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Astronomy 1 – Winter 2011
Astronomy 1 – Winter 2011

Natural Causes of Climate Change
Natural Causes of Climate Change

... and broke down the food chain. • This catastrophic collision is evident around the world from a thin layer of sediment deposit called the K-T boundary where it separates the end of the Cretaceous period, and the beginning of the Tertiary Period. • The K-T boundary is made up of iridium material whic ...
EssayFinal
EssayFinal

... The Asthenosphere, also known as the Low velocity zone which is called this because body waves, especially P waves travel much faster above and below this zone which can range from 100km to 300km in depth, S waves can travel though it which proves is not a continuous liquid but does slow them down. ...
AWegener_DavidH
AWegener_DavidH

... •Wrote a textbook called The Origin of Continents and Oceans •Came up with theory of continental drift •Proposed that there was a super-continent called Pangaea. ...
2. Key Question 1
2. Key Question 1

... Section 5.1 Forces in Earth’s Crust Reading Notes ...
Guided Notes – Lithospheric Plates
Guided Notes – Lithospheric Plates

7th Grade Science Notes
7th Grade Science Notes

... Wegener formed an hypothesis that the continents had once been joined together in a giant landmass he called “Pangea” meaning “all lands”. He also thought that they had drifted into their present position so his theory became known as the “Continental Drift Theory”. Wegener spent many years searchin ...
NAME: DATE: PERIOD:
NAME: DATE: PERIOD:

... Earth’s core contains iron and nickel, making it a giant magnet. ...
Spring 2007 Earth Science
Spring 2007 Earth Science

... Which natural resource found in Virginia is a common source of energy? F G H J ...
Presentation for perspective graduate students 2006
Presentation for perspective graduate students 2006

... The Earth is the only world known so far to harbor life. There is nowhere else, at least in the near future, to which our species could migrate. Visit, yes. Settle, not yet. Like it or not, for the moment the Earth is where we make our stand. It has been said that astronomy is a humbling and charact ...
Layers of the Earth and Plate Tectonics
Layers of the Earth and Plate Tectonics

... *This is like the magma in the mantle. The magma heats and rises to the surface and then cools and sinks. *Convection currents are what makes our plates move. *The heat from the core powers convection currents. ...
Earthquakes
Earthquakes

... Two of the crusts plates rub against each other and stick in one place. Pressure builds up as they try and move past each other. Suddenly, the pressure is too much and the plates jerk past each other. The place where this happens is called the focus. Vibrations go out in all directions through the r ...
Earth and Space Science (The Rock and Fossil Record)
Earth and Space Science (The Rock and Fossil Record)

... Content Statement ESS.1.2 Earth’s crust consists of major and minor tectonic plates that move relative to each other. ESS.1.2.a Historical data and observations such as fossil distribution, paleomagnetism, continental drift and sea-floor spreading contributed to the theory of plate tectonics. The ri ...
DoubleJeopardy2
DoubleJeopardy2

... C. Shale ...
Earth`s Structure
Earth`s Structure

... primarily made up of _________________________ and _________________________. Plate Tectonics 10. What evidence did Wegner find that supports the hypothesis that the Earth’s continents were once joined in a single large landmass? ...
The Earth How the crust moves…
The Earth How the crust moves…

... • Most are located on ocean floor, a few on land – Friction spawns earthquakes along slipstrike faults ...
A Brief History of Planetary Science
A Brief History of Planetary Science

... circulating, producing global weather patterns ...
Plate BoundaryTypes
Plate BoundaryTypes

... Rising hot rock forces the crust upward and out, along with the pulling of the plates already separating the crust. This causes large slabs of rock to sink, forming a rift valley. Continental divergence is currently occurring at the western edge of the Arabian plate. ...
2013-2014_PACING_GUIDE_EARTH_SCIENCE
2013-2014_PACING_GUIDE_EARTH_SCIENCE

... The rotation of the earth affects the movement of fluids. Energy transfer between the sun and earth's surface creates climate and weather patterns. The climate and weather on earth is affected by the composition of the ...
Earth PowerPoint
Earth PowerPoint

... Half-lives have been measured in the laboratory for almost all known isotopes. The most useful isotope for dating rock samples is uranium-238, which has a halflife of 4.5 billion years, comparable to the age of the Earth. ...
The Earth`s Interior & Plate Tectonics
The Earth`s Interior & Plate Tectonics

... numerous smaller segments called plates that are in motion relative to each other. ...
EARTH
EARTH

... • Arrive after P waves • Shear wave • Can travel through ...
course outline - UTSC - University of Toronto
course outline - UTSC - University of Toronto

... Planet Earth formed about 4.56 billion (Giga annum or Ga) years ago by condensation and accretion of planetary debris. The oldest rocks are dated at about 4 Ga, the oldest bacterial life forms at about 3.5 Ga and an oxygenated atmosphere developed somewhere around 2 Ga before present. Multicellular ...
Geology study guide
Geology study guide

...  Sedimentary rocks form when weathering breaks down rocks and erosion carries it to a different location  the oldest fossils are found in this type of ...
Chapter 5 Test
Chapter 5 Test

... Who came up with the idea of Pangaea? What is not evidence to support Pangaea? Tectonic plates can be made up of what two types of crust? At a mid-ocean ridge, the two plates are____________________________? In seafloor spreading the oldest rocks are found where? The major lithospheric plate the con ...
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History of geology



The history of geology is concerned with the development of the natural science of geology. Geology is the scientific study of the origin, history, and structure of the Earth. Throughout the ages geology provides essential theories and data that shape how society conceptualizes the Earth.
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