Plate Tectonics and the Earth's Interior

Total Page:16

File Type:pdf, Size:1020Kb

Plate Tectonics and the Earth's Interior PPllaattee TTeeccttoonniiccss aanndd tthhee EEaarrtthh’’ss IInntteerriioorr Chapter 5 Earth’’s Internal Structure Crust Mantle Core Crust Thin – ocean basins . ~ 3 miles – mountain ranges . ~ 30 miles Deepest hole drilled – About 7 miles . Russia Crust Constitutes less than 1% of Earth’’s total mass Average density – 2.8 g/cm3 Crust Crust ―floats‖ on mantle Continents stand higher – thick and less dense Oceanic crust – thin and more dense Oceanic Crust vs Continental Crust Continental crust made of sial – rocks containing silicon and aluminum – e.g., granite Oceanic crust made of sima – rocks containing silicon and magnesium – e.g., basalt Mohorovicic Discontinuity Boundary between the crust and the mantle – 1 to 2 km thick – seismic P-waves increase in velocity Mantle 1800 miles thick Density – 4.5 g/cm3 80% Earth’’s volume Mantle Mostly solid Denser silicates rich in Mg and Fe – olivine Lithosphere (Gk. stone shell) ~ 100 miles thick Crust + Upper mantle Asthenosphere (Gk. weak shell) Part of upper mantle Plastic layer – Completely liquid in places (magma) 18-60 miles thick Mesosphere (Gk. middle shell) Solid dense mantle below asthenosphere Core ~ 2000 miles thick Density – 3 11.0 g/cm Half the radius and one-third mass of Earth Outer Core Liquid molten iron, nickel, cobalt, sulfur, or silicon origin of Earth’’s magnetic field Inner Core Solid (near melting point or partly molten) Iron 8000° F 3 million atm PPllaattee TTeeccttoonniiccss Have the contiinents drifted? Have the continents drifted? Antonio Snider (1859) proposed the continents drifted – Creationist – Based his idea on Genesis 1:9-10 Genesis 1:9-10 9 And God said, Let the waters under the heaven be gathered together unto one place, and let the dry land appear: and it was so 10 And God called the dry land Earth; and the gathering together of the waters called he Seas: and God saw that it was good. Evidence? The fit of the continents (taking into account the continental shelves). Correlation of fossil types across ocean basins. A zebra-striped pattern of magnetic reversals parallel to mid-ocean floor rifts, in the volcanic rock formed along the rifts, implying seafloor spreading along the rifts. Seismic observations interpreted as slabs of former ocean floor now located inside the earth. Continental Drift Positional shifting of continents Alfred L. Wegner – German Geologist (1880-1930) Pangaea – ―all lands‖ – supercontinent Pangaea Plate Tectonic Theory The earth''s surface (lithosphere) consists of rigid plates, each moving relative to adjacent plates. Deformation occurs at the edges of the plates by three types of horizontal motion: – Divergence – plates moving apart – Convergence – plates compressing together or one sliding under the other (subduction) – Transform –plates sliding past each other along a fault line Earth’’s plates Theory of Plate Tectonics Movement of plates explains: – mountain formation – earthquakes – volcanoes Divergent Boundaries Occurs as the sea floor pulls apart at rifts or splits – Mid-Atlantic Ridge Convergent Boundaries Occurs when one plate slides under another (subduction) or two plates collide together – Pacific Plate beneath Japan – Cocos Plate beneath Central America – Indian-Australian plate colliding with Eurasian plate Three Types of Convergent Boundaries Ocean-ocean – two oceanic plates converge with one subducting under the other – Associated with island arcs (Aleutian Islands) Ocean-continent – oceanic pllate and continental plate collide with oceanic plate subducting under continental plate – trenches and volcanic mountain chains (Sierra Nevada mountain range) Continent-continent – two continental plates collide and ―buckle‖ – No subduction – Upfolded mountains (Appalachian Mountains and Himalayan Mountains) Transform Boundaries Occurs where one plate slides horizontally past another – San Andreas Fault (Pacific Plate slide against North American Plate) Mid-Atlantic Ridge 20,000 feet below surface ~38,000 miles of ridges around globe (oceanic ridge) divides Atlantic Ocean into two equal parts At sea level, forms Iceland Mid-Atlantic Ridge Rift (trough) in middle of crest – 20 miles wide Submarine earthquakes under crest Heat escaping rift Iceland ground cracks in Iceland are widening, often accompanied by volcanic activity – Between 1975 and 1984 there was a 23 feet separation Mid-Atlantic Ridge Satellite imagery Interpretation of Observations of Mid-Atlantic Ridge Magma rises up at the rift forming new oceaniic crust – ―Younger‖ crust is at ridge and ―older‖ crust away from ridge Rocks acquire magnetism as they cool – Records earth’’s magnetic field direction at time – Continuous seafloor spreading should have a smooth magnetic ―tape recording‖ of reversals Zebra stripe pattern Problems for ―Slow and Gradual Plate Tectonics‖ Zebra stripe pattern has been confirmed – Drilling in the basalt shows magnetic polarity changes in patches down the holes with no consistent pattern with depth. Indicates rapid formation of basalt—not slow and gradual formation Magnetic reversals in lava have been shown to occur rapidly Mid-Atlantic Ridge spreads about 2 inches per year IIss tthhee pprreesseenntt rreeaallllyy tthhee kkeeyy ttoo tthhee ppaasstt?? Catastrophic Plate Tectonics Pre-flood supercontinent and dense ocean floor rocks Cold dense ocean floor sinks into softer, less dense mantle – Edges sink faster due to friction and drag the rest of the floor with it in conveyor belt fashion Catastrophic Plate Tectonics Faster movement creates more friction and heat in the mantle, reducing its resistance, and making the mantle move faster – Runaway subduction Catastrophic Plate Tectonics Mantle material is displaced, causing large scale movement through entire mantle – Causes enough tension throughout earth to break up original single land mass Hot, mantle material rises up amid cracks and vaporizes some ocean water causing geysers (Gen 7:11; Gen 8:2) Steam condenses in atmosphere to cause global rain (Gen 7:11-12) Catastrophic Plate Tectonics Rapid subduction of the cooler pre-flood ocean floor into the mantle would have resulted in increased circulation of viscous fluid (note: plastic, not molten) rock within the mantle. accelerated convection in the core would cause rapid geomagnetiic reversals – these would be erratic and locally patchy, laterally and at depth, just as the data indicate Catastrophic Plate Tectonics Model provides mechanism for retreat of flood waters (Psalm 104:6-8) – Vertical earth movements at end of flood as opposed to horizontal movements at beginning Plate collisions would have pushed up mountains – Slow movement would not be forceful enough to push up Himalayans at Indian-Australian and Eurasian plates Psalm 104:6-8 6 You covered it with the deep as if it were a garment; the waters stood above the mountains. 7 At Your rebuke the waters fled; at the sound of Your thunder they hurried away - 8 mountains rose and valleys sank -to the place You established for them Final Summary The idea is quite new, and radical, and much work has yet to be done to flesh out the details. There may even be major modifications to the theory that increase its explanatory power, or future discoveries could cause the model to be abandoned. Such is the nature of scientific progress. Scientific models come and go, "But the word of the Lord endures forever" (1 Peter 1:25). Future Consequences predicted by Plate Tectonic Theory Portions of California will separate from the rest of North America The Italian ―boot‖ will disappear Australia will link to Asia Africa will separate from the Near East .
Recommended publications
  • A Continuous Plate-Tectonic Model Using Geophysical Data to Estimate
    GEOPHYSICAL JOURNAL INTERNATIONAL, 133, 379–389, 1998 1 A continuous plate-tectonic model using geophysical data to estimate plate margin widths, with a seismicity based example Caroline Dumoulin1, David Bercovici2, Pal˚ Wessel Department of Geology & Geophysics, School of Ocean and Earth Science and Technology, University of Hawaii, Honolulu, 96822, USA Summary A continuous kinematic model of present day plate motions is developed which 1) provides more realistic models of plate shapes than employed in the original work of Bercovici & Wessel [1994]; and 2) provides a means whereby geophysical data on intraplate deformation is used to estimate plate margin widths for all plates. A given plate’s shape function (which is unity within the plate, zero outside the plate) can be represented by analytic functions so long as the distance from a point inside the plate to the plate’s boundary can be expressed as a single valued function of azimuth (i.e., a single-valued polar function). To allow sufficient realism to the plate boundaries, without the excessive smoothing used by Bercovici and Wessel, the plates are divided along pseudoboundaries; the boundaries of plate sections are then simple enough to be modelled as single-valued polar functions. Moreover, the pseudoboundaries have little or no effect on the final results. The plate shape function for each plate also includes a plate margin function which can be constrained by geophysical data on intraplate deformation. We demonstrate how this margin function can be determined by using, as an example data set, the global seismicity distribution for shallow (depths less than 29km) earthquakes of magnitude greater than 4.
    [Show full text]
  • Experimental Early Crystallization of K-Feldspar in Granitic Systems. Implications on the Origin of Magmatic Fabrics in Granitic Rocks
    Geologica Acta, Vol.15, Nº 4, December 2017, 261-281 DOI: 10.1344/GeologicaActa2017.15.4.2 J. Díaz-Alvarado, 2017 CC BY-SA Experimental early crystallization of K-feldspar in granitic systems. Implications on the origin of magmatic fabrics in granitic rocks J. DÍAZ-ALVARADO1 1Departamento de Geología. Universidad de Atacama Copayapu 485, Copiapó, Chile. E-mail: [email protected] ABS TRACT One of the most outstanding characteristics of some granodioritic to granitic rocks is the presence of K-feldspar megacrysts. For instance, granodiorites and monzogranites of the Spanish Central System batholith present variable amounts of large (up to 10cm in length) euhedral K-feldspar crystals. The porphyritic textures, the euhedral shape, the alignment of plagioclase and biotite inclusions and the magmatic fabrics point to a magmatic origin for these megacrysts. This work presents a phase equilibria study in a high-K2O granodioritic system. A series of experiments were conducted with a granodioritic composition (GEMbiot) to study the crystallization sequence at the emplacement conditions in the Gredos massif, i.e. 4 H2O wt.% and 0.4GPa. Experimental results show that orthopiroxene is the liquidus phase at 1010ºC, which reacts with the H2O-rich melt to stabilize biotite between 980 and 940ºC. Plagioclase crystallizes at around 910ºC, and K-feldspar crystallizes in the matrix between 750 and 700ºC when the crystal fraction is around 0.5. However, at 850ºC, a pelite-doped experiment shows euhedral K-feldspar (≈5vol%) in both the reactive xenolith domain together with cordierite and the granodioritic domain, where the K2O wt.% rose from 4.5 in the normal experiment to 5.9 in the doped experiment.
    [Show full text]
  • Sterngeryatctnphys18.Pdf
    Tectonophysics 746 (2018) 173–198 Contents lists available at ScienceDirect Tectonophysics journal homepage: www.elsevier.com/locate/tecto Subduction initiation in nature and models: A review T ⁎ Robert J. Sterna, , Taras Geryab a Geosciences Dept., U Texas at Dallas, Richardson, TX 75080, USA b Institute of Geophysics, Dept. of Earth Sciences, ETH, Sonneggstrasse 5, 8092 Zurich, Switzerland ARTICLE INFO ABSTRACT Keywords: How new subduction zones form is an emerging field of scientific research with important implications for our Plate tectonics understanding of lithospheric strength, the driving force of plate tectonics, and Earth's tectonic history. We are Subduction making good progress towards understanding how new subduction zones form by combining field studies to Lithosphere identify candidates and reconstruct their timing and magmatic evolution and undertaking numerical modeling (informed by rheological constraints) to test hypotheses. Here, we review the state of the art by combining and comparing results coming from natural observations and numerical models of SI. Two modes of subduction initiation (SI) can be identified in both nature and models, spontaneous and induced. Induced SI occurs when pre-existing plate convergence causes a new subduction zone to form whereas spontaneous SI occurs without pre-existing plate motion when large lateral density contrasts occur across profound lithospheric weaknesses of various origin. We have good natural examples of 3 modes of subduction initiation, one type by induced nu- cleation of a subduction zone (polarity reversal) and two types of spontaneous nucleation of a subduction zone (transform collapse and plumehead margin collapse). In contrast, two proposed types of subduction initiation are not well supported by natural observations: (induced) transference and (spontaneous) passive margin collapse.
    [Show full text]
  • Environmental Geology Chapter 2 -‐ Plate Tectonics and Earth's Internal
    Environmental Geology Chapter 2 - Plate Tectonics and Earth’s Internal Structure • Earth’s internal structure - Earth’s layers are defined in two ways. 1. Layers defined By composition and density o Crust-Less dense rocks, similar to granite o Mantle-More dense rocks, similar to peridotite o Core-Very dense-mostly iron & nickel 2. Layers defined By physical properties (solid or liquid / weak or strong) o Lithosphere – (solid crust & upper rigid mantle) o Asthenosphere – “gooey”&hot - upper mantle o Mesosphere-solid & hotter-flows slowly over millions of years o Outer Core – a hot liquid-circulating o Inner Core – a solid-hottest of all-under great pressure • There are 2 types of crust ü Continental – typically thicker and less dense (aBout 2.8 g/cm3) ü Oceanic – typically thinner and denser (aBout 2.9 g/cm3) The Moho is a discontinuity that separates lighter crustal rocks from denser mantle below • How do we know the Earth is layered? That knowledge comes primarily through the study of seismology: Study of earthquakes and seismic waves. We look at the paths and speeds of seismic waves. Earth’s interior boundaries are defined by sudden changes in the speed of seismic waves. And, certain types of waves will not go through liquids (e.g. outer core). • The face of Earth - What we see (Observations) Earth’s surface consists of continents and oceans, including mountain belts and “stable” interiors of continents. Beneath the ocean, there are continental shelfs & slopes, deep sea basins, seamounts, deep trenches and high mountain ridges. We also know that Earth is dynamic and earthquakes and volcanoes are concentrated in certain zones.
    [Show full text]
  • Plate Tectonics and the Cycling of Earth Materials
    Plate Tectonics and the cycling of Earth materials Plate tectonics drives the rock cycle: the movement of rocks (and the minerals that comprise them, and the chemical elements that comprise them) from one reservoir to another Arrows are pathways, or fluxes, the I,M.S rocks are processes that “reservoirs” - places move material from one reservoir where material is temporarily stored to another We need to be able to identify these three types of rocks. Why? They convey information about the geologic history of a region. What types of environments are characterized by the processes that produce igneous rocks? What types of environments are preserved by the accumulation of sediment? What types of environments are characterized by the tremendous heat and pressure that produces metamorphic rocks? How the rock cycle integrates into plate tectonics. In order to understand the concept that plate tectonics drives the rock cycle, we need to understand what the theory of plate tectonics says about how the earth works The major plates in today’s Earth (there have been different plates in the Earth’s past!) What is a “plate”? The “plate” of plate tectonics is short for “lithospheric plate” - - the outermost shell of the Earth that behaves as a rigid substance. What does it mean to behave as a rigid substance? The lithosphere is ~150 km thick. It consists of the crust + the uppermost mantle. Below the lithosphere the asthenosphere behaves as a ductile layer: one that flows when stressed It means that when the substance undergoes stress, it breaks (a non-rigid, or ductile, substance flows when stressed; for example, ice flows; what we call a glacier) Since the plates are rigid, brittle 150km thick slabs of the earth, there is a lot of “action”at the edges where they abut other plates We recognize 3 types of plate boundaries, or edges.
    [Show full text]
  • Epidote-Bearing Calc-Alkalic Granitoids in Northeast Brazil
    Revista Brasileira de Geociências 20(1-4): 88-100, março/dezembro de 1990 EPIDOTE-BEARING CALC-ALKALIC GRANITOIDS IN NORTHEAST BRAZIL ALCIDES NÓBREGA SIAL* RESUMO GRANITÓIDES COM EPÍDOTO MAGMÁTICO NO NORDESTE DO BRASIL. Um grande número de granitóides cálcio-alcalinos com epidoto são encontrados no Domínio Estrutural Central (DEC) - que compreende três segmentos: Seridó, Cachoeirinha-Salgueiro e Riacho do Pontal - e em algu- mas outras localidades no Nordeste do Brasil. No cinturão Cachoerinha-Salgueiro (CCS), granodioritos e tonalitos com epidoto, meta a peraluminosos, intrudiram fllitos há cerca de 620 Ma, enquanto no Seridó, uma maior variedade de plutões com epfdoto fgneo intrudiu gnaisses Jucurutu ou xistos Seridó. Granodio- ritos com duas micas com (±) granada e epfdoto ígneo (?) intrudiram metassedimentos do Cinturão Riacho do Pontal. Epídoto magmático está também presente nos plutões trondhjemítícos e shoshonítícos - que in- trudiram, respectivamente, xistos Salgueiro e rochas de embasamento ao longo do limite sul do CCS - bem como em plutões no Complexo Surubim-Caroalina e nos cinturões Pajed-Paraíba e Sergipano. E encontra- do em quatro relações texturais, duas das quais indiscutivelmente magmáticas, e duas outras de reações sub- solidus. No CCS, granitóides com epfdoto solidificaram-se geralmente em torno de 6 kbar - 7 kbar, de acor- do com seus teores de Al na homblenda. Pressões mais baixas obtidas para encraves quartzo - dioríticos são devidas à perda de Al através de reação subsolidus com plagioclásio, produzindo epídoto granular. Diferem de granitóides mesozóicos similares na América do Norte porque, embora suas pressões de solidificação se- jam altas, eles intrudiram tanto metassedimentos da fácies xistos verdes como plutões paleozóicos na Argen- tina (Cadeias Pampeanas), Nova Inglaterra (área de Sherbrooke-Lewiston) e Nova Zelândia (Cadeia de Vi- tória).
    [Show full text]
  • Constitution of the Earth's Interior
    Component-I (A) - Personal Details Role Name Affiliation Principal Investigator Prof. Masood Ahsan Siddiqui Department of Geography ,Jamia Millia Islamia, New Delhi Paper Coordinator, if any Dr. Sayed Zaheen Alam, Dayal Singh Singh College, Delhi University Content Writer/Author (CW) Dr.Ramashray Prasad DrBhim Rao Ambedkar Associate Professor College (University of Delhi) Yamuna Vihar, Delhi Content Reviewer (CR) Dr. Sayed Zaheen Alam, Dayal Singh Singh College, Delhi University Language Editor (LE) Component-I (B) - Description of Module Items Description of Module Subject Name Geography Paper Name Geomorphology Module Name/Title CONSTITUTION OF THE EARTH’S INTERIOR Module Id GEO/13 Pre-requisites Objectives Keywords SIAl, SIMA, NIFE, Volcanicity, Seismology Introduction Learning Objectives Meaning of Composition and Structure Studying the Earth’s Interior a. Artificial Sources and b. Natural Sources a. Artificial Sources: Density Pressure and Temperature Density Pressure Temperature Relationships of Density, Pressure and Temperature with Depths in the Interior b. Natural Sources Volcanism and Seismology. Volcanicity Seismology Primary, Secondary and Surface waves Characteristics of Primary (P) waves: Characteristics of Secondary (S) waves: Characteristics of Surface (L) waves: Interpretation of Propagating Different Waves Seismology and Constitution of the Earth’s Interior Chemical Composition of the Earth SIAL: SIMA: NIFE Earth’s Internal Structure Crust Mantle Core Conclusions Multiple Choice Questions Answers of MCQs References Web Links ================== CONSTITUTION OF THE EARTH’S INTERIOR Introduction The interior of the earth is that portion which is, possibly, not reachable for us. The parts, from where the sample is not supposed to be taken in our hands, are difficult to understand very well directly.
    [Show full text]
  • Reading Notes on KKV Ch 2: the Interior of the Earth 2.1 EQ
    Reading notes on KKV Ch 2: The interior of the earth 2.1 EQ SEISMOLOGY seismic waves, their speed double couple model and focal mechanisms. elastic rebound theory --EXPLAIN how the fault plane and auxiliary plane are different than a fault plane and its conjugate seismic tomography - like medical xrays - an energy source, illuminates the volume, and detected on the other side. in medical you know the energy and the distance travelled - all delays and attenuation of energy arrival at the detector can be attributed to complex paths and rigidity of materials. in earth, beat down the uncertainties by using more and more earthquakes and more and more stations. tomography techniques typically use one type of wave at a time. For body waves (p and s) use travel time, better for deeper imaging of velocity structure. surface waves can be better for picking up anisotropy and shorter wavelength changes. Iterative - between velocity structure and raypath. this process improves earthquake location and magnitude estimation. 2.2 VELOCITY STRUCTURE OF THE EARTH Moho was discovered in 1909. Key observation was that at 200 km from epicenter, p-wave arrivals were before predicted because the crustal paths were at 5.6 km/s and the mantle speed was 7.9 km/s. calculated depth was 54 km. same pattern is found globally - strong velocity contrast from 5.5-6 to 8 km/s at depths of 20 (new cont or rift) -80 (Himalaya) km. mean 40 km. Made my own diagram - purple is direct wave. red is a path to a station near the epicenter pink is a path to a station farther from epicenter.
    [Show full text]
  • A Preserved Early Ediacaran Magmatic Arc at the Northernmost
    DOI: 10.1590/2317-4889201620160004 ARTICLE A preserved early Ediacaran magmatic arc at the northernmost portion of the Transversal Zone central subprovince of the Borborema Province, Northeastern South America Arco magmático eoediacarano na porção setentrional da Zona Transversal, sub-província central da Província Borborema, nordeste da América do Sul Benjamim Bley de Brito Neves1*, Edilton José dos Santos2, Reinhardt Adolfo Fuck3, Lauro César Montefalco Lira Santos4 ABSTRACT: Magmatic arcs are an essential part of crust-forming events RESUMO: O objetivo deste trabalho é introduzir o conceito de um in planet Earth evolution. The aim of this work was to describe an early arco magmático eoediacarano (ca. 635–580 Ma) na porção norte da Ediacaran magmatic arc (ca. 635-580 Ma) exposed in the northernmost zona transversal, subprovíncia central da Província Borborema. Nossas portion of the Transversal Zone, central subprovince of Borborema Pro- pesquisas foram beneficiadas pela preexistência de sínteses de diferentes vince, northeast Brazil. Our research took advantage of several syntheses by autores, incluindo teses e dissertações, sobre a zona transversal nos úl- different authors, including theses and dissertations, carried out on mag- timos 30 anos. O arco proposto está situado entre 35º15’W e 42º30’W matic rocks of the study area for the last 30 years. The ca. 750 km long and (extensão ca. 750 km) e 7º15’S e 8ºS (largura de até 140 km), segundo up to 140 km wide arc, trending ENE-WSW, is preserved to the south of trend geral NNE-SSW, ao sul do Lineamento Patos. Cerca de 90 stocks the Patos Lineament, between 35º15’ and 42º30’W and 7º15’ and 8ºS.
    [Show full text]
  • Seafloor Spreading and Plate Tectonics
    OCN 201: Seafloor Spreading and Plate Tectonics I Revival of Continental Drift Theory • Kiyoo Wadati (1935) speculated that earthquakes and volcanoes may be associated with continental drift. • Hugo Benioff (1940) plotted locations of deep earthquakes at edge of Pacific “Ring of Fire”. • Earthquakes are not randomly distributed but instead coincide with mid-ocean ridge system. • Evidence of polar wandering. Revival of Continental Drift Theory Wegener’s theory was revived in the 1950’s based on paleomagnetic evidence for “Polar Wandering”. Earth’s Magnetic Field Earth’s magnetic field simulates a bar magnet, but it is caused by A bar magnet with Fe filings convection of liquid Fe in Earth’s aligning along the “lines” of the outer core: the Geodynamo. magnetic field A moving electrical conductor induces a magnetic field. Earth’s magnetic field is toroidal, or “donut-shaped”. A freely moving magnet lies horizontal at the equator, vertical at the poles, and points toward the “North” pole. Paleomagnetism in Rocks • Magnetic minerals (e.g. Magnetite, Fe3 O4 ) in rocks align with Earth’s magnetic field when rocks solidify. • Magnetic alignment is “frozen in” and retained if rock is not subsequently heated. • Can use paleomagnetism of ancient rocks to determine: --direction and polarity of magnetic field --paleolatitude of rock --apparent position of N and S magnetic poles. Apparent Polar Wander Paths • Geomagnetic poles 200 had apparently 200 100 “wandered” 100 systematically with time. • Rocks from different continents gave different paths! Divergence increased with age of rocks. 200 100 Apparent Polar Wander Paths 200 200 100 100 Magnetic poles have never been more the 20o from geographic poles of rotation; rest of apparent wander results from motion of continents! For a magnetic compass, the red end of the needle points to: A.
    [Show full text]
  • Plate Tectonics
    Plate tectonics tive motion determines the type of boundary; convergent, divergent, or transform. Earthquakes, volcanic activity, mountain-building, and oceanic trench formation occur along these plate boundaries. The lateral relative move- ment of the plates typically varies from zero to 100 mm annually.[2] Tectonic plates are composed of oceanic lithosphere and thicker continental lithosphere, each topped by its own kind of crust. Along convergent boundaries, subduction carries plates into the mantle; the material lost is roughly balanced by the formation of new (oceanic) crust along divergent margins by seafloor spreading. In this way, the total surface of the globe remains the same. This predic- The tectonic plates of the world were mapped in the second half of the 20th century. tion of plate tectonics is also referred to as the conveyor belt principle. Earlier theories (that still have some sup- porters) propose gradual shrinking (contraction) or grad- ual expansion of the globe.[3] Tectonic plates are able to move because the Earth’s lithosphere has greater strength than the underlying asthenosphere. Lateral density variations in the mantle result in convection. Plate movement is thought to be driven by a combination of the motion of the seafloor away from the spreading ridge (due to variations in topog- raphy and density of the crust, which result in differences in gravitational forces) and drag, with downward suction, at the subduction zones. Another explanation lies in the different forces generated by the rotation of the globe and the tidal forces of the Sun and Moon. The relative im- portance of each of these factors and their relationship to each other is unclear, and still the subject of much debate.
    [Show full text]
  • STRUCTURE of the EARTH Module-2/3
    STRUCTURE OF THE EARTH Module-2/3 On the basis of data assembled from studies of the travel habits of earthquake waves the earth has been divided into three major zones. (i) Crust (ii) Mantle (iii) Core The Crust The outermost thin layer of the lithosphere is crust. Its thickness varies from 16 to 40 km.The crust contain the continental landmass and the ocean basins. In the continental areas, crust is about 40 km thick and in the ocean basin, the thickness of the crust is 5 to 10km.From seismic waves it seems that the surface layer of the continent is composed mainly of granite rocks with specific gravity 2.65 where the seismic velocity is 6km/sec.Because these rocks contain a large proportion of silica and aluminum they are collectively called SIAL. The basement layer is continuous which is exposed on the ocean floor or the ocean basin. The specific gravity is 3.0 and the earthquake waves travel at a speed of 6.7km/sec. The rocks contain silica and minerals rich in magnesium and iron. This layer of basic rocks is termed as SIMA. The Mantle Below the earth’s crust is the second zone, themantle, having mean density of 4.6 gcm-3extends to a depth of approximately 2900km, into the interior of the earth. The line of function between the earth crust and the mantle is called Moho discontinuity after the scientist Mohorovicic who discovered it in 1909.Moho discontinuity lying at a depth of up to 40kms beneath the continents and 6-10 km beneath the ocean floor.
    [Show full text]