Full Unit Plan (MS Word)
... This unit engages students in an in-depth, student-directed investigation and several guided inquiries to discover, test, and use The Theory of Plate Tectonics. Plate tectonics is a relatively new, well-supported scientific theory that helps explain Earth’s landforms, catastrophic events like earthq ...
... This unit engages students in an in-depth, student-directed investigation and several guided inquiries to discover, test, and use The Theory of Plate Tectonics. Plate tectonics is a relatively new, well-supported scientific theory that helps explain Earth’s landforms, catastrophic events like earthq ...
Plate Tectonics - Hope Valley Library
... who figured out that freshwater dinosaur fossils were found in spots across the country . The thing is the sections are separated by salt oceans. That means that since the dinosaurs could not cross the water the land had to be connected at their time. He was the one that figured out that plates move ...
... who figured out that freshwater dinosaur fossils were found in spots across the country . The thing is the sections are separated by salt oceans. That means that since the dinosaurs could not cross the water the land had to be connected at their time. He was the one that figured out that plates move ...
The Earth`s Crust
... ■ Most geologists think that all the continents were once part of one big supercontinent called Pangaea. ...
... ■ Most geologists think that all the continents were once part of one big supercontinent called Pangaea. ...
Unit Objectives
... 7. I can explain the theory of plate tectonics. 8. I can use the theory of plate tectonics to explain how sea-floor spreading occurs. 9. I can use the theory of plate tectonics to explain how mid-ocean ridges are formed. 10. I can use the theory of plate tectonics to explain how subduction zones are ...
... 7. I can explain the theory of plate tectonics. 8. I can use the theory of plate tectonics to explain how sea-floor spreading occurs. 9. I can use the theory of plate tectonics to explain how mid-ocean ridges are formed. 10. I can use the theory of plate tectonics to explain how subduction zones are ...
File - Mr Michael mccloskey
... • If you look at a map of the world, you may notice that some of the continents could fit together like pieces of a puzzle. ...
... • If you look at a map of the world, you may notice that some of the continents could fit together like pieces of a puzzle. ...
Obtaining information about inside the earth.
... (hitgabshoot) happens when the chamber cools and the minerals are formed, causing the minerals to be attracted to one another in the magma chamber. Granite is made inside planet earth and is exposed as a result of weathering process and internal process The formation of volcanic (Peretz) Igneous roc ...
... (hitgabshoot) happens when the chamber cools and the minerals are formed, causing the minerals to be attracted to one another in the magma chamber. Granite is made inside planet earth and is exposed as a result of weathering process and internal process The formation of volcanic (Peretz) Igneous roc ...
Chapter Review
... 2. The hypothesis that continents can drift apart and have done so in the past is known as ______________________. 3. The ______________________ is the soft layer of the mantle on which the tectonic plates move. 4. ______________________ is stress that occurs when forces act to stretch an object. 5. ...
... 2. The hypothesis that continents can drift apart and have done so in the past is known as ______________________. 3. The ______________________ is the soft layer of the mantle on which the tectonic plates move. 4. ______________________ is stress that occurs when forces act to stretch an object. 5. ...
Layers of the Earth - Mrs. Rasmussen Science Class
... like: nitrogen (78%), oxygen (21%), and other gases like argon and carbon dioxide (1%). Since there isn’t a distinct boundary between the atmosphere and outer space, it is generally stated that the atmosphere is around 100 km thick but it can extend up to 480 km if you count the very thinnest parts. ...
... like: nitrogen (78%), oxygen (21%), and other gases like argon and carbon dioxide (1%). Since there isn’t a distinct boundary between the atmosphere and outer space, it is generally stated that the atmosphere is around 100 km thick but it can extend up to 480 km if you count the very thinnest parts. ...
Chapter Pages... 4 ..... 21 landform patterns and processes
... - Plates push against each other and create intense heat and pressure and the decay of radioactive materials. - The intense heat melts the rock beneath the crust changing it to magma - The magma flows into cracks and fractures. - If the magma does not reach the surface and fills the cavities between ...
... - Plates push against each other and create intense heat and pressure and the decay of radioactive materials. - The intense heat melts the rock beneath the crust changing it to magma - The magma flows into cracks and fractures. - If the magma does not reach the surface and fills the cavities between ...
Chapter 3:The Dynamic Earth
... World Oceans- Arctic, Pacific, Atlantic, Indian 70% of earth surface Regulates Planet’s environment High salt concentrations (salinity)( lower where freshwater or rain runs into it, high in areas where evaporation is high) • Temperature zones- surface warmed by sun, deep clod no sunlight (surface zo ...
... World Oceans- Arctic, Pacific, Atlantic, Indian 70% of earth surface Regulates Planet’s environment High salt concentrations (salinity)( lower where freshwater or rain runs into it, high in areas where evaporation is high) • Temperature zones- surface warmed by sun, deep clod no sunlight (surface zo ...
The North American continent has developed through a series of
... The main question to be discussed at the workshop is how to best use USArray to unravel the geologic history in the Great Plains region. The USArray itself will be a group of instruments that are systematically moved across the United States, gathering slices of information about the inner Earth. US ...
... The main question to be discussed at the workshop is how to best use USArray to unravel the geologic history in the Great Plains region. The USArray itself will be a group of instruments that are systematically moved across the United States, gathering slices of information about the inner Earth. US ...
DTU 8e Chap 6 Earth and Moon
... Frozen water has been discovered in numerous places just below the Moon’s surface. The collision-ejection theory of the Moon’s origin, accepted by most astronomers, holds that the young Earth was struck by a huge planetesimal, and debris from this collision coalesced to form the Moon. The Moon was m ...
... Frozen water has been discovered in numerous places just below the Moon’s surface. The collision-ejection theory of the Moon’s origin, accepted by most astronomers, holds that the young Earth was struck by a huge planetesimal, and debris from this collision coalesced to form the Moon. The Moon was m ...
Unit 8 ~ Learning Guide Name
... Using a pencil, complete the following notes as you work through the related lessons. Show ALL work as is explained in the lessons. You are required to have this package completed BEFORE you write your unit test. Do your best and ask questions if you don’t understand anything! ...
... Using a pencil, complete the following notes as you work through the related lessons. Show ALL work as is explained in the lessons. You are required to have this package completed BEFORE you write your unit test. Do your best and ask questions if you don’t understand anything! ...
Instructions: Earth`s Layers Questions
... Using a pencil, complete the following notes as you work through the related lessons. Show ALL work as is explained in the lessons. You are required to have this package completed BEFORE you write your unit test. Do your best and ask questions if you don’t understand anything! ...
... Using a pencil, complete the following notes as you work through the related lessons. Show ALL work as is explained in the lessons. You are required to have this package completed BEFORE you write your unit test. Do your best and ask questions if you don’t understand anything! ...
Name Class___________ Date
... _____1. Limestone is a sedimentary rock and marble is a metamorphic rock. They are classified as different rocks because they: (1) were formed from different fossils (2) formed at different times (3) formed in different ways _____2. Which information would probably be least reliable for someone tryi ...
... _____1. Limestone is a sedimentary rock and marble is a metamorphic rock. They are classified as different rocks because they: (1) were formed from different fossils (2) formed at different times (3) formed in different ways _____2. Which information would probably be least reliable for someone tryi ...
Inside the Earth - Pacific Climate Change Portal
... 3. Lightly tap one half of the egg on a hard surface. The shell will break into fragments that represent earth’s tectonic plates. Carefully lift two of the larger fragments and drop some water underneath them. Now, you can slide those fragments, or plates, more easily. Describe your observations as ...
... 3. Lightly tap one half of the egg on a hard surface. The shell will break into fragments that represent earth’s tectonic plates. Carefully lift two of the larger fragments and drop some water underneath them. Now, you can slide those fragments, or plates, more easily. Describe your observations as ...
Document
... • Many pieces of Earth’s crust, called plates, fit together like a jigsaw puzzle. The plates rest on Earth’s mantle and are always moving. • The theory that Earth’s crust is divided into moving plates is called plate tectonics. • Plates are made from continental crust, oceanic crust, or a combinatio ...
... • Many pieces of Earth’s crust, called plates, fit together like a jigsaw puzzle. The plates rest on Earth’s mantle and are always moving. • The theory that Earth’s crust is divided into moving plates is called plate tectonics. • Plates are made from continental crust, oceanic crust, or a combinatio ...
Inside the Earth
... • Crust and Lithosphere- rigid outer layer • Mantle and Asthenosphere- solid rock that flows slowly (like hot asphalt) • Outer Core- liquid layer • Inner Core- solid, very dense ...
... • Crust and Lithosphere- rigid outer layer • Mantle and Asthenosphere- solid rock that flows slowly (like hot asphalt) • Outer Core- liquid layer • Inner Core- solid, very dense ...
mantle - National Geographic
... the crust and core by measuring the spread of shock waves from earthquakes, called seismic waves. Two types of seismic waves pass through the Earth’s interior: P-waves, which represent vertical motion, and S-waves, which represent horizontal motion. Instruments placed around the world measure these ...
... the crust and core by measuring the spread of shock waves from earthquakes, called seismic waves. Two types of seismic waves pass through the Earth’s interior: P-waves, which represent vertical motion, and S-waves, which represent horizontal motion. Instruments placed around the world measure these ...
Structure of the Earth
... From your reading, you will see… • That the science leading to our understanding of Earth’s structure is interesting and complicated. • It involves Snell’s Law and the physics of wave propagation, wave theory and spherical geometry combined with experimental highpressure mineral physics. • We ...
... From your reading, you will see… • That the science leading to our understanding of Earth’s structure is interesting and complicated. • It involves Snell’s Law and the physics of wave propagation, wave theory and spherical geometry combined with experimental highpressure mineral physics. • We ...
Superplumes and single plumes: their magmatic trails on moving
... provinces), otherwise called superswells, situated within the D00 layer. They represent a paleomagnetically supported “reference frame for movements in and on the Earth” [Torsvik et al., 2014]. Arriving to asthenosphere and then lithosphere, they induce melting, which results in magmatism of various ...
... provinces), otherwise called superswells, situated within the D00 layer. They represent a paleomagnetically supported “reference frame for movements in and on the Earth” [Torsvik et al., 2014]. Arriving to asthenosphere and then lithosphere, they induce melting, which results in magmatism of various ...
ES Ch 1 NOTES Plate Tectonics
... creatures have been found on opposite shores, like the Mesosaurus. ...
... creatures have been found on opposite shores, like the Mesosaurus. ...
Earth`s Tectonic Plates - kmstorres
... Pressure builds up. It is released when there are earthquakes. ...
... Pressure builds up. It is released when there are earthquakes. ...
Chapter 5: Plate Tectonics
... What are the characteristics of Earth's crust, mantle, and core? ...
... What are the characteristics of Earth's crust, mantle, and core? ...
Spherical Earth
The concept of a spherical Earth dates back to around the 6th century BC, when it was mentioned in ancient Greek philosophy, but remained a matter of philosophical speculation until the 3rd century BC, when Hellenistic astronomy established the spherical shape of the earth as a physical given. The paradigm was gradually adopted throughout the Old World during Late Antiquity and the Middle Ages. A practical demonstration of Earth's sphericity was achieved by Ferdinand Magellan and Juan Sebastián Elcano's expedition's circumnavigation (1519−1522).The concept of a spherical Earth displaced earlier beliefs in a flat Earth: In early Mesopotamian mythology, the world was portrayed as a flat disk floating in the ocean and surrounded by a spherical sky, and this forms the premise for early world maps like those of Anaximander and Hecataeus of Miletus. Other speculations on the shape of Earth include a seven-layered ziggurat or cosmic mountain, alluded to in the Avesta and ancient Persian writings (see seven climes).The realization that the figure of the Earth is more accurately described as an ellipsoid dates to the 18th century (Maupertuis).In the early 19th century, the flattening of the earth ellipsoid was determined to be of the order of 1/300 (Delambre, Everest). The modern value as determined by the US DoD World Geodetic System since the 1960s is close to 1/298.25.