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Continental Drift Notes
Continental Drift Notes

... In 1912, a German scientist (he was an explorer, astronomer, and meteorologist proposed that at one time all of the continents had been ______________ to form one huge continent  His name was ________________  He called this supercontinent _______________ (it means “all Earth”)  And, over time (m ...
Curriculum Map and Pacing Guide – Earth Systems
Curriculum Map and Pacing Guide – Earth Systems

... composition from other solar system bodies and cite evidence for the body they feel is most like/dislike the Earth (levels 1, 2, 3) ***Develop a logical argument for the age of the Earth and critique other students’ arguments ...
Earth Science Study guide answers
Earth Science Study guide answers

... What are the processes which cause volcanoes to form? Hot Spots are locations where volcanoes form far from plate boundaries ...
Geology - Lone Star College
Geology - Lone Star College

... Global Scale – plate tectonics, mountain building, large scale volcanic eruptions producing global climate change, large meteorites strikes producing global climate change, Ice ages. ...
The Interior of the Earth
The Interior of the Earth

... The Earth is thought to be similar to Meteorites, about 5% of the meteorites are Iron-Nickel metal. These are believed to have been the center of former bodies in space where the Iron-Nickel, a dense material, settled to the center when the body was molten. A later collision broke apart the body int ...
The Earth as a System
The Earth as a System

... Formation of Earth  Most researchers believe that Earth and the other planets formed at essentially the same time from the same primordial material as the Sun.. ...
Astronomy Test - The Summer Science Safari Summer Camp
Astronomy Test - The Summer Science Safari Summer Camp

... 5. If you see a quasar that is 6 billion light-years away, how old is the light you are seeing? 6. What is the Big Bang Theory? What evidence is used to support it?? 7. What type of galaxy is our Milky Way galaxy? 8. What type of stars are the majority of stars in our galaxy? 9. How do we measure th ...
Worksheet: The movement of tectonic plates
Worksheet: The movement of tectonic plates

... joined and have since drifted apart “by earthquakes and floods”. His “evidence” was the jigsaw fit of the continents. This fit is especially close when the continental shelves of the continents are considered. About 165 million years ago, the great southern landmass called Gondwana, split up to form ...
Chapter 3 The Dynamic Earth Section 1, The Geosphere Day 1
Chapter 3 The Dynamic Earth Section 1, The Geosphere Day 1

... • In addition to gases, the atmosphere contains many types of tiny, solid particles, or ______________________________________. Composition of the Atmosphere • In addition to nitrogen and oxygen, other gases such as ___________________________________________________________________ make up the rest ...
docx: Earth`s Interior Pre Assessment
docx: Earth`s Interior Pre Assessment

... 18. On your journey to the center of the Earth, which layer on your map would have the shortest distance to cover? a. The mantle b. The asthenosphere c. The outer core d. They are all the same distance across 19. Heat inside the Earth came/comes from which of the following? a. Collisions during form ...
Lecture 2: Dynamic Earth: Plate Tectonics
Lecture 2: Dynamic Earth: Plate Tectonics

... sites where the ocean crust is drawn back to the mantle. ...
Continental Drift Powerpoint
Continental Drift Powerpoint

... one time all of the continents had been joined together to form one huge continent  His name was Alfred Wegener  He called this supercontinent Pangaea (it means “all Earth”)  And, over time (millions of years), the continents slowly drifted apart and ended up in the positions we see on Earth toda ...
SAI109 Dealing 4 Dynamic Response Earths Surface
SAI109 Dealing 4 Dynamic Response Earths Surface

... Which layers of the earth are composed primarily of rocky material? ...
The Earth`s Layers From least to most dense
The Earth`s Layers From least to most dense

... much deeper. If we can’t go very deep into the earth, how do we know what is below the surface when we can't see it? Isaac Newton (the scientist that discovered gravity) was one of the first scientists to develop theories about the structure of the earth. Based on his studies about gravity, Newton c ...
Studyguide
Studyguide

...  ____________________ is the process of wearing away rocks by natural means  Blowing wind can cause sand to hit rock and over time the sand will wear away the rock by breaking it into smaller pieces Changes Caused by Moving Water  Water can change Earth’s surface by carrying soil and small pieces ...
Earth Systems Science Core Curriculum
Earth Systems Science Core Curriculum

... Science provides evidence that the universe is more than 10 billion years old. The most accepted science theory states that the universe expanded explosively from a hot, dense chaotic mass. Gravity causes clouds of the lightest elements to condense into massive bodies. The mass and density of these ...
Venus
Venus

... •  Temperature
of
surface
reaches
boiling
point
(100
 C
or
212
F)
of
water.

Water
evaporates
from
 oceans,
dumping
H2O
into
atmosphere
‐>
 increasing
temp
‐>
acceleraVng
the
evaporaVon‐>
 dumps
more
water
into
sky
‐>
increases
temp
and
 so
on….
 •  Note
that
Venus
temperature
is
way
beyond
the
 boi ...
Chapter 17 - Auburn City Schools
Chapter 17 - Auburn City Schools

... Varying ages of rocks: pattern ◦ Younger rocks near ridges ◦ Older rocks farther away ...
Science Notes December, 2012 SOL 5.7 Rock Cycle, Weathering
Science Notes December, 2012 SOL 5.7 Rock Cycle, Weathering

... Rock Cycle, Weathering, Erosion, and Human Impact The rock cycle is the ongoing process by which rocks can change from one type to another. The three basic types of rocks are igneous, sedimentary, and metamorphic. These rock types are classified by how they are formed. Igneous rock forms when magma ...
Where did the water for the oceans come from?
Where did the water for the oceans come from?

...  Earliest direct evidence for voyaging was from the Mediterranean. There may well have been intentional or unintentional ocean travel previous to that time.  The origins of marine science lie in voyaging – traveling on the ocean for a purpose, which varied form one culture and time to another. Tec ...
EARTH DIFFERENTIATES
EARTH DIFFERENTIATES

... > Vertical movement of heat & material through time > Lithosphere (plates)- cold strong outer boundary later of earth ...
Name
Name

... Hypothesis for Convergent Boundary: ...
APES Review: Earth Systems and Global Changes
APES Review: Earth Systems and Global Changes

...  Convection in the atmosphere is responsible for global winds (think back to Hadley, Ferrel and Polar cells), formation of some clouds, high and low pressure systems, and ultimately for various climates and biomes.  Convection in the oceans helps to move cold and warm water currents around the glo ...
CGF 3MO - TeacherWeb
CGF 3MO - TeacherWeb

... Multiple Choice – a variety of questions from throughout the course with greater emphasis on material learned since midterm. True or False – primarily questions from the current unit on atmosphere & storms with a few questions from oceans and glaciers Short Answer – questions primarily from material ...
Unit 1 Plate Tectonics UNIT 2: LAYERS OF THE EARTH STUDY
Unit 1 Plate Tectonics UNIT 2: LAYERS OF THE EARTH STUDY

... the tremendous pressure upon it. There are two types of crust: oceanic crust and continental crust. ...
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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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