Powerpoint for today
... mantle allow molten material to rise => volcanoes. Core temperature is 6000 K. Metallic - mostly nickel and iron. Outer core molten, inner core solid. Atmosphere very thin ...
... mantle allow molten material to rise => volcanoes. Core temperature is 6000 K. Metallic - mostly nickel and iron. Outer core molten, inner core solid. Atmosphere very thin ...
prompt questionnaire for teachers
... 3. There are metamorphic rocks here. 4. A peninsula. 5. In Co. Mayo. (Annagh Head) ...
... 3. There are metamorphic rocks here. 4. A peninsula. 5. In Co. Mayo. (Annagh Head) ...
Visualizing Earth Science
... • Explain the connection between earthquakes and plate tectonics. • Identify several earthquake-related hazards. • Define body waves and surface waves. • Explain how the materials in Earth’s interior affect seismic waves. • Define and describe the composition of Earth’s crust, mantle and core. ...
... • Explain the connection between earthquakes and plate tectonics. • Identify several earthquake-related hazards. • Define body waves and surface waves. • Explain how the materials in Earth’s interior affect seismic waves. • Define and describe the composition of Earth’s crust, mantle and core. ...
Chapter 11
... The fluid outer core generates at least 90% of Earth's magnetic field and the magnetosphere that surrounds and protects Earth from the solar wind (A flow of gas and energetic charged particles, mostly protons and electrons [plasma] which stream from the sun). An intriguing feature of Earth's magneti ...
... The fluid outer core generates at least 90% of Earth's magnetic field and the magnetosphere that surrounds and protects Earth from the solar wind (A flow of gas and energetic charged particles, mostly protons and electrons [plasma] which stream from the sun). An intriguing feature of Earth's magneti ...
Sc 7 Unit 5 Rocks and Minerals
... why you believe those are the most reliable sites from a scientific point of view. Dig This! The Cretaceous Period Explore for fossils and uncrate the Cretaceous Period then move on to play Paleo Pursuit. Fossil Fun - Skeleton Jigsaws : The aim of the game is to construct the skeleton of a beast, in ...
... why you believe those are the most reliable sites from a scientific point of view. Dig This! The Cretaceous Period Explore for fossils and uncrate the Cretaceous Period then move on to play Paleo Pursuit. Fossil Fun - Skeleton Jigsaws : The aim of the game is to construct the skeleton of a beast, in ...
Geography - Oxford University Press
... The heat inside the earth causes a lot of pressure. Because the plates are always moving, holes or cracks sometimes form in the crust. If there is a lot of pressure, the hot liquid magma will explode through the cracks. This explosion is called a volcanic eruption. When magma comes out of the earth, ...
... The heat inside the earth causes a lot of pressure. Because the plates are always moving, holes or cracks sometimes form in the crust. If there is a lot of pressure, the hot liquid magma will explode through the cracks. This explosion is called a volcanic eruption. When magma comes out of the earth, ...
Rubrics for Earth Stations
... You will be creating a model of Earth's interior. You may choose the material in which want to show the different layers of the earth. Your choices include construction paper, styrofoam sphere, paint, scissors, toothpicks, markers, &/or styrofoam pie shape. You may watch “Earth's Core” to gather inf ...
... You will be creating a model of Earth's interior. You may choose the material in which want to show the different layers of the earth. Your choices include construction paper, styrofoam sphere, paint, scissors, toothpicks, markers, &/or styrofoam pie shape. You may watch “Earth's Core” to gather inf ...
Answers for "175 Things to know for the 2016 midterm"
... 35. What is the formula for gradient? Find it in your ESRT page 1 36. What is another name for gradient? (hint: begins with s….) Slope 37. What is a contour line? Isoline that connects points of equal elevation 38. What is a contour interval? The interval between two adjacent contour lines on a map ...
... 35. What is the formula for gradient? Find it in your ESRT page 1 36. What is another name for gradient? (hint: begins with s….) Slope 37. What is a contour line? Isoline that connects points of equal elevation 38. What is a contour interval? The interval between two adjacent contour lines on a map ...
Midterm Review Questions - Red Hook Central Schools
... 35. What is the formula for gradient? Find it in your ESRT page 1 36. What is another name for gradient? (hint: begins with s….) Slope 37. What is a contour line? Isoline that connects points of equal elevation 38. What is a contour interval? The interval between two adjacent contour lines on a map ...
... 35. What is the formula for gradient? Find it in your ESRT page 1 36. What is another name for gradient? (hint: begins with s….) Slope 37. What is a contour line? Isoline that connects points of equal elevation 38. What is a contour interval? The interval between two adjacent contour lines on a map ...
Plate Tectonics, Earthquakes, and Volcanoes Study Guide
... Many expressed skepticism because the theory did not explain what force was strong enough to move continents. Later, scientists investigating the ocean floor found evidence that explained how continents were able to move. Plate tectonics, which grew from the theory of continental drift, now explains ...
... Many expressed skepticism because the theory did not explain what force was strong enough to move continents. Later, scientists investigating the ocean floor found evidence that explained how continents were able to move. Plate tectonics, which grew from the theory of continental drift, now explains ...
Structure of the Earth
... • 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 will not cover the geophysics of s ...
... • 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 will not cover the geophysics of s ...
Edible Tectonics
... the lithosphere where the plates are moving apart, as in the Mid-Ocean Ridge system or rift valleys like the one running through eastern Africa. As the plates separate, pressure on the mantle directly below decreases. The decrease in pressure causes the temperature in that portion of the mantle to r ...
... the lithosphere where the plates are moving apart, as in the Mid-Ocean Ridge system or rift valleys like the one running through eastern Africa. As the plates separate, pressure on the mantle directly below decreases. The decrease in pressure causes the temperature in that portion of the mantle to r ...
The structure of the earth and plate tectonics powerpoint[1].
... • Transform plate boundaries (moving over/under each other) • Name 3 plate tectonics. • If pressure builds up at plate boundaries and is released, what can happen? • What plate is Scotland on? ...
... • Transform plate boundaries (moving over/under each other) • Name 3 plate tectonics. • If pressure builds up at plate boundaries and is released, what can happen? • What plate is Scotland on? ...
File
... moon does not have plate tectonics!) • The moon is more eggshaped than round. (This might mean the moon was moving rapidly when it cooled off.) ...
... moon does not have plate tectonics!) • The moon is more eggshaped than round. (This might mean the moon was moving rapidly when it cooled off.) ...
Earth Science with Mr. Lanik Study Guide for Semester 2 Final Exam
... found today in Maine. State when this event happened, and which plate movements caused the rock to form. ...
... found today in Maine. State when this event happened, and which plate movements caused the rock to form. ...
File
... Type and geographic distribution of organisms changed through time. Some species indicate specific conditions. Sudden catastrophic changes in record indicate catastrophic events * THE HADEAN EAON Hell-like (Hadean): Moon (4.6 – 3.8Ga) Earth formed 4.57 GA based on radiometric analysis of planetesima ...
... Type and geographic distribution of organisms changed through time. Some species indicate specific conditions. Sudden catastrophic changes in record indicate catastrophic events * THE HADEAN EAON Hell-like (Hadean): Moon (4.6 – 3.8Ga) Earth formed 4.57 GA based on radiometric analysis of planetesima ...
Theory of plate tectonics - 8th Grade Social Studies
... Wegener was intrigued by the fossil species and unusual geologic structures found in both S. America and Africa Further evidence existed in the discovery of glacial deposits in Africa and tropical plant fossils in Antarctica At the time, Wegener could not explain what force would be strong enough to ...
... Wegener was intrigued by the fossil species and unusual geologic structures found in both S. America and Africa Further evidence existed in the discovery of glacial deposits in Africa and tropical plant fossils in Antarctica At the time, Wegener could not explain what force would be strong enough to ...
Classroom Space Volcano!
... The lava flows are relatively young and continued to flow long after the periods of heavy bombardment (after 3.5 billion years ago), therefore each new lava flow created new igneous rock and erased any surface features that previously existed. Again there will be some small craters on the lava flows ...
... The lava flows are relatively young and continued to flow long after the periods of heavy bombardment (after 3.5 billion years ago), therefore each new lava flow created new igneous rock and erased any surface features that previously existed. Again there will be some small craters on the lava flows ...
Earth`s Systems and Resources - Lexington County School District
... information about the relative position, density, and composition of Earth’s layers (crust, mantle and core). The primary focus of assessment should be for students to obtain and communicate information from a variety of sources (informational texts, primary and secondary sources, models, seismic da ...
... information about the relative position, density, and composition of Earth’s layers (crust, mantle and core). The primary focus of assessment should be for students to obtain and communicate information from a variety of sources (informational texts, primary and secondary sources, models, seismic da ...
Volcanoes Magma and Igneous Rocks Earthquakes notes sheet
... Pressure- because pressure increases with depth, it takes rocks longer to melt—they need higher temperatures to melt. Water- if a rock has water in it, it will melt at lower temperatures ...
... Pressure- because pressure increases with depth, it takes rocks longer to melt—they need higher temperatures to melt. Water- if a rock has water in it, it will melt at lower temperatures ...
Seismic Waves - Fort Thomas Independent Schools
... 4. If one string is thicker than the other at the same tension, what happens to the pitch 5. If two bottles have water in them, one more than the other, which will produce a higher pitch when someone blows over the opening? 6. If one chime is longer than another, which will produce the higher pitch. ...
... 4. If one string is thicker than the other at the same tension, what happens to the pitch 5. If two bottles have water in them, one more than the other, which will produce a higher pitch when someone blows over the opening? 6. If one chime is longer than another, which will produce the higher pitch. ...
Age of the Earth
The age of the Earth is 4.54 ± 0.05 billion years (4.54 × 109 years ± 1%). This age is based on evidence from radiometric age dating of meteorite material and is consistent with the radiometric ages of the oldest-known terrestrial and lunar samples.Following the development of radiometric age dating in the early 20th century, measurements of lead in uranium-rich minerals showed that some were in excess of a billion years old.The oldest such minerals analyzed to date—small crystals of zircon from the Jack Hills of Western Australia—are at least 4.404 billion years old. Comparing the mass and luminosity of the Sun to those of other stars, it appears that the Solar System cannot be much older than those rocks. Calcium-aluminium-rich inclusions – the oldest known solid constituents within meteorites that are formed within the Solar System – are 4.567 billion years old, giving an age for the solar system and an upper limit for the age of Earth.It is hypothesised that the accretion of Earth began soon after the formation of the calcium-aluminium-rich inclusions and the meteorites. Because the exact amount of time this accretion process took is not yet known, and the predictions from different accretion models range from a few millions up to about 100 million years, the exact age of Earth is difficult to determine. It is also difficult to determine the exact age of the oldest rocks on Earth, exposed at the surface, as they are aggregates of minerals of possibly different ages.