Regions Bank Former Employee W2, Tuscany Sinks Dxf, Articles A

Or does it have something. Third, as mentioned before, the continents look as if they are puzzle pieces that fit together. Society for Science & the Public 20002023. A new volcano is forming today on the ocean floor south of the island of Hawaii. The evidence for Plate Tectonics is very conclusive. Accessibility StatementFor more information contact us atinfo@libretexts.orgor check out our status page at https://status.libretexts.org. Geophysical and electromagnetic theory provides clear and convincing evidence of multiple polar reversals or polar flips throughout the course of Earth's history. Another line of evidence in support of plate tectonics came from the long-known existence of ophiolte suites (slivers of oceanic floor with fossils) found in upper levels of mountain chains. As methods of dating improved, one of the most conclusive lines of evidence in support of plate tectonics derived from the dating of rock samples. This website helped me pass! They initially assumed that this meant that Earths magnetic field had, over time, departed significantly from its present position, which is close to the rotational pole. Scientists studying the sea floor found stretches of magnetic material that were oriented south instead of north. have gotten under way as early as 3.2 billion years ago, about 400 million Some researchers have NW-SE stretching orientation . Why are ice cores important to geologic history? Igneous rocks are found on the earth's mantle. The Internal Layers & Structure of the Earth, Natural Disasters Caused By Tectonic Plates | Earthquakes, Volcanoes & Tsunamis. What is the Ring of Fire, and where is it? You go a little bit older, and right now we think it's about 780,000 years ago roughly. Earthquake experts recognized an interesting pattern of earthquake distribution. Different materials transmit and reflect seismic shock waves in different ways, and of particular importance to theory of plate tectonics is the fact that liquid does not transmit a particular form of seismic wave known as an S wave. Tremendously persuasive evidence of plate tectonics is also derived from correlation of studies of the magnetic orientation of the rocks to known changes in Earth's magnetic field as predicted by electromagnetic theory. latitude of about 45, Imagine the world fast-forwarding a few thousand or even a few million years, and you'll see the continents have moved. of crust subducted. These studies revealed the prominent undersea ridges with undersea rift valleys that ultimately were understood to be divergent plate boundaries. Paleomagnetic evidence, both reversals and polar wandering data, was instrumental in verifying the theories of continental drift and plate tectonics in the 1960s and 1970s. Second, fossils of the same organism are found on different continents, which points to the possibility that the continents were once connected as one giant continent called. When a magnetic reversal occurs, new ocean crust faithfully records it as a reversed magnetic "stripe" on both sides of the MOR. It helped me pass my exam and the test questions are very similar to the practice quizzes on Study.com. Why does the seafloor spread when it meets continental crust? Only 5 percent of all rocks on Earth are older than 2.5 billion years old, and no rock is older than about 4 billion years. Third, the continental shapes themselves look as if they are puzzle pieces that fit together. minerals that can act as tiny signposts pointing the way toward Earths The Pacific plate is moving north over a stationary lava source in the mantle, known as a hot spot. Why do tectonic plates float on the mantle? modern plate tectonics, says Michael Brown, These data have led some to speculate that a magnetic reversal may be imminent. However, it later became clear that slivers of continental crust adjacent to the deep-sea trench, as well as sediments deposited in the trench, may be dragged down the subduction zone. Modern understanding of the structure of Earth is derived in large part from the interpretation of seismic studies Plate Tectonics Basics. The Pandian deposit is a newly discovered contact metasomatic skarn magnetite deposit found in the Cainozoic super-thick overburden on the northwest margin of Luxi Uplift (LXU). The main features of plate tectonics are: A) The Earth's surface is covered by a series of crustal plates. New research, however, shows plate dynamics are driven significantly by the additional force of heat drawn from the Earth's core. At spreading rates of about 15 cm (6 inches) per year, the entire crust beneath the Pacific Ocean (about 15,000 km [9,300 miles] wide) could be produced in 100 million years. Irrespective of the exact mechanism, the geologic record indicates that the resistance to subduction is overcome eventually. stage for modern plate tectonics (SN: 6/5/19). Since then he's researched and written newspaper and magazine stories on city government, court cases, business, real estate and finance, the uses of new technologies and film history. Two plates carrying continental crust collide when the oceanic lithosphere between them has been eliminated. According to the theory of plate tectonics, the continents are moving because the plates the continents sit on are moving slowly over the molten mantle of the Earth. First, the age of the crust is youngest at the plate boundaries, where older rock is pushed up and the youngest rock stays on the bottom. Plate Tectonics Evidence: Model Plate Tectonics: research drilling beneath sea: layers of earth Density, Crust, . Why are sedimentary rocks important in paleontology? rocks. Rocks with a different orientation to the current orientation of the Earth's magnetic field also produce disturbances or unexpected readings (anomalies) when scientists attempt to measure the magnetic field over a particular area. 1 ). 1719 N Street, N.W., Washington, D.C. 20036, What the first look at the genetics of Chernobyls dogs revealed, Plant/animal hybrid proteins could help crops fend off diseases, Wildfires in boreal forests released a record amount of CO, The Yamnaya may have been the worlds earliest known horseback riders, Muons unveiled new details about a void in Egypts Great Pyramid, We Are Electric delivers the shocking story of bioelectricity, Many Antarctic glaciers are hemorrhaging ice. Active, modern-style plate Heres why that may be a problem, 50 years ago, Earths chances of contacting E.T. I would definitely recommend Study.com to my colleagues. high-resolution map of magnetic orientations within the rock. More importantly, dating studies show that the age of the rocks increases as their distance from the divergent boundary increases. It can be said that 70%. Why do lithospheric plates move constantly? For example, fossils of ''Cynognathus'' are found in South America, as well as in Africa. Scientists didn't just come up with this theory out of the blue, but after considering the pieces of evidence. copyright 2003-2023 Homework.Study.com. subduction to occur, in which one crustal plate dives beneath another. The progress of the Earth Sciences and the advancement of technologies associated with the understanding of our planet during the 1940s and 1950s have led geologists to develop a new way of looking at the world and how it works. This unit will be confined to considerations of internal energy release. Why are the largest waves found in the Southern Ocean? Because of the shape of the field lines, the magnetic force trends at different angles to the surface in different locations (red arrows of Figure \(\PageIndex{1}\)). succeed. Contemporary geologic thinking could not easily explain these topographic variations, or "oceanscapes." Tell us As it bends and sinks, the subducting lithosphere cracks extensively, triggering earthquakes in the . Surveys in the 1950s and 1960s provided an even more detailed picture of the ocean bottom. These age data also allow the rate of seafloor spreading to be determined, and they show that rates vary from about 0.1 cm (0.04 inch) per year to 17 cm (6.7 inches) per year. Pilbara Craton, an ancient bit of continent in Western Australia that includes Why are iron atoms so strongly affected by magnetic fields? (c) Continental-continental. Why do sediment deposits tend to form layers? 9.3 Earth's Magnetic Field Heat is also being transferred from the solid inner core to the liquid outer core, and this leads to convection of the liquid iron of the outer core. Those data suggest Plate Tectonics plate tectonics perron 12.001 overview: today: lecture: history of ideas about plate tectonics lab: scientific specialties day lecture: rates . Seafloor-spreading rates are much more rapid in the Pacific Ocean than in the Atlantic and Indian oceans. The causes of continental drift are perfectly explained by the plate tectonic theory. Modern continents hold clues to their distant past. After much debate, scientists concluded that new ocean crust must form at the MORs, recording the current magnetic orientation. Magnetism is part of the evidence for plate tectonic theory. Lava rises upwards from this hot spot to the surface and forms a volcano. considerably, from 2.5 centimeters per year to 0.37 centimeters per year, he Continental Drift Theory Overview & Evidence | What is Continental Drift? Stripes of magnetic material in the seafloor provide strong evidence for tectonic theory. The reason some crystals didn't orient to Earth's current magnetic field was that the continents containing the rocks had shifted position. As with continental drift theory two of the proofs of plate tectonics are based upon the geometric fit of the displaced continents and the similarity of rock ages and Paleozoic fossils in corresponding bands or zones in adjacent or corresponding geographic areas (e.g., between West Africa and the eastern coast of South America). Under these conditions the rocks recrystallize, or metamorphose, to form a suite of rocks known as blueschists, named for the diagnostic blue mineral called glaucophane, which is stable only at the high pressures and low temperatures found in subduction zones. rocks as old as 3.5 billion years. D. Magnetic striping occurs at subduction zones. See below Mountains by continental collision. The south pole? Freeman and Co. ; The Earth's Dynamic Systems by W. Kenneth Hamblin, 1975 by Burgess Publishing Co. ; Global Tectonics by Philip Kearey & Frederick J. Vine, 1996 by Blackwell Sciences Ltd. ; Physical Geology by Carla W. Montgomery, 1987 by Wm. Why is the lithosphere rigid and the asthenosphere plastic, even though they are both part of the mantle? Thats because researchers arent sure whether Earths magnetic poles Why is it important to identify planetary boundaries? When Alfred Wegener proposed the idea the continents could move, other scientists scoffed. And yes, this same theory of plate tectonics also explains why earthquakes typically happen along plate boundaries. A geologist armed with a magnetometer could sample down through the layers of solidified lava and thus track the direction and intensity of the field over the span of geologic time recorded by that volcano. . Plate tectonics -- the concept the continents are rock plates moving on the magma underneath -- is now accepted. The overriding plate scrapes sediments and elevated portions of ocean floor off the upper crust of the lower plate, creating a zone of highly deformed rocks within the trench that becomes attached, or accreted, to the overriding plate. That is, the ocean floor is oldest next to the continents and youngest near the center of ocean basins. Sediment eroded from Earths earliest continents may also have helped grease the wheels, setting the Where plates come into contact, energy is released. Accordingly, rocks of similar ages are found at similar distances from divergent boundaries, and the rocks near the divergent boundary where crust is being created are younger than the rocks more distant from the boundary. 60 seconds. During magnetic surveys of the deep ocean basins, geologists found areas where numerous magnetic reversals occur in the ocean crust. Subscribers, enter your e-mail address for full access to the Science News archives and digital editions. magnetic poles. conference. Because the mantle transmits S-waves, it was long thought to be a cooling solid mass. *"Physical Geology" by Steven Earle used under a CC-BY 4.0 international license. Scientists believe in the plate tectonics theory because of the following pieces of evidence. The first type of melting occurs at diverging plate boundaries (mid-ocean ridges; continental rift zones) and hotspots, where mantle beneath plates is hot but remains solid because it is under great pressure. The LibreTexts libraries arePowered by NICE CXone Expertand are supported by the Department of Education Open Textbook Pilot Project, the UC Davis Office of the Provost, the UC Davis Library, the California State University Affordable Learning Solutions Program, and Merlot. We can see evidence of magnetic polarity reversals by examining the geologic record. found, was on the move In the 1950s, geologists discovered magnetic minerals in older layers of volcanic rock oriented in the "wrong" direction. This chaotic mixture is known as an accretionary wedge. Magnetic patterns are important evidence for plate tectonics because we can use the magnetic signatures of rock to identify the movement of large Our experts can answer your tough homework and study questions. of crust moved in fits and starts as the planet began to cool after its formation (SN: Satellites have detected two areas in the mantle that appear to have reversed polarity. Why is convection important to plate tectonics? Subducting plates, where one tectonic plate is being driven under another, are associated with volcanoes and earthquakes. between 3.19 billion and 3.18 billion years ago. This page titled 4.2: Paleomagnetic Evidence for Plate Tectonics is shared under a CC BY 4.0 license and was authored, remixed, and/or curated by Paul Webb via source content that was edited to the style and standards of the LibreTexts platform; a detailed edit history is available upon request. We also acknowledge previous National Science Foundation support under grant numbers 1246120, 1525057, and 1413739. Subducting plates melt into the mantle, and diverging plates create new crust material. Why is geology important to the study of natural history? Either way, this bit Archean, plate tectonics occurred regionally: Plates could have been broken Electricity and Magnetism: What Are They & Why Are They Important? Paleomagnetic evidence for modern-like plate motion velocities at 3.2 Ga. Science Advances. The floating plates move incredibly slowly, but they do move, shifting the rocks they carry with them. surface many times over, leaving few outcrops that are older than 3 billion How Earth and other objects in the Solar System formed. Identical fossils are found in bands and zones equidistant from divergent boundaries. Reversals of the Earth's magnetic field means that rock erupted during such a period will show different magnetic directions than the older (and, we can ass. In 1969, geophysicist J. Tuzo Wilson compared the impact of this intellectual revolution in earth science to Einstein's general theory of relativity, which had produced a similar upending of. Why does Earth have plate tectonics and continents? They based their idea of continental drift on several lines of evidence: fit of the continents, paleoclimate indicators, truncated geologic features, and fossils. As upwelling of magma continues, the plates continue to diverge, a process known as seafloor spreading. Its like a teacher waved a magic wand and did the work for me. They found that rocks of different ages sampled from generally the same area showed quite different apparent magnetic pole positions (green line, Figure \(\PageIndex{2}\)). Your support enables us to keep our content free and accessible to the next generation of scientists and engineers. Why are trilobites important to oceanography? Get unlimited access to over 88,000 lessons. Sobolev has suggested previously that, for about a billion years during the Why are fossils never found in igneous rocks? Why is the continental crust thicker than the oceanic crust? that measure the reflection of seismic waves off features in Earth's interior. The curve defined by the paleomagnetic data was called a polar wandering path because Runcorn and his colleagues initially thought that their data represented actual movement of the magnetic poles (since geophysical models of the time suggested that the magnetic poles did not need to be aligned with the rotational poles). Spotting a Supercontinent: How Pangea Was Discovered. Given that Earth is constant in volume, the continuous formation of Earths new crust produces an excess that must be balanced by destruction of crust elsewhere. The tectonic plates are constantly in motion and new surfaces are always being created. answer choices. This pattern later served as evidence for the location of plate margins, that is, the zones of contact between different crustal plates. a rate of at least 2.5 centimeters per year. In his important 1960 publication, "History of Ocean Basins," geologist and U.S. Navy Admiral Harry Hess (19061969) provided the missing explanatory mechanism for plate tectonic theory by suggesting that the thermal convection currents in the athenosphere provided the driving force behind plate movements. Nineteenth century surveys of the oceans indicated that rather than being flat featureless plains, as was previously thought, some ocean areas are mountainous while others plummet to great depths. orienting themselves to align with either the north or south magnetic pole. Magnetic Patterns in Rock: Magnetic patterns refer to the pattern of magnetic orientation and magnetic signatures. similar proto-plate tectonics may have been to the modern process. Who first proposed the idea of plate tectonics? In the 1950's and 1960's scientists used the magnetic field-information stored in rocks to investigate the behavior of the geomagnetic field. (b) Oceanic-oceanic. | Earth's Crust Facts, Composition & Temperature. At greater depths the subducted plate is partially recycled into the mantle. How does plate tectonic work and what evidence supports this theory "Basic Principles of Plate Tectonic Summarized-The Earth's lithosphere is divided into plates that move relative to one another. 1.1: Earth's Internal Structure Earth has-a hot solid inner core of nearly pure metal;-a similarly hot but liquid . Why are most earthquakes and volcanoes at plate boundaries? They were able to determine that rocks from the same. Rearranging the continents based on their positions in Pangaea caused these wandering curves to overlap, showing that the continents had moved over time. bit of ancient continent to have traveled so far so quickly, he says, large-scale D) The source of heat driving the convection currents is . One of the key pieces of evidence supporting plate tectonic theory was the discovery that rocks on the seafloor record ancient reversals of the Earth's magnetic field: as rocks are formed where plates are moving away from one another, they record the current direction of the Earth's magnetic field, which flip-flops irregularly over very long The stripes alternate between those with magnetic material orientated toward magnetic north, and. Before the middle of the 20th century, most geoscientists maintained that continental crust was too buoyant to be subducted. This paleomagnetic work of the 1950s was the first new evidence in favor of continental drift, and it led a number of geologists to start thinking that the idea might have some merit. The rocks in the subduction zone experience high pressures but relatively low temperatures, an effect of the descent of the cold oceanic slab. Geologists were comfortable in accepting these magnetic anomalies located on the sea floor as evidence of sea floor spreading because they were able to correlate these anomalies with equidistant radially distributed magnetic anomalies associated with outflows of lava from land-based volcanoes. But as the magma cools and solidifies, movement ceases and the mineral orientation and position become fixed. Older magnetic reversals were likewise recorded; these stripes are now located farther from the MOR. called a quantum diamond microscope that can detect traces of magnetism at the Fig. Experiments show that the subducted oceanic lithosphere is denser than the surrounding mantle to a depth of at least 600 km (about 400 miles). Why are waves an important feature of the ocean surface? In its fluid form, the minerals that make up magma are free to move in any direction and take on any orientation. 1 ). In the 1950s, geologists discovered magnetic minerals in older layers of volcanic rock oriented in the "wrong" direction. Not all the crustal rock found on the Earth is the same age. Mountain Building Overview & Types | How are Mountains Formed? chemical reactions between once-buried rocks and the atmosphere that can A polarity reversal means that the magnetic North flips to where we know the South Pole is. . The theory of continental drift would become the spark that ignited a new way of viewing the Earth. This lesson provides a definition of plate tectonics, explains the theory of plate tectonics, and what phenomena in the natural world that the theory explains. There is variety of evidence that supports the claims that plate tectonics accounts for (1) the distribution of fossils on different continents, (2) the occurrence of earthquakes, and (3) continental and ocean floor features including mountains, volcanoes, faults, and trenches. tectonics, the researchers say. A much slower but certainly more spectacular proof of plate movement is exemplified by the still-ongoing formation of the Hawaiian Islands. What are the 3 main evidences for plate tectonics? Let's explore them now. Because the plates form an integrated system, it is not necessary that new crust formed at any given divergent boundary be completely compensated at the nearest subduction zone, as long as the total amount of crust generated equals that destroyed. Alfred Wegener and the concept of continental drift, Paleomagnetism, polar wandering, and continental drift, Gestation and birth of plate-tectonic theory, Plate-driving mechanisms and the role of the mantle, Dissenting opinions and unanswered questions, Interactions of tectonics with other systems. See the picture. lessons in math, English, science, history, and more. D) Thermal springs developing in stress fractures are depositing large volumes of material, increasing the height. After a few million years, that volcano becomes extinct as it moves north, away from the hot spot, and a new volcano begins to form to the south. Why is foliation only associated with regional metamorphism? apart by large meteorite impacts or powerful plumes rising from the mantle, These rocks can have magnetic properties that geologists study to record the history of the magnetic field. Martn et al., 2000). C. Brown . steps of drifting bits of continent. When surveys were run on the other side of the MORs, they showed that the magnetic reversal patterns were remarkably similar on both sides of the MORs. modern plate motions, the team reports April 22 in Science Advances. South America matches up with Africa. This gust of solar wind disturbs the outer part of the Earth's magnetic field, which undergoes a complex oscillation. That, in turn, suggests that the 4/9/12). The existence of ophiolte suites are consistent with the uplift of crust in collision zones predicted by plate tectonic theory. The measured strength of the magnetic field has dropped by 5-10% in the last 150 years, and less precise readings suggest it may have weakened by 25-50% over the last 5,000 years. As a member, you'll also get unlimited access to over 88,000 Continental bedrock is over a billion years old in many areas of the continents, with a maximum age of 3.6 billion years. Geologists considered whether the poles had created the effect by wandering, but that didn't fit the patterns. Geologists figured out that the differing orientations made sense if the continents weren't frozen in place. But Seafloor Spreading Theory Overview & Diagram | Who Discovered Seafloor Spreading? Plates sliding past each other cause friction and heat. A. Once formed, continental crust becomes a permanent part of Earth's surface. Why is oceanic lithosphere subducted but the continental lithosphere is not? Oil companies were soon using them aboard airplanes, mapping the weak magnetism of rocks to help locate oil deposits. Carolyn Gramling is the earth & climate writer. than around 2.8 billion years ago. Why is uniformitarianism important to historical geology? heat and pressure from which could have altered the minerals and reset their magnetic Magnetic storms have two basic causes: The Sun sometimes emits a strong surge of solar wind called a coronal mass ejection. Book: Introduction to Oceanography (Webb), { "4.01:_Alfred_Wegener_and_the_Theory_of_Plate_Tectonics" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "4.02:_Paleomagnetic_Evidence_for_Plate_Tectonics" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "4.03:_Mechanisms_for_Plate_Motion" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "4.04:_Plates_and_Plate_Motions" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "4.05:_Divergent_Plate_Boundaries" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "4.06:_Convergent_Plate_Boundaries" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "4.07:_Transform_Plate_Boundaries" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "4.08:_Earthquakes_and_Plate_Tectonics" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "4.09:_Seamounts_and_Hot_Spots" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "4.10:_Coral_Reefs" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "4.11:_Hydrothermal_Vents" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()" }, { "00:_Front_Matter" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "01:_Introduction_to_the_Oceans" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "02:_Getting_our_Bearings" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "03:_The_Origin_and_Structure_of_Earth" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "04:_Plate_Tectonics_and_Marine_Geology" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "05:_Chemical_Oceanography" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "06:_Physical_Oceanography" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "07:_Primary_Production" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "08:_Oceans_and_Climate" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "09:_Ocean_Circulation" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "10:_Waves" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "11:_Tides" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "12:_Ocean_Sediments" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "13:_Coastal_Oceanography" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "14:_Ice" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "zz:_Back_Matter" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()" }, 4.2: Paleomagnetic Evidence for Plate Tectonics, [ "article:topic", "showtoc:no", "license:ccby", "authorname:pwebb", "paleomagnetism", "polar wandering path", "licenseversion:40", "source@https://rwu.pressbooks.pub/webboceanography" ], https://geo.libretexts.org/@app/auth/3/login?returnto=https%3A%2F%2Fgeo.libretexts.org%2FBookshelves%2FOceanography%2FBook%253A_Introduction_to_Oceanography_(Webb)%2F04%253A_Plate_Tectonics_and_Marine_Geology%2F4.02%253A_Paleomagnetic_Evidence_for_Plate_Tectonics, \( \newcommand{\vecs}[1]{\overset { \scriptstyle \rightharpoonup} {\mathbf{#1}}}\) \( \newcommand{\vecd}[1]{\overset{-\!-\!\rightharpoonup}{\vphantom{a}\smash{#1}}} \)\(\newcommand{\id}{\mathrm{id}}\) \( \newcommand{\Span}{\mathrm{span}}\) \( \newcommand{\kernel}{\mathrm{null}\,}\) \( \newcommand{\range}{\mathrm{range}\,}\) \( \newcommand{\RealPart}{\mathrm{Re}}\) \( \newcommand{\ImaginaryPart}{\mathrm{Im}}\) \( \newcommand{\Argument}{\mathrm{Arg}}\) \( \newcommand{\norm}[1]{\| #1 \|}\) \( \newcommand{\inner}[2]{\langle #1, #2 \rangle}\) \( \newcommand{\Span}{\mathrm{span}}\) \(\newcommand{\id}{\mathrm{id}}\) \( \newcommand{\Span}{\mathrm{span}}\) \( \newcommand{\kernel}{\mathrm{null}\,}\) \( \newcommand{\range}{\mathrm{range}\,}\) \( \newcommand{\RealPart}{\mathrm{Re}}\) \( \newcommand{\ImaginaryPart}{\mathrm{Im}}\) \( \newcommand{\Argument}{\mathrm{Arg}}\) \( \newcommand{\norm}[1]{\| #1 \|}\) \( \newcommand{\inner}[2]{\langle #1, #2 \rangle}\) \( \newcommand{\Span}{\mathrm{span}}\)\(\newcommand{\AA}{\unicode[.8,0]{x212B}}\), 4.1: Alfred Wegener and the Theory of Plate Tectonics, http://upload.wikimedia.org/wikipedia/commons/, source@https://rwu.pressbooks.pub/webboceanography, status page at https://status.libretexts.org.