• Study Resource
  • Explore
    • Arts & Humanities
    • Business
    • Engineering & Technology
    • Foreign Language
    • History
    • Math
    • Science
    • Social Science

    Top subcategories

    • Advanced Math
    • Algebra
    • Basic Math
    • Calculus
    • Geometry
    • Linear Algebra
    • Pre-Algebra
    • Pre-Calculus
    • Statistics And Probability
    • Trigonometry
    • other →

    Top subcategories

    • Astronomy
    • Astrophysics
    • Biology
    • Chemistry
    • Earth Science
    • Environmental Science
    • Health Science
    • Physics
    • other →

    Top subcategories

    • Anthropology
    • Law
    • Political Science
    • Psychology
    • Sociology
    • other →

    Top subcategories

    • Accounting
    • Economics
    • Finance
    • Management
    • other →

    Top subcategories

    • Aerospace Engineering
    • Bioengineering
    • Chemical Engineering
    • Civil Engineering
    • Computer Science
    • Electrical Engineering
    • Industrial Engineering
    • Mechanical Engineering
    • Web Design
    • other →

    Top subcategories

    • Architecture
    • Communications
    • English
    • Gender Studies
    • Music
    • Performing Arts
    • Philosophy
    • Religious Studies
    • Writing
    • other →

    Top subcategories

    • Ancient History
    • European History
    • US History
    • World History
    • other →

    Top subcategories

    • Croatian
    • Czech
    • Finnish
    • Greek
    • Hindi
    • Japanese
    • Korean
    • Persian
    • Swedish
    • Turkish
    • other →
 
Profile Documents Logout
Upload
Hotspot Geodynamics Detailed Planning Group
Hotspot Geodynamics Detailed Planning Group

Earth Planet. Sci. Lett., 139, 1-16, 1996.
Earth Planet. Sci. Lett., 139, 1-16, 1996.

Deformation in the asthenospheric mantle beneath the Carpathian
Deformation in the asthenospheric mantle beneath the Carpathian

... 80∘ N display a nearly normal distribution around an average value of 120∘ N. The majority of the measurements fall into this distribution, in the range of 85∘ N to 145∘ N, while there are a number of good quality measures showing fast azimuths less than 80∘ N. To represent the individual measuremen ...
Workman, Hart, 2005 - University of Maryland, Department of Geology
Workman, Hart, 2005 - University of Maryland, Department of Geology

... We derive an estimate for the chemical composition of the depleted MORB mantle (DMM), the source reservoir to mid-ocean ridge basalts (MORBs), which represents at least 30% the mass of the whole silicate Earth. A database for the chemical and physical properties of abyssal peridotites has become rob ...
Hoffman2013_Cordille.. - Department of Earth Sciences
Hoffman2013_Cordille.. - Department of Earth Sciences

... McKenzie and Parker had reason to be cocky. Dan was of the opinion that seismic slip vectors, determined from earthquake first motions, would prove more useful in tectonics than principal stress axes, preferred by seismologists. He remembered Teddy Bullard’s explicit use of Euler’s theorem in an ico ...
Fluvial erosion
Fluvial erosion

... Provide shorter-lived radionuclides in local dust clouds ...
Exploring Earth: Plate Tectonics
Exploring Earth: Plate Tectonics

... by the National Science Education Standards). In Immersion Units, students learn academic content by working like scientists: making observations, asking questions, doing further investigations to explore and explain natural phenomena, and communicating results based on evidence. Immersion Units are ...
The Mantle and its Products
The Mantle and its Products

Linking collisional and accretionary orogens during Rodinia
Linking collisional and accretionary orogens during Rodinia

... suggests that breakup was initiated by a top-down process driven by accretionary tectonics along the periphery of the supercontinent. Plume-related magmatism may be present at specific times and in specific places during breakup but is not the prime driving force. Comparison of the Rodinia record of c ...
A relatively reduced Hadean continental crust and - HAL
A relatively reduced Hadean continental crust and - HAL

... (McCammon, 2005; Rohrbach et al., 2007). The atmosphere also experienced changes in fO2, being initially low, and rising markedly at ~2.3 Ga, during the so-called Great Oxidation Event (GOE) (Collerson and Kamber, 1999; Holland, 2002; Zahnle et al., 2010), progressively reaching its present oxidati ...
The Model of Oceanic Crust Expansion
The Model of Oceanic Crust Expansion

Intrinsic versus extrinsic seismic anisotropy: The radial anisotropy in
Intrinsic versus extrinsic seismic anisotropy: The radial anisotropy in

Directional Variations in Travel-Time Residuals of Teleseismic P
Directional Variations in Travel-Time Residuals of Teleseismic P

Seismic velocity structure and anisotropy of the Alaska subduction
Seismic velocity structure and anisotropy of the Alaska subduction

Linking Porphyry Deposit Geology to Geophysics via Physical
Linking Porphyry Deposit Geology to Geophysics via Physical

... This report summarizes the results of a study initiated to investigate physical rock properties of the hosting and mineralized rocks associated with the porphyry deposits targeted for geophysical surveys as part of the QUEST and QUEST-West projects. This research was conducted as part of a Geoscienc ...
The westward drift of the lithosphere
The westward drift of the lithosphere

... the basal décollements affect the entire crust and upper mantle, and the resulting belt has much larger volumes of rocks involved (Doglioni et al., 1999). This could explain why the topography of the east-directed subduction-related orogens is higher than the opposite subduction zones. In fact, when ...
Mechanical and thermal effects of floating continents on the global
Mechanical and thermal effects of floating continents on the global

Three distinct types of hotspots in the Earth`s mantle
Three distinct types of hotspots in the Earth`s mantle

Constraining the extent of crust–mantle coupling in central Asia
Constraining the extent of crust–mantle coupling in central Asia

Earth/Space Science Pretest 2014-2015 Multiple Choice Identify the
Earth/Space Science Pretest 2014-2015 Multiple Choice Identify the

... ____ 45. What force causes most of the erosion in desert areas? a. wind c. running water b. gravity d. ice ____ 46. Why can a heavy rain shower cause a large amount of erosion in a desert area? a. Temperatures are very high. b. Streams overflow easily. c. There is a lack of vegetation to hold the so ...
Geodynamics Workshop 2012 PROGRAM AND ABSTRACTS
Geodynamics Workshop 2012 PROGRAM AND ABSTRACTS

The thermochemical structure and evolution of Earth`s mantle
The thermochemical structure and evolution of Earth`s mantle

... 4. Modelling mantle thermochemical evolution Here, a new model is introduced that integrates geochemical tracking, mantle convection and self-consistently generated plate tectonics. This is an improvement on previous convection models with geochemical tracking both in the range of elements tracked a ...
Mantle plumes and dynamics of the Earth interior — towards a new
Mantle plumes and dynamics of the Earth interior — towards a new

... lherzolites = pyrolites) with 1 to 5% of intergranular melt. The lower boundary of LVZ (Lehmann discontinuity) is associated both with a waning of fluid fraction and with a considerable increase in the upper mantle viscosity. In the classical plate tectonic interpretations, LVZ was a “sliding layer” ...
Breast Mri
Breast Mri

... a combination of a large magnet radio waves and a, breast mri radiologyinfo org - what is mri of the breast magnetic resonance imaging mri is a noninvasive medical test that physicians use to diagnose and treat medical conditions, breast mri magnetic resonance imaging breastcancer org - mri or magne ...
Chemical composition of Earth`s primitive mantle and its variance: 2
Chemical composition of Earth`s primitive mantle and its variance: 2

< 1 2 3 4 5 6 7 ... 386 >

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.
  • studyres.com © 2025
  • DMCA
  • Privacy
  • Terms
  • Report