Continental drift is the movement of the Earth's continents relative to each other by appearing to drift across the ocean bed The speculation that continents might have 'drifted' was first put forward by Abraham Ortelius in 1596. The concept was independently and more fully developed by Alfred Wegener in 1912, but his theory was rejected for being incomplete. The idea of continental drift has been subsumed by the theory of plate tectonics which explains how the continents moveThe formation and evolution of the Solar System,
In geology subduction is the process that takes place at convergent boundaries by which one tectonic plate moves under another tectonic plate and sinks into the mantle as the plates converge. Regions where this process occurs are known as subduction zones. Rates of subduction are typically centimetres per year, with the average rate of convergence being approximately two to eight centimetres per year
Sedimentary rocks are types of rock that are formed by the deposition of material at the Earth's surface and within bodies of water. Sedimentation is the collective name for processes that cause mineral and/or organic particles (detritus) to settle and accumulate or minerals to precipitate from a solution. Particles that form a sedimentary rock by accumulating are called sediment. Before being deposited, sediment was formed by weathering and erosion in a source area, and then transported to the place of deposition by water, wind, ice, mass movement or glaciers which are called agents
lithosphere is divided into several rigid segments, or tectonic plates, that migrate across the surface over periods of many millions of years. Over 70% percent of Earth's surface is covered with wate[ with the remainder consisting of continents and islands which together have many lakes and other sources of water that contribute to the hydrosphere. Earth's poles are mostly covered with ice that is the solid ice of the Antarctic ice sheet and the sea ice that is the polar ice packs. The planet's interior remains active
A mineral is a naturally occurring substance that is solid and stable at room temperature, representable by a chemical formula, usually abiogenic, and has an ordered atomic structure. It is different from a rock, which can be an aggregate of minerals or non-minerals and does not have a specific chemical composition. The exact definition of a mineral is under debate, especially with respect to the requirement a valid species be abiogenic, and to a lesser extent with regards to it having an ordered atomic structure.
Understanding of Earth history,
The Earth is the stage on which the evolutionary play is performed. Darwin studied evolution in the context of Charles Lyell's geology, but our present understanding of Earth history includes some critical advances made during the last half-century.
Igneous rock is one of the three main rock types, the others being sedimentary and metamorphic rock. Igneous rock is formed through the cooling and solidification of magma or lava. Igneous rock may form with or without crystallization, either below the surface as intrusive (plutonic) rocks or on the surface as extrusive (volcanic) rocks. This magma can be derived from partial melts of pre-existing rocks in either a planet's mantle or crust. Typically, the melting is caused by one or more of three processes: an increase in temperature, a decrease in pressure, or a change in composition. Over 700 types of igneous rocks have been described, most of them having formed beneath the surface of Earth's crust
Earth materials, internel structure of the earth, composition of the earth Jahangir Alam
Internal Structure of the Earth
The Processes that Change the Shape of the Earth
Composition of the Earth
Basic Rocks Types
Common Rock Forming Minerals
In geology subduction is the process that takes place at convergent boundaries by which one tectonic plate moves under another tectonic plate and sinks into the mantle as the plates converge. Regions where this process occurs are known as subduction zones. Rates of subduction are typically centimetres per year, with the average rate of convergence being approximately two to eight centimetres per year
Sedimentary rocks are types of rock that are formed by the deposition of material at the Earth's surface and within bodies of water. Sedimentation is the collective name for processes that cause mineral and/or organic particles (detritus) to settle and accumulate or minerals to precipitate from a solution. Particles that form a sedimentary rock by accumulating are called sediment. Before being deposited, sediment was formed by weathering and erosion in a source area, and then transported to the place of deposition by water, wind, ice, mass movement or glaciers which are called agents
lithosphere is divided into several rigid segments, or tectonic plates, that migrate across the surface over periods of many millions of years. Over 70% percent of Earth's surface is covered with wate[ with the remainder consisting of continents and islands which together have many lakes and other sources of water that contribute to the hydrosphere. Earth's poles are mostly covered with ice that is the solid ice of the Antarctic ice sheet and the sea ice that is the polar ice packs. The planet's interior remains active
A mineral is a naturally occurring substance that is solid and stable at room temperature, representable by a chemical formula, usually abiogenic, and has an ordered atomic structure. It is different from a rock, which can be an aggregate of minerals or non-minerals and does not have a specific chemical composition. The exact definition of a mineral is under debate, especially with respect to the requirement a valid species be abiogenic, and to a lesser extent with regards to it having an ordered atomic structure.
Understanding of Earth history,
The Earth is the stage on which the evolutionary play is performed. Darwin studied evolution in the context of Charles Lyell's geology, but our present understanding of Earth history includes some critical advances made during the last half-century.
Igneous rock is one of the three main rock types, the others being sedimentary and metamorphic rock. Igneous rock is formed through the cooling and solidification of magma or lava. Igneous rock may form with or without crystallization, either below the surface as intrusive (plutonic) rocks or on the surface as extrusive (volcanic) rocks. This magma can be derived from partial melts of pre-existing rocks in either a planet's mantle or crust. Typically, the melting is caused by one or more of three processes: an increase in temperature, a decrease in pressure, or a change in composition. Over 700 types of igneous rocks have been described, most of them having formed beneath the surface of Earth's crust
Earth materials, internel structure of the earth, composition of the earth Jahangir Alam
Internal Structure of the Earth
The Processes that Change the Shape of the Earth
Composition of the Earth
Basic Rocks Types
Common Rock Forming Minerals
T he geologic time scale (GTS) is a system of chronological measurement that relates stratigraphy to time, and is used bygeologists, paleontologists, and other earth scientists to describe the timing and relationships between events that have occurred throughout Earth's history. The table of geologic time spans presented here agrees with the dates and nomenclature set forth by theInternational Commission on Stratigraphy standard color codes of the International Commission on Stratigraphy.
Evidence from radiometric dating indicates that the Earth is about 4.54 billion years old. The geology or deep time of Earth's past has been organized into various units according to events which took place in each period. Different spans of time on the GTS are usually delimited by changes in the composition of strata which correspond to them, indicating major geological or paleontological events, such as mass extinctions.
Geological time, Understanding of Earth history,
Solar technologies , Mineral resources , Igneous rock .definition of a mineral , Alfred Wegener Earth's lithosphere,plate tectonics, Abraham Ortelius , The continents drift, the Earths interior, drrobisawesome, ESE 11, Bronx Community college
Orogeny refers to forces and events leading to a large structural deformation of the Earth's lithosphere (crust and uppermost mantle) due to the engagement of tectonic plates. Response to such engagement results in the formation of long tracts of highly deformed rock called orogens or orogenic belts. The word "orogeny" comes from the Greek (oros for "mountain" plus genesis for "creation" or "origin"),[1] and it is the primary mechanism by which mountains are built on continents. Orogens develop while a continental plate is crumpled and is pushed upwards to form mountain ranges, and involve a great range of geological processes collectively calledorogenesis.
A metamorphic facies is a set of metamorphic mineral assemblages that were formed under similar pressures and temperatures. The assemblage is typical of what is formed in conditions corresponding to an area on the two dimensional graph of temperature vs. pressure (See diagram at right).Rocks which contain certain minerals can therefore be linked to certain tectonic settings, times and places in geological history of the area. The boundaries between facies (and corresponding areas on the temperature v. pressure graph), are wide, because they are gradational and approximate
Origin and Abundance of elements in the Solar system and in the Earth and its...AkshayRaut51
Definition of Elements and atom
Origin of Universe
Theories of origin of Solar system and Earth
Chemical Composition of Planets
Chemical Composition of Earth
Chemical composition of Meteorites
Abundance of Elements
The earliest material found in the Solar System is dated to 4.5672±0.0006 by] therefore, it is inferred that the Earth must have been formed by accretion around this time. By 4.54±0.04 by the primordial Earth had formed. The formation and evolution of the Solar System bodies occurred in tandem with the Sun. In theory a solar nebula partitions a volume out of a molecular cloud by gravitational collapse, which begins to spin and flatten into a circumstellar disk, and then the planets
grow out of that in tandem with the star. A nebula contains gas, ice grains and dust
T he geologic time scale (GTS) is a system of chronological measurement that relates stratigraphy to time, and is used bygeologists, paleontologists, and other earth scientists to describe the timing and relationships between events that have occurred throughout Earth's history. The table of geologic time spans presented here agrees with the dates and nomenclature set forth by theInternational Commission on Stratigraphy standard color codes of the International Commission on Stratigraphy.
Evidence from radiometric dating indicates that the Earth is about 4.54 billion years old. The geology or deep time of Earth's past has been organized into various units according to events which took place in each period. Different spans of time on the GTS are usually delimited by changes in the composition of strata which correspond to them, indicating major geological or paleontological events, such as mass extinctions.
Geological time, Understanding of Earth history,
Solar technologies , Mineral resources , Igneous rock .definition of a mineral , Alfred Wegener Earth's lithosphere,plate tectonics, Abraham Ortelius , The continents drift, the Earths interior, drrobisawesome, ESE 11, Bronx Community college
Orogeny refers to forces and events leading to a large structural deformation of the Earth's lithosphere (crust and uppermost mantle) due to the engagement of tectonic plates. Response to such engagement results in the formation of long tracts of highly deformed rock called orogens or orogenic belts. The word "orogeny" comes from the Greek (oros for "mountain" plus genesis for "creation" or "origin"),[1] and it is the primary mechanism by which mountains are built on continents. Orogens develop while a continental plate is crumpled and is pushed upwards to form mountain ranges, and involve a great range of geological processes collectively calledorogenesis.
A metamorphic facies is a set of metamorphic mineral assemblages that were formed under similar pressures and temperatures. The assemblage is typical of what is formed in conditions corresponding to an area on the two dimensional graph of temperature vs. pressure (See diagram at right).Rocks which contain certain minerals can therefore be linked to certain tectonic settings, times and places in geological history of the area. The boundaries between facies (and corresponding areas on the temperature v. pressure graph), are wide, because they are gradational and approximate
Origin and Abundance of elements in the Solar system and in the Earth and its...AkshayRaut51
Definition of Elements and atom
Origin of Universe
Theories of origin of Solar system and Earth
Chemical Composition of Planets
Chemical Composition of Earth
Chemical composition of Meteorites
Abundance of Elements
The earliest material found in the Solar System is dated to 4.5672±0.0006 by] therefore, it is inferred that the Earth must have been formed by accretion around this time. By 4.54±0.04 by the primordial Earth had formed. The formation and evolution of the Solar System bodies occurred in tandem with the Sun. In theory a solar nebula partitions a volume out of a molecular cloud by gravitational collapse, which begins to spin and flatten into a circumstellar disk, and then the planets
grow out of that in tandem with the star. A nebula contains gas, ice grains and dust
An earthquake (also known as a quake, tremor or temblor) is the result of a sudden release of energy in the Earth's crust that creates seismic waves. The seismicity, seismism or seismic activity of an area refers to the frequency, type and size of earthquakes experienced over a period of time.
Earthquakes are measured using observations from seismometers. The moment magnitude is the most common scale on which earthquakes larger than approximately 5 are reported for the entire globe. The more numerous earthquakes smaller than magnitude 5 reported by national seismological observatories are measured mostly on the local magnitude scale, also referred to as the Richter scale.
Sedimentary rocks are types of rock that are formed by the deposition of material at the Earth's surface and within bodies of water. Sedimentation is the collective name for processes that cause mineral and/or organic particles (detritus) to settle and accumulate or minerals to precipitate from a solution. Particles that form a sedimentary rock by accumulating are called sediment. Before being deposited, sediment was formed by weathering and erosion in a source area, and then transported to the place of deposition by water, wind, ice, mass movement or glaciers which are called agents
Plate Tectonics is the driving force of geologic structures th.docxrandymartin91030
Plate Tectonics is the driving force of geologic structures that shape the world that we live in. The
first indication that continents might have been linked physically took place as soon as there was
mapping. It was known by the sixteenth and seventeenth century that the continents fitted together like
pieces of a puzzle. This and other proofs listed below lead to the concept of continental drift, that the
large continents had once been linked together. The scale movements of continents across the across
the surface of the planet was mind boggling.
By the close of the nineteenth century the geologist Edward Suess postulated that the southern
continents were joined together. This was from evidence seen by fossil animal distribution. Ancient life
forms have ranges just as modern animals. Tigers are found in India and Siberia, not in North America.
These ancient animals couldn’t get from South America to Africa, from Antarctica to Australia to India.
There were rock layers both sedimentary and igneous that were continuous on all of the five continents.
He christened this large continent Gondwanaland.
In 1915 Alfred Wegener wrote a book on continental drift. He proposed another super continent
called Pangaea. This continent included all of the modern continents. His mechanism for the movement
of the continents was that the continents moved through ocean crust, drifting until they joined then
breaking apart again. Wegener and others argued for their evidence pointing out rock similarities
type, similarities in rock trends and ages using all of the information gathered from Steno's laws and
fossil assemblages. They also showed that certain distant continents had similar plants and animals that
entered a different evolutionary path after the continents separated. An example of this is the fresh
water fish the Arowana found in both South America and Australia. Another example of this is the large
amount of marsupial
fossils found in South
America and Australia.
Placental mammals
were the dominant
mammalian life forms
in Eurasia, North
America and Africa.
Only in South America
and Australia were
marsupial fossils
dominated. It wasn't
until 3 million years ago
North and South
America joined
allowing placental
mammals to gain
dominance in South America. Despite this evidence Wegener and his followers mechanism for
continental movement was badly flawed. They proposed that the tidal forces from the Sun and Moon
like the tides in the ocean. This force is much too weak to move a continent so the theory was rejected.
Fossil plants and animal distribution on southern continents
In 1928 a geologist Arthur Holmes proposed the convection currents split the continents and that
these currents were in the mantel. Remember the knowledge of a mantel was already known at this
time. Ironically this was a mechanism had been proposed by Benjamin Franklin in 1782. Many
geologi.
Continental drift is the hypothesis that the Earth's continents have moved over geologic time relative to each other, thus appearing to have "drifted" across the ocean bed.
Wegener argued that there was once a super continent (which he named Pangea -meaning ''all land ) which split up over millions of year and gradually drifted over to their current place on earth at a rate of a few centimeter year.
Alfred Wegener produced evidence in 1912 that the continents are in motion, but because he could not explain what forces could move them, geologists rejected his ideas. Almost 50 years later, Harry Hess confirmed Wegener’s ideas by using the evidence of seafloor spreading to explain what moved the continents.
Register to explore the whole course here: https://school.bighistoryproject.com/bhplive?WT.mc_id=Slideshare12202017
How to Create Map Views in the Odoo 17 ERPCeline George
The map views are useful for providing a geographical representation of data. They allow users to visualize and analyze the data in a more intuitive manner.
This is a presentation by Dada Robert in a Your Skill Boost masterclass organised by the Excellence Foundation for South Sudan (EFSS) on Saturday, the 25th and Sunday, the 26th of May 2024.
He discussed the concept of quality improvement, emphasizing its applicability to various aspects of life, including personal, project, and program improvements. He defined quality as doing the right thing at the right time in the right way to achieve the best possible results and discussed the concept of the "gap" between what we know and what we do, and how this gap represents the areas we need to improve. He explained the scientific approach to quality improvement, which involves systematic performance analysis, testing and learning, and implementing change ideas. He also highlighted the importance of client focus and a team approach to quality improvement.
How to Split Bills in the Odoo 17 POS ModuleCeline George
Bills have a main role in point of sale procedure. It will help to track sales, handling payments and giving receipts to customers. Bill splitting also has an important role in POS. For example, If some friends come together for dinner and if they want to divide the bill then it is possible by POS bill splitting. This slide will show how to split bills in odoo 17 POS.
Synthetic Fiber Construction in lab .pptxPavel ( NSTU)
Synthetic fiber production is a fascinating and complex field that blends chemistry, engineering, and environmental science. By understanding these aspects, students can gain a comprehensive view of synthetic fiber production, its impact on society and the environment, and the potential for future innovations. Synthetic fibers play a crucial role in modern society, impacting various aspects of daily life, industry, and the environment. ynthetic fibers are integral to modern life, offering a range of benefits from cost-effectiveness and versatility to innovative applications and performance characteristics. While they pose environmental challenges, ongoing research and development aim to create more sustainable and eco-friendly alternatives. Understanding the importance of synthetic fibers helps in appreciating their role in the economy, industry, and daily life, while also emphasizing the need for sustainable practices and innovation.
2024.06.01 Introducing a competency framework for languag learning materials ...Sandy Millin
http://sandymillin.wordpress.com/iateflwebinar2024
Published classroom materials form the basis of syllabuses, drive teacher professional development, and have a potentially huge influence on learners, teachers and education systems. All teachers also create their own materials, whether a few sentences on a blackboard, a highly-structured fully-realised online course, or anything in between. Despite this, the knowledge and skills needed to create effective language learning materials are rarely part of teacher training, and are mostly learnt by trial and error.
Knowledge and skills frameworks, generally called competency frameworks, for ELT teachers, trainers and managers have existed for a few years now. However, until I created one for my MA dissertation, there wasn’t one drawing together what we need to know and do to be able to effectively produce language learning materials.
This webinar will introduce you to my framework, highlighting the key competencies I identified from my research. It will also show how anybody involved in language teaching (any language, not just English!), teacher training, managing schools or developing language learning materials can benefit from using the framework.
Read| The latest issue of The Challenger is here! We are thrilled to announce that our school paper has qualified for the NATIONAL SCHOOLS PRESS CONFERENCE (NSPC) 2024. Thank you for your unwavering support and trust. Dive into the stories that made us stand out!
Model Attribute Check Company Auto PropertyCeline George
In Odoo, the multi-company feature allows you to manage multiple companies within a single Odoo database instance. Each company can have its own configurations while still sharing common resources such as products, customers, and suppliers.
Palestine last event orientationfvgnh .pptxRaedMohamed3
An EFL lesson about the current events in Palestine. It is intended to be for intermediate students who wish to increase their listening skills through a short lesson in power point.
The French Revolution, which began in 1789, was a period of radical social and political upheaval in France. It marked the decline of absolute monarchies, the rise of secular and democratic republics, and the eventual rise of Napoleon Bonaparte. This revolutionary period is crucial in understanding the transition from feudalism to modernity in Europe.
For more information, visit-www.vavaclasses.com
2. Drifting Continents and Spreading Seas
Prepared by
Ronald Parker,
Earlham College Department of Geosciences
Richmond, Indiana
3. Continental Drift
The hypothesis that continents are mobile.
Proposed by German meteorologist Alfred Wegener.
The Origins of Oceans and Continents published in 1915.
Wegener hypothesized a former supercontinent Pangaea.
Idea was based on abundant evidence.
“Fit” of the continents.
Location of glaciations.
Fossil evidence.
Rock type and structural similarities.
Paleoclimatic evidence.
Earth: Portrait of a Planet, 3rd edition, by Stephen Marshak
Chapter 3: Drifting Continents and Spreading Seas
4. Continental Drift
Wegener’s idea was debated and ridiculed.
Most scientists didn’t believe him.
Lack of a mechanism for drift a major criticism.
Wegener died in 1930 at the age of 40.
Lacking an advocate, the drift
hypothesis faded.
His idea was revived in the 1950s.
Earth: Portrait of a Planet, 3rd edition, by Stephen Marshak
Chapter 3: Drifting Continents and Spreading Seas
5. Continental Drift
Now we can measure drift; Wegener was right!
Sea-floor spreading.
Subduction.
Plate tectonics.
Why was Wegener’s model dismissed by scientists?
Earth: Portrait of a Planet, 3rd edition, by Stephen Marshak
Chapter 3: Drifting Continents and Spreading Seas
6. Before Continental Drift
What were scientists thinking?
The oceans and the continents were permanently fixed.
There were no changes in continents back in time.
Evidence of drastic changes interpreted as…
Shrinkage effects.
Rebound from thick sediment loading.
The result of “upheaval.”
Earth: Portrait of a Planet, 3rd edition, by Stephen Marshak
Chapter 3: Drifting Continents and Spreading Seas
7. Continental “Fit”
Wegener noted the continents seem to fit together.
He argued that the fit could not be coincidental.
Present shorelines make a rough fit.
The continental shelf edges make a better fit.
Earth: Portrait of a Planet, 3rd edition, by Stephen Marshak
Chapter 3: Drifting Continents and Spreading Seas
8. Glacial Evidence
Permian glacial till is found on 4 continents.
The tills in Africa and India are now near equator.
A cooler earth? No, tropical plants also preserved.
Earth: Portrait of a Planet, 3rd edition, by Stephen Marshak
Chapter 3: Drifting Continents and Spreading Seas
9. Paleoclimatic Evidence
Placing Pangea over the Permian South Pole…
He correctly predicted…
Tropical coals.
Tropical reefs.
Subtropical deserts.
Subtropical evaporites.
Earth: Portrait of a Planet, 3rd edition, by Stephen Marshak
Chapter 3: Drifting Continents and Spreading Seas
10. Fossil Evidence
Identical fossils found on widely separated land.
Mesosaurus – A freshwater reptile.
Glossopteris – Subpolar plant with heavy seeds.
Earth: Portrait of a Planet, 3rd edition, by Stephen Marshak
Chapter 3: Drifting Continents and Spreading Seas
11. Fossil Evidence
Identical fossils found on widely separated land.
Lystrosaurus – A non-swimming, land-dwelling reptile.
Cynognathus – A non-swimming, land-dwelling reptile.
These organisms could not
have crossed an ocean.
Earth: Portrait of a Planet, 3rd edition, by Stephen Marshak
Chapter 3: Drifting Continents and Spreading Seas
12. Matching Geology
Geologic phenomena match across the Atlantic.
Geologic structures.
Rock types.
Rock ages.
Earth: Portrait of a Planet, 3rd edition, by Stephen Marshak
Chapter 3: Drifting Continents and Spreading Seas
13. Matching Geology
Geologic phenomenon match across the Atlantic.
Mountain belts.
Appalachians.
Caledonides.
Earth: Portrait of a Planet, 3rd edition, by Stephen Marshak
Chapter 3: Drifting Continents and Spreading Seas
14. Criticisms of Drift
Why wasn’t continental drift accepted?
There were no mechanisms for moving continents.
Wegener suggested that continents plowed through the
ocean crust, much like ice breakers cut through ice.
He invoked rotational (centrifugal) forces.
These ideas were easily discredited; so was his theory.
Earth: Portrait of a Planet, 3rd edition, by Stephen Marshak
Chapter 3: Drifting Continents and Spreading Seas
15. Continental Drift
When Wegener died, the debate did too.
A few continued to champion Wegener’s idea.
Arthur Holmes –Earth’s mantle moved by convection.
The drift hypothesis awaited the evidence provided
by paleomagnetism (see Interlude A).
Earth: Portrait of a Planet, 3rd edition, by Stephen Marshak
Chapter 3: Drifting Continents and Spreading Seas
16. The Ocean Floor
In the 1950s, ocean bathymetry was mapped by sonar.
Oceanographers were surprised to discover that…
The deepest parts of the ocean occur near land.
A mountain range runs through every ocean basin.
Submarine volcanoes form lines across ocean floors.
Earth: Portrait of a Planet, 3rd edition, by Stephen Marshak
Chapter 3: Drifting Continents and Spreading Seas
17. The Ocean Floor
Sonar mapping delineated bathymetric features.
Trenches.
Mid-ocean ridges (MORs).
Seamounts,
Guyots.
Earth: Portrait of a Planet, 3rd edition, by Stephen Marshak
Chapter 3: Drifting Continents and Spreading Seas
18. The Ocean Floor
Modern views of the ocean floor reveal:
Mid-ocean ridges.
Trenches.
Fracture zones.
Earth: Portrait of a Planet, 3rd edition, by Stephen Marshak
Chapter 3: Drifting Continents and Spreading Seas
19. Oceanic Crust
By 1950, we had learned much about oceanic crust.
Oceanic crust is covered by sediment.
Thickest near the continents.
Thinnest (or absent) at the mid-ocean ridge.
Oceanic crust is mafic (basalt and gabbro).
No granitic rocks.
No metamorphic rocks.
High heat flow characterizes the mid-ocean ridge.
Earth: Portrait of a Planet, 3rd edition, by Stephen Marshak
Chapter 3: Drifting Continents and Spreading Seas
20. Oceanic Crust
Belts of concentrated subsea earthquakes were found.
The earthquakes were surprising. They were limited to…
Parts of oceanic fracture zones.
Mid-ocean ridge axes.
Deep ocean trenches.
Earth: Portrait of a Planet, 3rd edition, by Stephen Marshak
Chapter 3: Drifting Continents and Spreading Seas
21. Sea Floor Spreading
In 1960, Harry Hess published his “Essay in Geopoetry.”
He called his theory “sea-floor spreading.”
Upwelling mantle erupts at the mid-ocean ridges.
New crust moves away from ridges, gathering sediment.
At trenches the sea-floor dives back into the mantle.
Provided a potential mechanism for continental drift.
Earth: Portrait of a Planet, 3rd edition, by Stephen Marshak
Chapter 3: Drifting Continents and Spreading Seas
22. Magnetic Anomalies
Towed magnetometers measure ocean crust.
Magnetism oscillates perpendicular to the MOR.
These variations are + and - magnetic anomalies.
Anomalies are linear belts that parallel MOR.
Earth: Portrait of a Planet, 3rd edition, by Stephen Marshak
Chapter 3: Drifting Continents and Spreading Seas
23. Magnetic Reversals
Layered lava flows reveal reversals in polarity.
Magnetic polarity is the direction of magnetic north.
When reversed, the north magnetic pole is near the south
geographic pole.
Reversals are geologically rapid.
Earth: Portrait of a Planet, 3rd edition, by Stephen Marshak
Chapter 3: Drifting Continents and Spreading Seas
24. Magnetic Reversals
Radioactivity permits rock age-dating.
A geomagnetic reversal time scale
has been assembled.
Reversals occur every 500-700 ka.
171 are known since the end Cretaceous.
Earth: Portrait of a Planet, 3rd edition, by Stephen Marshak
Chapter 3: Drifting Continents and Spreading Seas
25. Sea-Floor Spreading: Proof
Polarity reversals explain magnetic anomalies.
Positive anomalies – Crust with normal polarity.
Negative anomalies – Crust with reversed polarity.
Magnetic anomalies are symmetric across the MOR.
Earth: Portrait of a Planet, 3rd edition, by Stephen Marshak
Chapter 3: Drifting Continents and Spreading Seas
26. Sea-Floor Spreading: Proof
Magnetic anomalies mimic layered lava flows.
Magnetic “stripes” form as lava cools at a MOR.
Ocean crust spreads away from MOR.
Reversals are recorded within cooled lava.
SF spreading is the mechanism of continental drift.
Earth: Portrait of a Planet, 3rd edition, by Stephen Marshak
Chapter 3: Drifting Continents and Spreading Seas
27. Sea-Floor Spreading
Ages increase away from the MOR.
Ages are “mirror images” across the MOR.
Earth: Portrait of a Planet, 3rd edition, by Stephen Marshak
Chapter 3: Drifting Continents and Spreading Seas