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Although the Earth might seem stable, it is in constant motion, which
Although the Earth might seem stable, it is in constant motion, which

SAC: Solution to a scientific or technological problem
SAC: Solution to a scientific or technological problem

... Communication and expression of science ideas - terminology Communication and expression of science ideas - clarity and referencing AOS 2: How are fields used to move electrical energy SAC: Optimising magnetic field design Description: Modern flexible fridge magnets are made from magnetic materials ...
the earth`s spheres
the earth`s spheres

... (about 30 mi) above sea level, is about the same as the temperature at the surface of Earth. The layer from 50 to 90 km (30 to 55 mi), called the mesosphere, is characterized by a marked decrease in temperature as the altitude increases. 6. The Exo- or Celestial Sphere (outside or heavenly sphere) i ...
restless continents text
restless continents text

... When Wegener put forth his hypothesis of continental drift, many scientists would not accept his hypothesis. From the calculated strength of the rocks, it did not seem possible for the crust to move in this way. During Wegener’s life, no one knew the answer. It wasn’t until many years later that evi ...
Midterm review
Midterm review

... 6. The unit for measuring length is 7. The unit of measurement for measuring the surface area of an object is 8. The tool you would use to measure the length of a piece of string is 9. The tool you would use to determine the surface area of an object is ...
Origin of Earth/ Hadean Eon
Origin of Earth/ Hadean Eon

... ...
Homework #1
Homework #1

... the size of the Earth. He made a very simple model for this that involved the following assumptions: 1. The Earth is a sphere. 2. The Sun is very far away. Eratosthenes knew that at noon on June 21 (the summer solstice - longest day), the Sun would shine into the bottom of a deep vertical pit in the ...
Physical Science
Physical Science

... Magnet – an object that attracts certain materials (iron or steel) Magnetic poles – ends of a magnet (north- or southseeking pole) Magnetic field – space all around a magnet where the force of the magnet can act (strongest at the poles) – North and south poles attract (field strongest #15) – North-n ...
Revolution VS Rotation
Revolution VS Rotation

... • Rotation - The Earth spinning on its own axis • Rotation speed- 24,855 miles/24hr or 1,038 miles/hr ...
Part I (50 points)
Part I (50 points)

... the uniformly magnetized sphere (r0
Dynamic Planet Review
Dynamic Planet Review

... • The ocean floor is subducting into the mantle. • We are losing Pacific ocean floor. ...
Alfred Lothar Wegener, 1880-1930
Alfred Lothar Wegener, 1880-1930

... In the late 1950's, scientists mapped the present-day magnetic field generated by rocks on the floor of the Pacific Ocean. The volcanic rocks which make up the sea floor have magnetization because, as they cool, magnetic minerals within the rock align to the Earth's magnetic field. They found positi ...
Earth`s Interior Section 1
Earth`s Interior Section 1

...  Wegener thought that this supercontinent had broken apart and that the pieces had slowly moved to become the continents as they are today.  Wegener’s idea that the continents slowly moved over Earth’s surface became known as continental drift. ...
Ferromagnetic Materials : Curie
Ferromagnetic Materials : Curie

... ordering of the magnetic moments. The susceptibility of a material, χ, indicates how dramatically a material responds to an applied magnetic field, and is defined as the ratio of the magnetisation of the material, M, and the applied magnetic field, H. Equation 1 The magnetisation of a material, M, i ...
The Structure of the Magnetosphere
The Structure of the Magnetosphere

The Earth`s Magnetic north pole is in the North
The Earth`s Magnetic north pole is in the North

... The Earth’s Magnetic north pole is in the North Pole First, let’s make the distinction between North Pole (capital N and capital P) and magnetic north pole (lower case n and lower case p). North Pole with capitals is a location on Earth where Santa Clause is supposed to live and we often call it the ...
Slide 1
Slide 1

... – Directional quantization • HOW? – A beam of potassium atoms is deflected in a non-uniform magnetic field because of the magnetic moment of the atoms. – Magnitude and direction of the magnetic moment of the atoms are obtained by measuring the density of the beam. • WHY? – Electron spin and magnetic ...
Electromagnetism
Electromagnetism

... connected from the positive end to the negative end, the electrons will flow from the negative end to the positive end to balance the valence and drain the battery quickly. The wire will also produce a small magnetic field. The magnetic field runs perpendicular to the wire in a circular motion. By c ...
Earth Science - Canajoharie Central Schools
Earth Science - Canajoharie Central Schools

... plays in all of these processes. It is an objective of this course to provide students with a clear understanding of the dynamic nature of the Earth and its natural constructive and destructive processes so that they may better understand their environment, and be able to make informed and educated ...
Power Point format
Power Point format

... understanding of planet Earth • GEO=earth OLOGY = study of • Physical geology - examines the materials composing Earth and seeks to understand the many processes that operate beneath and upon its surface • Historical geology - seeks an understanding of the origin of Earth and its development through ...
Colorado State Science Content Standards
Colorado State Science Content Standards

... Earth and Space Science: Students know and understand the processes and interactions of Earth's systems and the structure and dynamics of Earth and other objects in space. (Focus: Geology, Meteorology, Astronomy, Oceanography) GRADES 9-12 In grades 9-12, students know and can demonstrate understandi ...
Chapter 29A Worksheet - Rose
Chapter 29A Worksheet - Rose

... able to slide with negligible friction on the conductor. The apparatus is in a uniform magnetic field of 0.800 T, perpendicular to the plane of the figure. (A) Find the magnitude of the emf induced in the rod when it is moving toward the right with a speed of 7.50 m/s. (B) In what direction does the ...
Electron Spin Resonance (ESR) Spectroscopy (Electron
Electron Spin Resonance (ESR) Spectroscopy (Electron

... g-values are determined by careful measurement of the frequency and magnetic field, or more commonly by using a reference of known g-value. A very common reference is the stable free radical diphenylpicrylhydrazyl (C6H5)2NN(&){C6H2(NO2)3} for which g = 2.0036 In liquid samples the average (isotropic ...
ISNS3371_041907_bw
ISNS3371_041907_bw

... The electron spins on its axis, giving rise to a electron current in the direction of rotation. The electron is like a magnetic dipole, a miniature magnet, with a north end and a south end. In most substances, electrons spin in random directions - magnetic fields cancel. For iron and other magnetic ...
Earth as a System Chapter 2.1 Earth: A Unique Planet Earth Basics
Earth as a System Chapter 2.1 Earth: A Unique Planet Earth Basics

... the solid, plastic layer of the mantle beneath the lithosphere; made of mantle rock that flows very slowly, which allows tectonic plates to move on top of it ...
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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.
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