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Chapter 1, Section 1 – Earth`s Interior
Chapter 1, Section 1 – Earth`s Interior

... c. Lower mantle: solid material that extends to core iii. Core: innermost layer of mantle 1. made of iron and nickel 2. two parts: a. liquid (molten metal) outer core b. solid metal inner core (under too much pressure for iron and nickel molecules to spread out) b. Core and magnetic field i. Created ...
GRAĐA ZEMLJE
GRAĐA ZEMLJE

... 3.3 Billion Years Ago? ...
03 Natural Causes of Climate Change
03 Natural Causes of Climate Change

... • Depending on their size, their impacts on climate can be larger than ...
Today`s Objectives
Today`s Objectives

... A. Earth is divided into three layers- the crust, mantle, and core. 1. Earth’s layers are arranged by their densities ...
Review for CFE-answers
Review for CFE-answers

... Cosmic Background radiation is believed to be the leftover energy from the Big Bang. The Doppler Effect shows, using wavelengths, which direction stars and galaxies are moving. Generally it shows these objects moving away from Earth. 4 = 1, 2, 1 ch 1:9 4. Describe the evolution of stars with a mass ...
Jeopardy
Jeopardy

... Type answer to appear with a mouse-click here ...
Earth
Earth

... Oceanic crust, primarily basaltic, is much thinner than continental crust. ...
sample test1 - this is only for questions style
sample test1 - this is only for questions style

... All of the following phrases below describe science: a) Science is the ability to formulate ideas. b) Science is the study of nature using observation and deductive reasoning c) Science is the method used to test an idea. d) Science will assume answers based on preconceived ideas. Science is: a) not ...
PPT-chp-6_edited
PPT-chp-6_edited

... atmosphere indicates that it contains life Earth has “environmental fitness” ...
Lecture - faculty
Lecture - faculty

... not whether warming exists, but its origin. • Increased greenhouse gases (carbon dioxide, methane, etc) act like a blanket to block the escape of infrared “heat” light. • The Earth has also undergone cycles in the past. • The main concern is the impact and control of warming. ...
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File

... 4) Axis- An imaginary line that passes through Earth’s center and the North and South Poles about which Earth rotates. 5) Big Bang- The initial explosion that resulted in the formation and expansion of the universe. 6) Bio- Life or living. 7) Cementation- The process by which dissolved minerals crys ...
Name:
Name:

... 5. The core (of the Earth) is composed mostly of ___________ and _____________. 6. In the ______________ core, the iron and nickel are ______________. 7. Although the inner core is very hot, intense pressure from the weight of the rest of the ____________ prevents the material of the inner core from ...
Slide 1
Slide 1

... http://www.youtube.com/watch?v=gmwylbF3-CA&feature=related ...
Plate Tectonics - Fort Thomas Independent Schools
Plate Tectonics - Fort Thomas Independent Schools

... In sea-floor spreading, the sea floor spreads apart along both sides of a mid-ocean ridge as new crust is added to the ocean floor. As a result, the ocean floors move like conveyor belts, carrying the continents along with ...
Layers of the Earth Lyrics and Diagram
Layers of the Earth Lyrics and Diagram

... The inner core, outer core, mantle, and crust Verse I The layer we’ll discuss first Is the central inner core, in the center of the earth A solid ball buried below the dirt We believe it’s primarily metallic iron You could never take a trip to the inner core, right? The heat will burn you up, 9,000º ...
Changes to Earth`s Surface
Changes to Earth`s Surface

... ocean floor to rise and fall and produces a large destructive wave that can travel great distances. What are the effects of a tsunami? Tsunamis flood costal regions and cause major damage and erosion. ...
The Layers of the Earth
The Layers of the Earth

...  Geologists have found rocks on earth’s surface that they believe were originally formed INSIDE the earth. These rocks are at the surface of the earth NOW…. but millions of years ago, they existed _______ ________ the earth. ...
VIDEO WEB HIT HOMEWORK – part 2
VIDEO WEB HIT HOMEWORK – part 2

... - Within a couple of hundred million years, the moon was formed - Generally, the only rocks available for the beginning of this time are meteorites - During this Hadean time, the Earth became layered (differentiated) with a core. An atmosphere and the oceans were beginning to develop by “outgassing” ...
Dangerous Earth: a plate tectonic story
Dangerous Earth: a plate tectonic story

... If you could sit in space and study the Earth you might see some strange patterns through the swirls of cloud. Many of the mountains are found in long chains; islands are found in long, curved chains; the coastline of South America fits the coast of Africa almost exactly. If you could probe beneath ...
Dangerous Earth: a plate tectonic story
Dangerous Earth: a plate tectonic story

... If you could sit in space and study the Earth you might see some strange patterns through the swirls of cloud. Many of the mountains are found in long chains; islands are found in long, curved chains; the coastline of South America fits the coast of Africa almost exactly. If you could probe beneath ...
Dangerous Earth: a plate tectonic story
Dangerous Earth: a plate tectonic story

... If you could sit in space and study the Earth you might see some strange patterns through the swirls of cloud. Many of the mountains are found in long chains; islands are found in long, curved chains; the coastline of South America fits the coast of Africa almost exactly. If you could probe beneath ...
Plate Tectonics - Department of Physics and Astronomy
Plate Tectonics - Department of Physics and Astronomy

... • Plate Tectonics: A Unifying View of Earth • Another Look at Volcanoes and Earthquakes ...
CRCT Review Packet
CRCT Review Packet

... to another. For example, rock A is older than rock B. 46.The Principle of Superposition states that in a horizontal sedimentary rock layer, the __________________ rocks are on the bottom. The layer on top would be ________________. 47.Radioactive dating is one method for determining the ____________ ...
Ch 5 S 1 Earth`s Interior
Ch 5 S 1 Earth`s Interior

... iv.After several tens of kilometers, the temperature increase slows. v.The high temperatures are the result of heat left over from the formation of Earth ...
The Interior of the Earth
The Interior of the Earth

... An understanding of the interior of the Earth helps us to understand the driving force behind plate tectonics. (Click on image for a video – 5:42) ...
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History of Earth



The history of Earth concerns the development of the planet Earth from its formation to the present day. Nearly all branches of natural science have contributed to the understanding of the main events of the Earth's past. The age of Earth is approximately one-third of the age of the universe. An immense amount of biological and geological change has occurred in that time span.Earth formed around 4.54 billion years ago by accretion from the solar nebula. Volcanic outgassing probably created the primordial atmosphere, but it contained almost no oxygen and would have been toxic to humans and most modern life. Much of the Earth was molten because of frequent collisions with other bodies which led to extreme volcanism. One very large collision is thought to have been responsible for tilting the Earth at an angle and forming the Moon. Over time, the planet cooled and formed a solid crust, allowing liquid water to exist on the surface.The first life forms appeared between 3.8 and 3.5 billion years ago. The earliest evidences for life on Earth are graphite found to be biogenic in 3.7-billion-year-old metasedimentary rocks discovered in Western Greenland and microbial mat fossils found in 3.48-billion-year-old sandstone discovered in Western Australia. Photosynthetic life appeared around 2 billion years ago, enriching the atmosphere with oxygen. Life remained mostly small and microscopic until about 580 million years ago, when complex multicellular life arose. During the Cambrian period it experienced a rapid diversification into most major phyla. More than 99 percent of all species, amounting to over five billion species, that ever lived on Earth are estimated to be extinct. Estimates on the number of Earth's current species range from 10 million to 14 million, of which about 1.2 million have been documented and over 86 percent have not yet been described.Geological change has been constantly occurring on Earth since the time of its formation and biological change since the first appearance of life. Species continuously evolve, taking on new forms, splitting into daughter species, or going extinct in response to an ever-changing planet. The process of plate tectonics has played a major role in the shaping of Earth's oceans and continents, as well as the life they harbor. The biosphere, in turn, has had a significant effect on the atmosphere and other abiotic conditions on the planet, such as the formation of the ozone layer, the proliferation of oxygen, and the creation of soil.
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