Richter Scale - WordPress.com
... The location of the fault line and the two tectonic plates. Where the epicentre and focus of an earthquake are likely to occur. Show the pattern of the seismic waves caused by an earthquake. ...
... The location of the fault line and the two tectonic plates. Where the epicentre and focus of an earthquake are likely to occur. Show the pattern of the seismic waves caused by an earthquake. ...
What type of volcano?
... • S6CS1.b Understand that hypotheses are valuable if they lead to fruitful • investigations, even if the hypotheses turn out not to be completely accurate • descriptions. • S6CS3.d Draw conclusions based on analyzed data. • S6CS5.b Identify several different models (such as physical replicas, • pict ...
... • S6CS1.b Understand that hypotheses are valuable if they lead to fruitful • investigations, even if the hypotheses turn out not to be completely accurate • descriptions. • S6CS3.d Draw conclusions based on analyzed data. • S6CS5.b Identify several different models (such as physical replicas, • pict ...
crust - Edmodo
... F 6. The center of the Earth is made of molten rock. T 7. Most of the Earth’s heat is stored in the mantle. T 8. The outer core is liquid. ...
... F 6. The center of the Earth is made of molten rock. T 7. Most of the Earth’s heat is stored in the mantle. T 8. The outer core is liquid. ...
Explore 2: Shifting Plates and Wandering Poles
... Students will model magnetic reversal patterns and use paleomagnetic data to demonstrate plate motion. Background Some rocks are naturally magnetized. How? When igneous rocks cool down from the molten stage, or when sand grains gently settle down through water, the iron-rich molecules tend to align ...
... Students will model magnetic reversal patterns and use paleomagnetic data to demonstrate plate motion. Background Some rocks are naturally magnetized. How? When igneous rocks cool down from the molten stage, or when sand grains gently settle down through water, the iron-rich molecules tend to align ...
Earth as a System - Salem Community Schools
... matter and energy that flow though them. • Even though each system can be described separately, all systems are linked. A large and complex system, such as the Earth system, operates as a result of the combination of smaller, interrelated systems. ...
... matter and energy that flow though them. • Even though each system can be described separately, all systems are linked. A large and complex system, such as the Earth system, operates as a result of the combination of smaller, interrelated systems. ...
The Earth
... cause earthquakes, volcanoes, and tsunamis. – Steps to reach goal: • 1. What are tectonic plates? • 2. What are earthquakes, volcanoes, and tsunamis? • 3. Where are they located? • 4. Can this information help us figure out how tectonic plates cause earthquakes, volcanoes, and tsunamis? ...
... cause earthquakes, volcanoes, and tsunamis. – Steps to reach goal: • 1. What are tectonic plates? • 2. What are earthquakes, volcanoes, and tsunamis? • 3. Where are they located? • 4. Can this information help us figure out how tectonic plates cause earthquakes, volcanoes, and tsunamis? ...
07_LectureOutline
... earthquakes, volcanic activity, mountain ranges, and rifts • New crust formed at rifts shows evidence of magnetic field reversals • Earth’s magnetic field traps charged particles from solar wind ...
... earthquakes, volcanic activity, mountain ranges, and rifts • New crust formed at rifts shows evidence of magnetic field reversals • Earth’s magnetic field traps charged particles from solar wind ...
PLATE TECTONICS THEORY
... the lithosphere — is composed of several major plates and many minor plates that change shape and position. Over time, these tectonic plates move, interact with each other, and are responsible for the formation of ocean basins, mountain ranges, islands, volcanoes, and earthquakes. The theory of plat ...
... the lithosphere — is composed of several major plates and many minor plates that change shape and position. Over time, these tectonic plates move, interact with each other, and are responsible for the formation of ocean basins, mountain ranges, islands, volcanoes, and earthquakes. The theory of plat ...
Space Camp - Georgia Standards
... Gravitational force of the Sun keeps planets in orbit around the Sun and governs the rest of the motion in the solar system. The Moon orbits the Earth once in about 28 days, which changes the part of the Moon lighted by the Sun and how much of that part can be seen from the Earth—phases of the Moon. ...
... Gravitational force of the Sun keeps planets in orbit around the Sun and governs the rest of the motion in the solar system. The Moon orbits the Earth once in about 28 days, which changes the part of the Moon lighted by the Sun and how much of that part can be seen from the Earth—phases of the Moon. ...
here
... Plate tectonics cause earthquakes and volcanoes(38). The point where two plates meet is called a plate boundary(39). Earthquakes and volcanoes are most likely to occur either on or near plate boundaries(40). There are three types of boundaries that we can observe. These plate boundaries are: Diverg ...
... Plate tectonics cause earthquakes and volcanoes(38). The point where two plates meet is called a plate boundary(39). Earthquakes and volcanoes are most likely to occur either on or near plate boundaries(40). There are three types of boundaries that we can observe. These plate boundaries are: Diverg ...
The emergence of plate tectonics and the Kuhnian
... the continents and oceans were considered to be permanent, rigidly fixed and immobile. According to that view, vertical and not horizontal tectonic movements played the principal role in the development of the Earth’s crust. In a complex process of scientific activities, this model (or theory; both ...
... the continents and oceans were considered to be permanent, rigidly fixed and immobile. According to that view, vertical and not horizontal tectonic movements played the principal role in the development of the Earth’s crust. In a complex process of scientific activities, this model (or theory; both ...
Continental Drift - Ms. Mosley
... other scientists. These scientists used new technology to collect information. They measured the ocean floor, recorded earthquakes, and studied the Earth’s magnetic fields. They used the things they learned to form a theory on how continents could move. This new theory was called plate tectonics. Th ...
... other scientists. These scientists used new technology to collect information. They measured the ocean floor, recorded earthquakes, and studied the Earth’s magnetic fields. They used the things they learned to form a theory on how continents could move. This new theory was called plate tectonics. Th ...
Fact Sheet - SharpSchool
... The seismicity, seismic or seismic activity of an area refers to the frequency, type and size of earthquakes experienced over a period of time. Earthquakes are measured using observations from seismometers. Seismometers should be attached to bedrock (the solid rock that lies beneath the soil and loo ...
... The seismicity, seismic or seismic activity of an area refers to the frequency, type and size of earthquakes experienced over a period of time. Earthquakes are measured using observations from seismometers. Seismometers should be attached to bedrock (the solid rock that lies beneath the soil and loo ...
Earth and Space Science Semester 2 Exam Review Part 1
... Mid-ocean ridge -A low lying mountain range that occurs alongside a Divergent Plate Boundary. - Oceanic crust and Sea-Floor Spreading is produced on both sides of the boundary. - Iceland is located on both sides of the Mid-Atlantic Ridge. ...
... Mid-ocean ridge -A low lying mountain range that occurs alongside a Divergent Plate Boundary. - Oceanic crust and Sea-Floor Spreading is produced on both sides of the boundary. - Iceland is located on both sides of the Mid-Atlantic Ridge. ...
the thin and solid outermost layer of Earth above the mantle
... Please DO NOT write on Quiz! Bubble in the correct answer on your scantron. 1. Continental Drift is a. the hypothesis that a single large landmass broke up into smaller landmasses to form the continents, which then drifted to their present locations; the movement of continents b. the theory that exp ...
... Please DO NOT write on Quiz! Bubble in the correct answer on your scantron. 1. Continental Drift is a. the hypothesis that a single large landmass broke up into smaller landmasses to form the continents, which then drifted to their present locations; the movement of continents b. the theory that exp ...
Earth: An Ever changing planet
... history are broken into periods of time,just like a year is broken into months, weeks, days and hours • Earth’s history is broken into eons, eras, periods, and epochs ...
... history are broken into periods of time,just like a year is broken into months, weeks, days and hours • Earth’s history is broken into eons, eras, periods, and epochs ...
Earth: An Ever changing planet
... history are broken into periods of time,just like a year is broken into months, weeks, days and hours • Earth’s history is broken into eons, eras, periods, and epochs ...
... history are broken into periods of time,just like a year is broken into months, weeks, days and hours • Earth’s history is broken into eons, eras, periods, and epochs ...
Earth`s Plates, Part 2: Movement
... two models: divergent plate boundaries (where crystal plates are moving away from each other) and convergent plate boundaries (where crystal plates are moving toward each other). Students will build each model, draw their model and describe what occurs during each geologic activity. Students will co ...
... two models: divergent plate boundaries (where crystal plates are moving away from each other) and convergent plate boundaries (where crystal plates are moving toward each other). Students will build each model, draw their model and describe what occurs during each geologic activity. Students will co ...
Earth: An Ever changing planet
... • Great ice age – 30% earth covered in ice • Wooly mammoths & saber-tooth cat go extinct • homo habilis • Dec. 31st: 10PM – 11:48 PM ...
... • Great ice age – 30% earth covered in ice • Wooly mammoths & saber-tooth cat go extinct • homo habilis • Dec. 31st: 10PM – 11:48 PM ...
LAB COURSES: 253B/255B SPRING 2014
... to gather data. Attached to this syllabus is a schedule of the labs. The type of report will depend on which type of lab you are doing. A. Traditional Lab Data will be collected manually and shared by all the members of the group. Report format is as follows (follow Reports: the format of the sample ...
... to gather data. Attached to this syllabus is a schedule of the labs. The type of report will depend on which type of lab you are doing. A. Traditional Lab Data will be collected manually and shared by all the members of the group. Report format is as follows (follow Reports: the format of the sample ...
Example or Rigor
... 1. Standard: What is the essential standard to be learned? Describe in student-friendly vocabulary. 2. Example or Rigor: What does proficient student work look like? Provide an example or description. 3. Prior Skills Needed: What prior knowledge, skills, or vocabulary are needed for a student to mas ...
... 1. Standard: What is the essential standard to be learned? Describe in student-friendly vocabulary. 2. Example or Rigor: What does proficient student work look like? Provide an example or description. 3. Prior Skills Needed: What prior knowledge, skills, or vocabulary are needed for a student to mas ...
Geologic Time and the Fossil Record
... After rock erodes, it is deposited somewhere. Newer deposits are left above older ones, so by looking at how an area of rock is layered, one can determine their relative age. -This principle is called superposition, and it says that younger deposits of rock lay above older deposits. ...
... After rock erodes, it is deposited somewhere. Newer deposits are left above older ones, so by looking at how an area of rock is layered, one can determine their relative age. -This principle is called superposition, and it says that younger deposits of rock lay above older deposits. ...
History of geomagnetism
The history of geomagnetism is concerned with the history of the study of Earth's magnetic field. It encompasses the history of navigation using compasses, studies of the prehistoric magnetic field (archeomagnetism and paleomagnetism), and applications to plate tectonics.Magnetism has been known since prehistory, but knowledge of the Earth's field developed slowly. The horizontal direction of the Earth's field was first measured in the fourth century BC but the vertical direction was not measured until 1544 AD and the intensity was first measured in 1791. At first, compasses were thought to point towards locations in the heavens, then towards magnetic mountains. A modern experimental approach to understanding the Earth's field began with de Magnete, a book published by William Gilbert in 1600. His experiments with a magnetic model of the Earth convinced him that the Earth itself is a large magnet.