Menu Zamknij

how does glacial evidence support continental drift

The next section provides the pieces of evidence that helped transform one mans wild notion into a scientific theory. The fossils of these organisms are found on lands that are now far apart. So, the fact that these organisms could not swim through the vast water bodies helps to substantiate the fact that the continents were once together to allow distribution of these organisms in various continents where their fossils were found on. The map below (based on data in the Paleobiology Database) shows locations where these fossils have been found. 18. Identical rocks, of the same type and age, are found on both sides of the Atlantic Ocean. Scientists had long known of strange magnetic anomalies that formed a striped pattern of symmetrical rows on both sides of mid-oceanic ridges. glaciation (countable and uncountable, plural glaciations) The process of covering with a glacier, or the state of being glaciated; the production of glacial phenomena; an ice age quotations ], which resulted in massive deposits of glacier-scrubbed sediment, each likely caused a subsequent boost in the global rate of plate tectonics. Since these match up points consisted of the same kind of rock further proves that the continents were once together before breaking away and drifting. There was almost certainly only one north magnetic pole through Earth's history. The location of the north magnetic north pole 80 million years before present (mybp), then 60, 40, 20, and now. n@.#|?W h +{j.xy( [:@3{LgZao}4KW{.ettF!0G B^qxIl k#1FS7MRY4@3{#j9R]D%w3_:jM& Can you fit the pieces together? { "5.01:_Continental_Drift" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.02:_Wegener_and_the_Continental_Drift_Hypothesis" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.03:_Magnetic_Polarity_Evidence_for_Continental_Drift" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.04:_Bathymetric_Evidence_for_Seafloor_Spreading" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.05:_Magnetic_Evidence_for_Seafloor_Spreading" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.06:_Seafloor_Spreading_Hypothesis" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.07:_Plate_Tectonics-_Challenge_1" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.08:_Earth\'s_Tectonic_Plates" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.09:_Tectonic_Plate_Motions" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.10:_Theory_of_Plate_Tectonics" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.11:_Divergent_Plate_Boundaries_in_the_Ocean" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.12:_Divergent_Plate_Boundaries" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.13:_Transform_Plate_Boundaries" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.14:_Plate_Tectonics-_Challenge_2" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.15:_Ocean-Continent_Convergent_Plates" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.16:_Ocean-Ocean_Convergent_Plate_Boundaries" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.17:_Continent-Continent_Convergent_Plate_Boundaries" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.18:_Continental_Margins" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.19:_Supercontinent_Cycle_and_Pangaea" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.20:_Intraplate_Activity" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.21:_Plate_Tectonics-_Challenge_3" : "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:_The_Nature_of_Science" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "02:_Introduction_to_Earth_Science" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "03:_Planet_Earth" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "04:_Earth\'s_Minerals_and_Rocks" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "05:_Plate_Tectonics" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "06:_Geological_Activity_and_Earthquakes" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "07:_Geological_Activity_and_Volcanoes" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "08:_Earth\'s_Fresh_Water" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "09:_Earth\'s_Oceans" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "10:_Atmospheric_Processes" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "11:_Weather" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "12:_Climate" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "13:_Weathering_and_Soils" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "14:_Erosion_and_Deposition" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "15:_Understanding_Earth\'s_History" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "16:_Earth\'s_History" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "17:_Evolution_and_Populations" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "18:_Ecosystems" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "19:_History_of_Life_on_Earth" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "20:_Earth\'s_Energy" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "21:_Earth\'s_Materials" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "22:_The_Solar_System" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "23:_Beyond_the_Solar_System" : "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]()" }, 5.3: Magnetic Polarity Evidence for Continental Drift, [ "article:topic", "showtoc:no", "program:ck12", "authorname:ck12", "license:ck12", "source@https://flexbooks.ck12.org/cbook/ck-12-middle-school-earth-science-flexbook-2.0" ], https://k12.libretexts.org/@app/auth/3/login?returnto=https%3A%2F%2Fk12.libretexts.org%2FBookshelves%2FScience_and_Technology%2FEarth_Science%2F05%253A_Plate_Tectonics%2F5.03%253A_Magnetic_Polarity_Evidence_for_Continental_Drift, \( \newcommand{\vecs}[1]{\overset { \scriptstyle \rightharpoonup} {\mathbf{#1}}}\) \( \newcommand{\vecd}[1]{\overset{-\!-\!\rightharpoonup}{\vphantom{a}\smash{#1}}} \)\(\newcommand{\id}{\mathrm{id}}\) \( \newcommand{\Span}{\mathrm{span}}\) \( \newcommand{\kernel}{\mathrm{null}\,}\) \( \newcommand{\range}{\mathrm{range}\,}\) \( \newcommand{\RealPart}{\mathrm{Re}}\) \( \newcommand{\ImaginaryPart}{\mathrm{Im}}\) \( \newcommand{\Argument}{\mathrm{Arg}}\) \( \newcommand{\norm}[1]{\| #1 \|}\) \( \newcommand{\inner}[2]{\langle #1, #2 \rangle}\) \( \newcommand{\Span}{\mathrm{span}}\) \(\newcommand{\id}{\mathrm{id}}\) \( \newcommand{\Span}{\mathrm{span}}\) \( \newcommand{\kernel}{\mathrm{null}\,}\) \( \newcommand{\range}{\mathrm{range}\,}\) \( \newcommand{\RealPart}{\mathrm{Re}}\) \( \newcommand{\ImaginaryPart}{\mathrm{Im}}\) \( \newcommand{\Argument}{\mathrm{Arg}}\) \( \newcommand{\norm}[1]{\| #1 \|}\) \( \newcommand{\inner}[2]{\langle #1, #2 \rangle}\) \( \newcommand{\Span}{\mathrm{span}}\)\(\newcommand{\AA}{\unicode[.8,0]{x212B}}\), 5.2: Wegener and the Continental Drift Hypothesis, 5.4: Bathymetric Evidence for Seafloor Spreading, source@https://flexbooks.ck12.org/cbook/ck-12-middle-school-earth-science-flexbook-2.0, Magnetite crystals in fresh volcanic rocks point to the current magnetic north pole (. Legal. Figure 1. WebHow does glacial evidence support the theory of continental drift? Continental drift can be regarded as theory which gives explanation about the shifting and changing of position of continents on Earth's surface. 8. One of the most compelling lines of evidence in support of continental drift came from the fossil record. In particular, very similar types of fossils were Instead, a collision between two continental plates crunches and folds the rock at the boundary, lifting it up and leading to the formation of mountains and mountain ranges. Some of the fossil evidence discovered on the continents includes mesosaurus, lystosaurus, cygnognathus and glossopteris. Its fossils are found only in South Africa and South America. It makes a much-cooled rock layer that should be solidifying into the crust. The earths outer shell is composed of plates that move a little bit every year. dLhktZvGZh4#('U s` R08Y 3VPwR959DZeAm`lX%2+favLCC ZPDT!}S p?=++ G/Mfk[Xnx}2c @K8a=U7^. @a4KM `7&G`#U4M7*l The fact that the seeds would have been unable to be blown or floated to these continents proves that these continents were once together. Better yet, use a map where the edges of the continents show the continental shelf. Accessibility StatementFor more information contact us atinfo@libretexts.org. |.3)zgm&4"/w.j4X-R WebGlacial Deposits. This indicates that these continents had to be once joined together because the extensive oceans between these land masses act as a type of barrier for fossil transfer. How do glaciers support the theory of plate tectonics? Over the course of millions of year ago, this gradual movement caused the once combined supercontinent to separate into 7 continents you witness in the present day. The distribution of these reptiles in different continents proves that these separate land masses were once together before splitting. When an oceanic and a continental plate collide, eventually the oceanic plate is subducted under the continental plate due to the high density of the oceanic plate. The discovery of fossils on different continents indicated that the continents were once together before they drifted away. shows us glaciers once covered a large portion of the land in the southern hemisphere. Paleoclimatic Evidence of Continental Drift. Web8. Compaction in the Rock Cycle: Understanding the Process Behind Sedimentary Rock Formation, Crystallization in the Water Cycle: A Fundamental Process in Water Distribution and Purification, Understanding Crystallization in the Rock Cycle: A Fundamental Process in Rock Formation, Extracting Lat/Lng from Shapefile using OGR2OGR/GDAL. 3. How does the Mesosaurus fossil evidence support the continental drift theory? Salt evaporites/beds in cold parts of U.S.A, Britain, Germany and Russia is evidence for continental drift from tropics because salt evaporites occur in tropics Proximity of continental land masses to the North Pole than in South Pole. WebThe continental drift hypothesis was developed in the early part of the 20 th century, mostly by Alfred Wegener. Magnetite crystals in fresh volcanic rocks point to the current magnetic north pole (figure 5) no matter what continent or where on the continent the rocks are located. How did glacial deposits provide evidence that Pangaea had existed? Geological fit evidence is the matching of large-scale geological features on different continents. The classic example is the collision between the Indian plate and the Asia plate. Roaming the terrains during the Triassic period (250 to 240 million years ago), the Cynognathus was as large as a modern wolf. According to the Lystrosaurus and Cygnognathus body anatomy, they are not designed for swimming. Abstract. Mantovani, R. Les fractures de lcorce terrestre et la thorie de Laplace. ermine! While making this claim, he had a collection of evidence to support it. This would indicate that the glaciers either formed in the middle of the ocean and/or covered most of the Earth. The continental drift hypothesis was developed in the early part of the 20th century, mostly by Alfred Wegener. When two plates collide one gets down the other plate and due to immense heat and pressure of the earth the plate moving down melts away and thus eventually gets destroyed and comes out in the form of magma. Antonio Snider-Pellegrini did preliminary work on continental separation and matching fossils in 1858. Describe how magnetite indicates magnetic pole. This suggested that these continents were once together and drifted away over time. The Appalachians of the eastern United States and Canada, for example, are just like mountain ranges in eastern Greenland, Ireland, Great Britain, and Norway (figure 2). What geological process is not involved in continental continental convergence? Modern day representation of the Mesosaurus. Figure 6. As a land dominant species, the Cynognathus would not have been capable of migrating across the Atlantic. This is what they learned: Earths current north magnetic pole is in northern Canada. We also acknowledge previous National Science Foundation support under grant numbers 1246120, 1525057, and 1413739. We also acknowledge previous National Science Foundation support under grant numbers 1246120, 1525057, and 1413739. What happens when two continental plates move towards each other? The continents remained fixed and the north magnetic pole moved. Geologist tested the idea that the pole remained fixed but the continents moved. However, a land bridge is not applicable due to the differences in densities between the continents and oceans floor and violation of the isostasy concept. If the continents had remained fixed while the north magnetic pole moved, there must have been two separate north poles. what was Wegener's first observation that lead to his idea of continental drift? Grooves and rock deposits left by ancient glaciers are found today on different continents very close to the equator. Illustration showing similar rock assemblages across different continents. Salt evaporites/beds in cold parts of U.S.A, Britain, Germany and Russia is evidence for continental drift from tropics because salt evaporites occur in tropics 14. McKenzie, D. P. & Parker, R. L. The North Pacific: an Example of Tectonics on a Sphere. The four pieces of evidence for the continental drift include continents fitting together like a puzzle, scattering ancient fossils, rocks, mountain ranges, and the old climatic zones' locations. Fossils of remarkably similar plants and animals have been discovered on opposite sides of the Atlantic Ocean. Puzzling new evidence came in the 1950s from studies on the Earths magnetic history (figure 4). What are glacial striations and how are they used as evidence for continental drift? 2. Why does it sometimes point to a spot that is not where the pole is located? Similar to the land dwelling Cynognathus, the Lystrosaurus would have not had the swimming capability to traverse any ocean. Obviously, the continents did not appear to move, and changing the conservative minds of the scientific community would require exceptional evidence that supported a credible mechanism. In fact, the first hard evidence to support plate motion came from paleomagnetism. 13. If the continents havent moved, then this would suggest an ice sheet extended from the south pole to the equator at this time - which is unlikely as the UK at this time was also close to the equator and has extensive coal and limestone deposits. So, technically, the creature would not have traveled through the ocean to get to the next continent. In particular, very similar types of fossils were found in now far-flung regions of the world. because it is unlikely that the mesosaurus could swim between continents. the continents seem to fit together like puzzle pieces. Contact Us . Magnetic Polarity. Glossopteris was Fossil from fern. If you look at the map before the continents drifted away, you find that Cygnognathus was situated in South America and Africa. If you have ever been hiking or camping, you may have used a compass to help you find your way. Copyright 2023 ScienceAlert.quest | Powered by Astra WordPress Theme. Now, looking at the current map after drifting of the continents, Cygnognathus is situated in Africa and South America. Paleomagnetic rocks on different continents provide different apparent polar wander paths for each continent, which indicates that it is not the poles that are moving, but the continents. Using technology, scientists would find more evidence that continents had drifted. The north magnetic pole is very likely in the same spot it has always been. How does paleomagnetism serve as evidence for continental drift? "dog jaw" - A non swimming, land dwelling, mammal-like reptile found only in South Africa and South America. Empowering curious minds, one answer at a time. Alfred Wegener investigated this field and found an anomaly in the Permo This would tell them where magnetic north was at the time the rocks cooled. Why shouldnt we drink salt water? 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. And forms solidified outer layer of the earth called lithosphere. Laurasia, makes up the northern continents of today. The Lystrosaurus, which translates to shovel reptile, is thought to have been an herbivore with a stout build like a pig. There is also much climatic evidence supporting continental drift, most notably glacial activity. This evidence for continental drift gave geologists renewed interest in understanding how continents could move about on the planets surface. What happens when a continental plate and oceanic plate collide? Other pro-continental drift followers used expansion, contraction, or even the moons origin to explain how the continents moved. The Himalayas were born when the Indian subcontinent smashed into Asia 45 million years ago. This occurs at an ocean trench (Figure below). d-vh@K,duLeJwepJN.-n)t,=M[t80=*4)E.dTJPzSxBtshrZeU\kx4O9JkIjUjYy|sIsZox*c;i3yFu@ mKm?`RZ* KR\Iob-4.UNLKfxBlb5Y2ed=\fNEX0 c1q/OS/'^;;mE7 T.#A2?FZN9B"wRU@ \Lr=Fc /bz+L;1!JuJ+U@4}p. Remove unwanted regions from map data QGIS. The problem with this hypothesis is the improbability of a land bridge being tall and long enough to stretch across a broad, deep ocean. This page titled 2.1: Alfred Wegeners Continental Drift Hypothesis is shared under a CC BY-NC-SA license and was authored, remixed, and/or curated by Chris Johnson, Matthew D. Affolter, Paul Inkenbrandt, & Cam Mosher (OpenGeology) . As a result of movement of the supercontinent, Pangaea split into two super landmasses namely Laurasia and Gondwanaland. Glacier evidence was found in places glaciers should never have been. A magnetometer is a device capable of measuring the magnetic field. When two continental plates converge the result is the formation of large folded mountains. Paleomagnetism was the most convincing evidence set forth to support the concepts of continental drift and seafloor spreading. What mountains in Northwestern Europe match up with the Appalachian Mountains in Eastern North America? Alfred Wegener in Greenland. Possibly the most important fossil evidence found is the plant, Glossopteris. Several independent research groups recognized earthquake epicenters traced the shapes of oceanic plates sinking into the mantle. { "5.01:_Why_It_Matters" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.02:_Geological_Development" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.03:_Basics_of_Plate_Tectonics" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.04:_Continental_Drift" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.05:_Continental_Drift" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.06:_Theory_of_Plate_Tectonics" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.07:_Theory_of_Plate_Tectonics" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.08:_Plate_Tectonics" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.09:_Effects_of_Plate_Tectonics" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.10:_The_Ring_of_Fire" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.11:_Intraplate_Deformation" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.12:_Folds" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.13:_Climates_and_Tectonics" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.14:_Hot_Spots" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.15:_Intraplate_Activity" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.16:_Hot_Spots" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "5.17:_Putting_It_Together" : "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:_Science_of_Geology" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "02:_Rock_Forming_Minerals" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "03:_Rocks_and_the_Rock_Cycle" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "04:_Soil" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "05:_Plate_Tectonics" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "06:_Earth\'s_Interior" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "07:_Crustal_Deformation" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "08:_Earthquakes" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "09:_Volcanic_Activity" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "10:_Mass_Movement" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "11:_Hydrology" : "property get [Map MindTouch.Deki.Logic.ExtensionProcessorQueryProvider+<>c__DisplayClass228_0.b__1]()", "12:_Geological_Implications" : "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]()" }, [ "article:topic", "showtoc:no", "license:ccby", "licenseversion:40" ], https://geo.libretexts.org/@app/auth/3/login?returnto=https%3A%2F%2Fgeo.libretexts.org%2FBookshelves%2FGeology%2FFundamentals_of_Geology_(Schulte)%2F05%253A_Plate_Tectonics%2F5.05%253A_Continental_Drift, \( \newcommand{\vecs}[1]{\overset { \scriptstyle \rightharpoonup} {\mathbf{#1}}}\) \( \newcommand{\vecd}[1]{\overset{-\!-\!\rightharpoonup}{\vphantom{a}\smash{#1}}} \)\(\newcommand{\id}{\mathrm{id}}\) \( \newcommand{\Span}{\mathrm{span}}\) \( \newcommand{\kernel}{\mathrm{null}\,}\) \( \newcommand{\range}{\mathrm{range}\,}\) \( \newcommand{\RealPart}{\mathrm{Re}}\) \( \newcommand{\ImaginaryPart}{\mathrm{Im}}\) \( \newcommand{\Argument}{\mathrm{Arg}}\) \( \newcommand{\norm}[1]{\| #1 \|}\) \( \newcommand{\inner}[2]{\langle #1, #2 \rangle}\) \( \newcommand{\Span}{\mathrm{span}}\) \(\newcommand{\id}{\mathrm{id}}\) \( \newcommand{\Span}{\mathrm{span}}\) \( \newcommand{\kernel}{\mathrm{null}\,}\) \( \newcommand{\range}{\mathrm{range}\,}\) \( \newcommand{\RealPart}{\mathrm{Re}}\) \( \newcommand{\ImaginaryPart}{\mathrm{Im}}\) \( \newcommand{\Argument}{\mathrm{Arg}}\) \( \newcommand{\norm}[1]{\| #1 \|}\) \( \newcommand{\inner}[2]{\langle #1, #2 \rangle}\) \( \newcommand{\Span}{\mathrm{span}}\)\(\newcommand{\AA}{\unicode[.8,0]{x212B}}\), Original content from Kimberly Schulte (Columbia Basin College) and supplemented by, Magnetic Polarity on the Same Continent with Rocks of Different Ages, Magnetic Polarity on Different Continents with Rocks of the Same Age, Creative Commons Attribution 4.0 International.

1993 Ford L9000 Headlight Assembly, Committee For Police Officers' Defense Legit, Pamana Peta 2013 Summary, Ray Hadley Wedding Photos, Articles H

how does glacial evidence support continental drift