USA), the Ural Mountains formed about 300 million years ago, near the end of the Carboniferous period, when the first reptiles were evolving. This was when the tectonic plates began to form the supercontinent of Pangaea. When the western Siberia plate smashed into the Baltica and N ...
Chapter 9 – the Moon
Chapter 9 – the Moon

... Earth, no geological activity for a long time (plate tectonics, wind, water erosion) ...
File
File

• Internal Structure of Earth and Plate Tectonics • Chapter 2 The
• Internal Structure of Earth and Plate Tectonics • Chapter 2 The

8th Grade Science
8th Grade Science

... • Weight is gravitational force and is often confused with mass. Weight is proportional to mass, but depends upon the gravitational field at a particular location. An object will have the same mass when it is on the moon as it does on Earth. However, the weight (force of gravity) will be different ...
Studyguide_PTtest
Studyguide_PTtest

... ~ The theory Harry Hess put forth – What did he find? What other evidence added to the idea that the seafloor was spreading? (new crust formed at mid-ocean ridge – younger closer to ridge, older farther away; trenches & subduction zones; magnetic striping of seafloor) ~ The 4 basic layers of the Ear ...
Continental Drift and Plate Tectonics ANSWER KEY
Continental Drift and Plate Tectonics ANSWER KEY

... 11.) Diverging plates create: mid ocean ridges such as the Mid-Atlantic ridge that runs north to south along the middle of the Atlantic Ocean between North and South America and Europe and Africa. 12.) Transform boundaries are where plates slide by one another, but because they are jagged they often ...
Chapter 10-2 - Seafloor Spreading
Chapter 10-2 - Seafloor Spreading

... sound waves to detect (to find) submarines.  In the 1940’s during World War II, scientists began to use sound waves to map the ocean floor.  This is sometimes called echo sounding.  Sound waves echo off the bottom of the ocean, so the longer the sound waves take to return to a ship the deeper the ...
Earthquakes
Earthquakes

... Gap Hypothesis-states that sections at active faults that have had relatively few earthquakes are likely to have strong earthquakes in the future Seismic Gap-an area along a fault where relatively few earthquakes have occurred Moho-a place within the earth where the speed of seismic waves increases ...
Sonar (stands for Sound Navigation and Ranging)
Sonar (stands for Sound Navigation and Ranging)

...  Scientists are able to measure the direction and speed of ocean currents.  Measure the different heights of the ocean surface to make maps of ocean floor.  Can cover more territory using ...
The 2002 Johannesburg World Summit on Sustainable Development
The 2002 Johannesburg World Summit on Sustainable Development

... December 1989: UN General Assembly decided to call an "Earth Summit" - negotiations began on FCCC and CBD to have them ready for signature at the Convention - also desertification (led to convention), set of forest principles - Agenda 21 on Sustainability: an action plan - Rio Declaration At Rio: 15 ...
Earth Science Notes - watertown.k12.wi.us
Earth Science Notes - watertown.k12.wi.us

... Evidence shows the plates move… How do they move? Convection is caused by differences in • Heat rises because the molecules move pushing other molecules out of the way making ...
Science Grade 6 - Norwich City Schools
Science Grade 6 - Norwich City Schools

Marks`s powerpoint presentation (as a pdf), 0
Marks`s powerpoint presentation (as a pdf), 0

raging planet - Classroom@Sea
raging planet - Classroom@Sea

the_solid_earth
the_solid_earth

... The process of compaction and cementation is known as lithication. Some common types of sedimentary rocks are limestone, shale, and sandstone. Gypsum represents a sedimentary rock precipitated from solution. Fossil fuels such as coal and oil shale are sedimentary rocks formed from organic matter. M ...
09-SCIENCE GRADE 6 RN
09-SCIENCE GRADE 6 RN

... know energy entering ecosystems as sunlight is transferred by producers into chemical energy through photosynthesis and then from organism to organism through food webs. know matter is transferred over time from one organism to others in the food web and between organisms and the physical environmen ...
Dynamic Ocean Floor
Dynamic Ocean Floor

... • Two plates move away from one another. • This is a zone of weakness. • As two plates move apart at the mid-ocean ridges, magma from the mantle up wells through a crack in the oceanic crust and cooled by the sea creating new ocean floor. • Energy is released in the form of earthquakes. • Shallow fo ...
Determining Earth`s Interior Structure
Determining Earth`s Interior Structure

... Long-Term Climatic Change ...
Review Worksheet – Mechanical and Chemical Weathering and
Review Worksheet – Mechanical and Chemical Weathering and

... Water Dissolves Minerals in Rocks ...
File
File

... A. The process of moving materials from their source to another location through weathering. B. The breaking down of rock soil and minerals. C. Magma coming up from the Earth’s mantle through openings in the crust. 2. Wind carrying abrasive materials blows against a rock formation, wearing it down o ...
Continental drift and plate tectonics
Continental drift and plate tectonics

... around the world because Australia was so isolated. The marsupials had no competition from placental mammals for a long time, so they thrived. Australia’s isolation from the rest of the world meant that unique flora and fauna could evolve. Even though new species have been introduced into Australia, ...
Structure of the Earth Lithosphere System In this lecture we will learn
Structure of the Earth Lithosphere System In this lecture we will learn

... The lithosphere consists of the oceanic crust, continental crust, and uppermost mantle. Beneath the lithosphere is the asthenosphere. This layer, which is also part of the upper mantle, extends to a depth of about 200 kilometers. Sedimentary deposits are commonly found at the boundaries between the ...
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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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