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Notes: Plate Tectonics - Riverdale Middle School
Notes: Plate Tectonics - Riverdale Middle School

... the theory of continental drift a. __________________- about 225 million years ago 1.) all the continents formed a supercontinent called ...
Oceanography Chapter 4 Bathymetry
Oceanography Chapter 4 Bathymetry

... ♦ Base is granite (an igneous rock) ♦ Much like the continent ♦ 7.4 % ocean area ♦ Most material of shelf is derived from eroded stuff from the continent ♦ Width of shelf is determined by plate boundaries ...
Pangea - Mrs. LeFevre`s Class
Pangea - Mrs. LeFevre`s Class

... Australia, and Antarctica) were one gigantic continent which scientists call Pangaea (pan-gee-uh). The name Pangaea is derived from the Ancient Greek words “pan”  meaning "entire," and “Gaia”  meaning "Earth." Continental drift, the process by which the continents broke apart and spread out across t ...
Earth Science 4
Earth Science 4

... suggesting that Earth continents are moving. – Animal Fossils – Plant Fossils – Landforms • BUT is that good enough? What do you think? • Be a SKEPTIC, discuss other explanations for these so called pieces of evidence. ...
Name Period
Name Period

... 4. Wegener hypothesized that the continents formed part of a single land mass, or __________________. a. mid-ocean ridge. b. monocontinent. c. supercontinent. d. world land. 5. When did Wegener think that small continents began forming? ____________________________. a. 25 million years ago. b. 2.5 b ...
Introduction to Plate Tectonics
Introduction to Plate Tectonics

... According to the theory, the continents were once a part of a super continent. ...
Continental Drift and Plate Tectonics
Continental Drift and Plate Tectonics

... America), Great Rift Valley (East Africa) ...
Plate Tectonics
Plate Tectonics

... were once compressed into a single continent which he called Pangaea (meaning "all lands"), and over time they have drifted apart into their current distribution. He believed that Pangaea was intact until about 300 million years ago, when it began to break up and drift apart. ...
Plate Tectonics Review
Plate Tectonics Review

... Similar geologic features (similar rocks) were found on different continents, matching fossils on different continents, evidence of different climates (such as coal in Antarctica) ...
Plate Tectonic Notes
Plate Tectonic Notes

... II. Theory of Plate Tectonics A. states that the earth’s crust is broken into large moving pieces (plates) to which the continents are attached. B. Why Change the Theory? 1. new technology allows scientists to discover new ...
Evidence for Continental Drift
Evidence for Continental Drift

... coastline and Africa’s western coastline seemed to match, giving Wegener his first piece of evidence for continental drift. The fit suggested that, millions of years ago, all the continents were joined as a “supercontinent” named Pangaea (from the Greek words pan, meaning all, and gaea, meaning Eart ...
Continental Drift and Plate Tectonics Notes
Continental Drift and Plate Tectonics Notes

... 1: ________________________________ ...
Sea-Floor Spreading 49
Sea-Floor Spreading 49

... 5. because sea-floor spreading is due to pulling apart, or movement of plates, at mid-ocean ridges ...
plate driving force
plate driving force

... PLATE MOTIONS CAUSE EARTHQUAKES, VOLCANOS, MOUNTAIN BUILDING AT PLATE BOUNDARIES PLATE TECTONICS MAKES EARTH WHAT IT IS - DIFFERENT FROM ...
Plate Tectonics Inside Earth Chapter 1 Study
Plate Tectonics Inside Earth Chapter 1 Study

... 7. What is the Theory of the Continental Drift and who developed it? Why it was not originally accepted? A. Developed by a scientist named Alfred Wegener 1 His hypothesis was that all the continents has once been joined together as a single landmass and have since drifted apart. 2. He named this sup ...
Continental Drift
Continental Drift

... moved from the tropics to positions closer to the poles ...
Evidence for plate tectonics
Evidence for plate tectonics

... 4- Magnetic Stripes –A geomagnetic reversal is a change in the Earth's magnetic field such that the positions of magnetic north and magnetic south are interchanged. The Earth's field has alternated between periods of normal polarity, in which the direction of the field was the same as the present di ...
Profile: Harry Hess: One of the Discoverers of Seafloor Spreading
Profile: Harry Hess: One of the Discoverers of Seafloor Spreading

... Supporting Wegener’s theory of continental drift, Hess explained how the once-joined continents had separated into the seven that exist today. The continents don’t change dramatically or move independently, but are transported by the shifting tectonic plates on which they rest. The theory also expla ...
Slide 1
Slide 1

... was assembled by 1.0 bya, however, by 750mya it began to split apart ...
Continental Drift & Seafloor Spreading
Continental Drift & Seafloor Spreading

... Older is farther away from ridges- trenches Newer rock will have less deposits on it- more dense, more layers, older rock is at the trenches ...
The Continental Drift Theory
The Continental Drift Theory

... up and the pieces drifted apart from each other, eventually forming the continents as we know them today. Wegener's theory was not well received and was generally not accepted. He did not seem'to have enough hard evidence or proof to support his ideas. In the 1960s, however, scientists uncovered new ...
Name:______________________________  o  ___________________ Samples
Name:______________________________ o ___________________ Samples

...  These rocks only form when molten material cools  ___________________ o Magnetic strips  The earth’s magnetic poles have ___________________ many times  Evidence in the ___________________ on the ocean floor o Drilling Samples  The samples far from the ridge are ___________________  The “youn ...
8.3 PowerPoint
8.3 PowerPoint

... 1. Huge landmass in which all continents were once joined. Pangaea - a 2. Hypothesis that Earth’s continents were once joined in a single landmass and gradually moved apart. Continental drift - d 3. Theory that Earth’s lithosphere is made up of huge, moving plates that are carried around the planet ...
Seafloor Spreading and Paleomagnetism
Seafloor Spreading and Paleomagnetism

... As new crust is created the iron bearing minerals point to where the magnetic pole is at that time. ...
Slide 1
Slide 1

... sedimentary rock • Today these sedimentary rocks form the bedrock for parts of every province • Organisms in seas form basis of oil/gas deposits in west • Swamps (tropical climate) create coal beds in east ...
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Geological history of Earth



The geological history of Earth follows the major events in Earth's past based on the geologic time scale, a system of chronological measurement based on the study of the planet's rock layers (stratigraphy). Earth formed about 4.54 billion years ago by accretion from the solar nebula, a disk-shaped mass of dust and gas left over from the formation of the Sun, which also created the rest of the Solar System.Earth was initially molten due to extreme volcanism and frequent collisions with other bodies. Eventually, the outer layer of the planet cooled to form a solid crust when water began accumulating in the atmosphere. The Moon formed soon afterwards, possibly as the result of a Mars-sized object with about 10% of the Earth's mass impacting the planet in a glancing blow. Some of this object's mass merged with the Earth, significantly altering its internal composition, and a portion was ejected into space. Some of the material survived to form an orbiting moon. Outgassing and volcanic activity produced the primordial atmosphere. Condensing water vapor, augmented by ice delivered from comets, produced the oceans.As the surface continually reshaped itself over hundreds of millions of years, continents formed and broke apart. They migrated across the surface, occasionally combining to form a supercontinent. Roughly 750 million years ago, the earliest-known supercontinent Rodinia, began to break apart. The continents later recombined to form Pannotia, 600 to 540 million years ago, then finally Pangaea, which broke apart 180 million years ago.The present pattern of ice ages began about 40 million years ago, then intensified at the end of the Pliocene. The polar regions have since undergone repeated cycles of glaciation and thaw, repeating every 40,000–100,000 years. The last glacial period of the current ice age ended about 10,000 years ago.
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