7.6 - Solids - mrayton.com
... (high amplitude), or dipping downward which are called synclines (lower amplitude). This folding has produced large mountain ranges such as the Himalayas in Asian and the Alps in Europe. Other mountains can form through two normal faults running parallel to each other, called a fault-block mountain. ...
... (high amplitude), or dipping downward which are called synclines (lower amplitude). This folding has produced large mountain ranges such as the Himalayas in Asian and the Alps in Europe. Other mountains can form through two normal faults running parallel to each other, called a fault-block mountain. ...
A history of supercontinents on planet Earth
... Kenorland and the first Snowball Earth Of course, continents that were just half the size of Australia can't really be considered supercontinents by today's standards, but that was the world in which they existed. The planet was almost entirely ocean at this phase in its history, and cratons weren't ...
... Kenorland and the first Snowball Earth Of course, continents that were just half the size of Australia can't really be considered supercontinents by today's standards, but that was the world in which they existed. The planet was almost entirely ocean at this phase in its history, and cratons weren't ...
The Earth-Moon System
... from the Moon about 3% greater than the force on a unit mass at the Earth’s center, which in turn is 3% greater than the force on a unit mass at the far side of the Earth. 3. On the side of the Earth nearest the Moon, water feels a greater force and flows to the area under the Moon, causing a high t ...
... from the Moon about 3% greater than the force on a unit mass at the Earth’s center, which in turn is 3% greater than the force on a unit mass at the far side of the Earth. 3. On the side of the Earth nearest the Moon, water feels a greater force and flows to the area under the Moon, causing a high t ...
Powerpoint Presentation Physical Geology, 10th ed.
... Geologic Time The best estimate for Earth's age is ~4.6 billion years (same as age of our Solar System, as indicated by meteorites). Historically, there has been much debate over "how fast" geology happens with two different camps of thought: CatastrophismUniformitarianism- ...
... Geologic Time The best estimate for Earth's age is ~4.6 billion years (same as age of our Solar System, as indicated by meteorites). Historically, there has been much debate over "how fast" geology happens with two different camps of thought: CatastrophismUniformitarianism- ...
Crust Solid surface, with great expanses of wate Mantle
... EARTHQUAKES – Plates are giant slabs of rock pushing on each other. They do not glide by smoothly! Sometimes they build up huge amount of energy and then slip violently – an Earthquake! ...
... EARTHQUAKES – Plates are giant slabs of rock pushing on each other. They do not glide by smoothly! Sometimes they build up huge amount of energy and then slip violently – an Earthquake! ...
Standard 3 Students will understand the processes of rock and fossil
... ___________________________________________ result when a large section of the sea floor suddenly moves and therefore displaces a massive amount of water. P or S Wave? Tidal waves get bigger when they reach the shallow __________________________________. What part of the world does it look like that ...
... ___________________________________________ result when a large section of the sea floor suddenly moves and therefore displaces a massive amount of water. P or S Wave? Tidal waves get bigger when they reach the shallow __________________________________. What part of the world does it look like that ...
KEY Earth`s Interiors Lab Sheet Student Name(s): Use the labeled
... crust of the Earth is the same temperature as the air. So, it might be as hot as 35 °C in the desert and below freezing in Antarctica. If you dig down, the temperature goes up. The crust is very thin, just 5-70 km. ...
... crust of the Earth is the same temperature as the air. So, it might be as hot as 35 °C in the desert and below freezing in Antarctica. If you dig down, the temperature goes up. The crust is very thin, just 5-70 km. ...
Situation
... on the base of data of permanent magnetic-variation observations were defined variations of Vize’s induction vector (Parkinson), caused by geodynamic processes in the Earth’s crust and by an influence of ionosphere effects and seismic-tectonic origin; - was investigated a structure of tectonomagneti ...
... on the base of data of permanent magnetic-variation observations were defined variations of Vize’s induction vector (Parkinson), caused by geodynamic processes in the Earth’s crust and by an influence of ionosphere effects and seismic-tectonic origin; - was investigated a structure of tectonomagneti ...
Seismic Waves - Fort Thomas Independent Schools
... • Earthquake waves travel out in all directions from a point where strain energy is released. This point is the focus. • The point on Earth’s surface directly above the focus is the epicenter. ...
... • Earthquake waves travel out in all directions from a point where strain energy is released. This point is the focus. • The point on Earth’s surface directly above the focus is the epicenter. ...
7th Grade Targeted TEKS - Texas Regional Collaboratives
... most of it is solid, the asthenosphere does contain a small amount of molten rock and exhibits plastic properties. It is located below the lithosphere (the crust and upper mantle), between about 100 and 250 kilometers deep. In total, the mantle comprises about 80 percent of the volume of the Earth a ...
... most of it is solid, the asthenosphere does contain a small amount of molten rock and exhibits plastic properties. It is located below the lithosphere (the crust and upper mantle), between about 100 and 250 kilometers deep. In total, the mantle comprises about 80 percent of the volume of the Earth a ...
Slide 1
... Lithosphere, because of its lower density “floats” or “sinks” to find its own isostatic equilibrium. Continental lithosphere is less dense so a larger proportion of it “floats” above the aesthenosphere. Changes in mass cause it to rise and fall. Similar to a boat unloading or loading cargo. Removal ...
... Lithosphere, because of its lower density “floats” or “sinks” to find its own isostatic equilibrium. Continental lithosphere is less dense so a larger proportion of it “floats” above the aesthenosphere. Changes in mass cause it to rise and fall. Similar to a boat unloading or loading cargo. Removal ...
Science 10 - Mr. Laura/ Ms. Reynolds Fleetwood Park Secondary
... 2. There are about 12 major tectonic plates and many smaller ones. • Tectonic plates are all moving at the same time. 3. ____________is thermal energy transfer in the mantle where hot, light magma rises and cold, dense lithospheric plate material sinks. • ____________is the amount of mass contained ...
... 2. There are about 12 major tectonic plates and many smaller ones. • Tectonic plates are all moving at the same time. 3. ____________is thermal energy transfer in the mantle where hot, light magma rises and cold, dense lithospheric plate material sinks. • ____________is the amount of mass contained ...
SECOND GRADE EARTHQUAKES
... surface. But how has this been determined? Many people might answer that question by saying scientists can drill into the Earth with machines. However, the drilling rigs that scientists use can only drill about 20 km in the Earth which is not very deep! In other words, we can only drill into upper p ...
... surface. But how has this been determined? Many people might answer that question by saying scientists can drill into the Earth with machines. However, the drilling rigs that scientists use can only drill about 20 km in the Earth which is not very deep! In other words, we can only drill into upper p ...
Earth Science 2: Earthquakes
... ES09‒Rock Cycle discusses the three major types of rock, and E01‒Stress & Strain explores mechanical stress in greater detail. ...
... ES09‒Rock Cycle discusses the three major types of rock, and E01‒Stress & Strain explores mechanical stress in greater detail. ...
Ocean - abyss of time planet earth
... What Earth processes affect the formation and evolution of continental margins, and what benefits and threats do continental margins offer to mankind? The relatively steep slopes of the continental margins, which extend vertically over several kilometres, can affect the directions of ocean currents ...
... What Earth processes affect the formation and evolution of continental margins, and what benefits and threats do continental margins offer to mankind? The relatively steep slopes of the continental margins, which extend vertically over several kilometres, can affect the directions of ocean currents ...
5-Continental Drift and Plate Tectonics
... bar magnet as it has a north and south pole, but temperatures in the core and mantle are too hot for permanent magnetism. Earth’s magnetism must be ...
... bar magnet as it has a north and south pole, but temperatures in the core and mantle are too hot for permanent magnetism. Earth’s magnetism must be ...
GEOLOGY FOR CIVIL ENGINEERS
... Within the past few decades, geologists have learned that continents creep across the Earth’s surface at a rate of a few centimeters every year. Catastrophic Change in Earth History Chances are small that the river flowing through your city will flood this spring, but if you lived to be 100 years o ...
... Within the past few decades, geologists have learned that continents creep across the Earth’s surface at a rate of a few centimeters every year. Catastrophic Change in Earth History Chances are small that the river flowing through your city will flood this spring, but if you lived to be 100 years o ...
Earth`s Changing Face - Lakewood City Schools
... everything. I realized it was raining volcanic ash!” That story was told by a teacher. Mount Redoubt is a volcano. Volcanoes are places where gases, ash, and lava can spew out from ...
... everything. I realized it was raining volcanic ash!” That story was told by a teacher. Mount Redoubt is a volcano. Volcanoes are places where gases, ash, and lava can spew out from ...
Chapter 3 Jig-Saw
... Describe in your report and in your visual aid how tectonic plates move. Group 2: Asthenosphere What is above me? What is below me? What am I made of? What state of matter do I consist of? What is my thickness? What’s my temperature? Describe how molecules in a liquid behave in your ...
... Describe in your report and in your visual aid how tectonic plates move. Group 2: Asthenosphere What is above me? What is below me? What am I made of? What state of matter do I consist of? What is my thickness? What’s my temperature? Describe how molecules in a liquid behave in your ...
Adlai E. Stevenson High School Course Description
... Describe how the continents were arranged in the past. ...
... Describe how the continents were arranged in the past. ...
Environmental Science THE DYNAMIC EARTH Good overview with
... Air that is constantly moving upward, downward, or sideways causes the Earth’s __ weather. ___. In the troposphere, less dense air warmed by the Earth’s surface, rise into the atmosphere and currents of colder, more dense air sinks. As air current’s rise, they cool, become denser, and sink. So, air ...
... Air that is constantly moving upward, downward, or sideways causes the Earth’s __ weather. ___. In the troposphere, less dense air warmed by the Earth’s surface, rise into the atmosphere and currents of colder, more dense air sinks. As air current’s rise, they cool, become denser, and sink. So, air ...
C:\Users\jmhemzac\Desktop\2016 spring\121rev1s16.wpd
... Name the three types of plate boundaries, describe the relative motion associated with each, and recognize and name geographic examples of each (e.g., from the plate tectonic worksheet) Given appropriate maps, be able to identify the presence of features that are associated with different types of g ...
... Name the three types of plate boundaries, describe the relative motion associated with each, and recognize and name geographic examples of each (e.g., from the plate tectonic worksheet) Given appropriate maps, be able to identify the presence of features that are associated with different types of g ...
Earth internal energy
... Tethys Sea. By the end of the Cretaceous period, the continents were separating into land masses that look like our continents. ...
... Tethys Sea. By the end of the Cretaceous period, the continents were separating into land masses that look like our continents. ...
Unit Rationale - (Secondary) Teacher
... safety in earthquake or volcanic areas. Although student interests and relevancy may not seem to directly promote educational equity, to create a classroom where the students feel that their point of view, interests and life context is relevant promotes equity in the ...
... safety in earthquake or volcanic areas. Although student interests and relevancy may not seem to directly promote educational equity, to create a classroom where the students feel that their point of view, interests and life context is relevant promotes equity in the ...
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.