Drifting

Pangaea or Pangea was the super-continent in the continental drift hypothesis.

The primary force behind seafloor spreading and continental drift is convection currents in the Earth's mantle. These currents move the tectonic plates above them, causing them to either spread apart or collide. The spreading of seafloor and the shifting of continents are part of the larger process of plate tectonics.

Alfred Wegener, a German meteorologist and geophysicist, first proposed the theory of continental drift in 1912. He suggested that the continents were once part of a single supercontinent called Pangaea, which later broke apart and drifted to their current positions due to the movement of the Earth's mantle caused by thermal convection.

Alfred Wegener proposed the theory of continental drift in 1912. He collected evidence from various fields, such as the fit of continental coastlines, matching rock types and structures across continents, and similar fossil distributions. However, his theory was not widely accepted until decades later when the concept of plate tectonics provided a mechanism for how continents could move.

Magnetic drift refers to the slow and gradual change in the orientation of the Earth's magnetic field over time. It is caused by various factors, including the movement of molten iron in the outer core of the Earth. Magnetic drift is an important phenomenon that is closely monitored by scientists to better understand the behavior of the Earth's magnetic field.

The man who pioneered the continental drift hypothesis was Alfred Wegener. He proposed the theory in 1912, suggesting that Earth's continents were once joined together in a single landmass called Pangea and have since drifted apart.

Quite simply, the answer is no. While there is no doubt better equipment will make the task easier, you basically need RWD vehicle with LSD or locked diff in it. Drifting an open diff car is very hard and almost impossible.

Deep-sea mountain ranges had caught his attention.

Alfred Wegener's fully developed theory of continental drift attempted to point out evidences that the continents were once joined into a single continent he called Pangaea. Wegener's theory hypothesized that the continents were able to push through the rock of the seafloor to their present positions.

As evidence, he noted (as had others before him), of the geographic correlation in coastline perimeters of South America and Africa. This was the feature that led Wegener to investigate other clues. His investigations revealed that mountain ranges in South America and Africa, and strata and composition of coal fields in Europe and North America matched or lined up. Additionally, matching reptilian fossils were found on either side of the ocean, indicating that the continents were once joined together. Although he was unable to find a mechanism for his proposed continental drift theory, he also observed that the more shallow an ocean, the younger its geologic age. It wasn't until the 1950's and 1960's, with the discovery of the Mid-Atlantic Ridge (and other sea floor mapping discoveries) that Wegener's hypothesis started to become more accepted. The newer science of plate tectonics owes much to Wegener's scientific groundwork.

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The idea of continental drift was first proposed by Alfred Wegener in 1912. He suggested that the continents were once joined together in a single supercontinent called Pangaea and have since drifted apart.

The difference between drift current and diffusion current is that drift current depends on the electric field applied: if there's no electric field, there's no drift current. Diffusion current occurs even though there isn't an electric field applied to the semiconductor. It does not have E as one of its parameters. The constants it does depend on are Dp and Dn, and +q and -q, for holes and electrons respectively. The first constants are called the diffusion coefficients, a proportionality factor. We don't worry too much about these because they are constants. We do worry about the gradient of the concentration of p and/or n, though. But, since we are talking about a one dimensional situation when we are solving for current densities, we only worry about the gradient (or derivative) with respect to the x-plane. The other difference between drift current and diffusion current, is that the direction of the diffusion current depends on the change in the carrier concentrations, not the concentrations themselves. In the equation, the signs are reversed as we are used to seeing them. We usually assign a +q to holes and -q to electrons. In the case of diffusion current, they are reversed to be opposite of the derivative of the concentrations. This occurs because the carriers are diffusing from areas of high concentrations to areas of low concentrations. For example, if the derivative of pwith respect to x is positive, then the concentration of holes is growing as you move towards the +x direction. Diffusion current will be the opposite of that, the holes will be diffusing in the -x direction to where there's a lower concentration of holes. If the derivative is negative, the opposite will occur. The concentration of holes is decreasing as you go from the -x to +x direction. Therefore, holes will diffuse to the +x direction where there's a lower concentration of holes. This is why the negative sign is needed in the equation for the hole diffusion current. The same goes for electrons, but in this case, the signs cancel for a positive derivative because the electrons, carrying -q, diffuse to the -x direction where there's less electrons. The sign remains if the derivative is negative, because electrons will be diffusing to the +xdirection carrying a -q charge. For these reasons it's not included in the equation for the electron diffusion current. source: http://www.ece.utep.edu/courses/ee3329/ee3329/Studyguide/ToC/Fundamentals/CAction/diffusion.html The difference between drift current and diffusion current is that drift current depends on the electric field applied: if there's no electric field, there's no drift current. Diffusion current occurs even though there isn't an electric field applied to the semiconductor. It does not have E as one of its parameters. The constants it does depend on are Dp and Dn, and +q and -q, for holes and electrons respectively. The first constants are called the diffusion coefficients, a proportionality factor. We don't worry too much about these because they are constants. We do worry about the gradient of the concentration of p and/or n, though. But, since we are talking about a one dimensional situation when we are solving for current densities, we only worry about the gradient (or derivative) with respect to the x-plane. The other difference between drift current and diffusion current, is that the direction of the diffusion current depends on the change in the carrier concentrations, not the concentrations themselves. In the equation, the signs are reversed as we are used to seeing them. We usually assign a +q to holes and -q to electrons. In the case of diffusion current, they are reversed to be opposite of the derivative of the concentrations. This occurs because the carriers are diffusing from areas of high concentrations to areas of low concentrations. For example, if the derivative of pwith respect to x is positive, then the concentration of holes is growing as you move towards the +x direction. Diffusion current will be the opposite of that, the holes will be diffusing in the -x direction to where there's a lower concentration of holes. If the derivative is negative, the opposite will occur. The concentration of holes is decreasing as you go from the -x to +x direction. Therefore, holes will diffuse to the +x direction where there's a lower concentration of holes. This is why the negative sign is needed in the equation for the hole diffusion current. The same goes for electrons, but in this case, the signs cancel for a positive derivative because the electrons, carrying -q, diffuse to the -x direction where there's less electrons. The sign remains if the derivative is negative, because electrons will be diffusing to the +xdirection carrying a -q charge. For these reasons it's not included in the equation for the electron diffusion current. source: http://www.ece.utep.edu/courses/ee3329/ee3329/Studyguide/ToC/Fundamentals/CAction/diffusion.html The difference between drift current and diffusion current is that drift current depends on the electric field applied: if there's no electric field, there's no drift current. Diffusion current occurs even though there isn't an electric field applied to the semiconductor. It does not have E as one of its parameters. The constants it does depend on are Dp and Dn, and +q and -q, for holes and electrons respectively. The first constants are called the diffusion coefficients, a proportionality factor. We don't worry too much about these because they are constants. We do worry about the gradient of the concentration of p and/or n, though. But, since we are talking about a one dimensional situation when we are solving for current densities, we only worry about the gradient (or derivative) with respect to the x-plane. The other difference between drift current and diffusion current, is that the direction of the diffusion current depends on the change in the carrier concentrations, not the concentrations themselves. In the equation, the signs are reversed as we are used to seeing them. We usually assign a +q to holes and -q to electrons. In the case of diffusion current, they are reversed to be opposite of the derivative of the concentrations. This occurs because the carriers are diffusing from areas of high concentrations to areas of low concentrations. For example, if the derivative of pwith respect to x is positive, then the concentration of holes is growing as you move towards the +x direction. Diffusion current will be the opposite of that, the holes will be diffusing in the -x direction to where there's a lower concentration of holes. If the derivative is negative, the opposite will occur. The concentration of holes is decreasing as you go from the -x to +x direction. Therefore, holes will diffuse to the +x direction where there's a lower concentration of holes. This is why the negative sign is needed in the equation for the hole diffusion current. The same goes for electrons, but in this case, the signs cancel for a positive derivative because the electrons, carrying -q, diffuse to the -x direction where there's less electrons. The sign remains if the derivative is negative, because electrons will be diffusing to the +xdirection carrying a -q charge. For these reasons it's not included in the equation for the electron diffusion current. source: http://www.ece.utep.edu/courses/ee3329/ee3329/Studyguide/ToC/Fundamentals/CAction/diffusion.html

Drift velocity is the average velocity with which charged particles, such as electrons, move in a conductor in the presence of an electric field. It is a very slow velocity due to frequent collisions with atoms in the material. Drift velocity is responsible for the flow of electric current in a circuit.

The magnetic quality of feldspar is caused by the presence of trace elements such as iron, titanium, or manganese in its structure. These trace elements create magnetic moments that align with an external magnetic field, giving feldspar its magnetic properties.

Alfred Wegener is credited with developing the theory of continental drift in the early 20th century. He proposed that the Earth's continents were once all joined together in a single supercontinent called Pangaea, which later broke apart and drifted to their current positions.

Specifically, drift relates the movement of a carrier (e.g., an electron or hole) to an applied electric field (i.e., the velocity of the carrier is proportional to the electric field, where the proportionality constant, mobility, is a quantity derived in solid-state physics). Diffusion relates the movement of carriers due to random (i.e., thermal) behavior and non-uniform distribution (i.e., the velocity of the carrier is proportional to the logarithmic derivative of the density of carriers, where the proportionality constant, the diffusion constant, is a quantity derived in solid-state physics).

There are many factors that can cause a vehicle to drift when moving at highway speed.

First off is the alignment of the vehicles tires. At slow speeds this may not be noticable to the driver, but as the vehicles speed increases, the small inperfection in the tires alignment becomes magnified, causing the vehicle to pull (drift) to one side or the other. This can also be caused by the slight variations in each individual tire's pressure as well.

Second, the drift can be caused by force of and direction of the prevailing wind passing over the highway. In addition, as the vehicle increases in speed, minor inperfections in the vehicles aerodynamic shape (tailpipes, muffler, dings, dents ect) can alter the force of the wind passing both above and below the vehicle causing drift.

Weight distribution in the vehicle also plays a part in this. More weight on one side will cause the vehicle to pull in that direction.

This is just a few of the basic reasons.

A drift current is electric charges being moved in the presence of an electric field, and a diffusion current is electric charges being moved by a chemical diffusion gradient (where no electric field exists, but where there is a concentration gradient of chemical species driving the current).

Pangaea was a supercontinent that existed around 300 million years ago, when all the Earth's landmasses were joined together. Over time, Pangaea broke apart due to tectonic plate movement, leading to the formation of the continents we have today. The current continents are still moving very slowly, which is known as plate tectonics.

Alfred Wegener used various pieces of evidence to support his theory of continental drift, including the fit of the continents, rock and fossil similarities across continents, glacial evidence, and similar geological features on different continents.

Tools such as sonar mapping, geologic sampling, and paleomagnetism studies were used to provide evidence for seafloor spreading. Sonar mapping allowed for the creation of detailed maps of the ocean floor, revealing features such as mid-ocean ridges and deep-sea trenches. Geologic sampling involved collecting rock samples from the ocean floor to study their age and composition. Paleomagnetism studies focused on analyzing the alignment of magnetic minerals in rocks, providing evidence of past changes in Earth's magnetic field that support the idea of seafloor spreading.

Weber's deductive theory of location of industries, also known as the theory of industrial location, posits that industries are located based on minimizing transportation costs related to inputs and outputs. It suggests that industries will choose locations that provide the most cost-efficient combination of factors such as raw materials, labor, and markets. The theory considers factors like labor, capital, transportation costs, and agglomeration effects to determine the optimal location for an industry.

Alfred Weber's Theory of Industrial Location, also known as the Least Cost Theory, suggests that the location of industries is determined by minimizing transportation costs and maximizing profits. According to this theory, industries will locate where they can minimize the costs of transporting raw materials to the factory and finished products to the market. Weber classified industries into three categories based on their location factors: weight-gaining, weight-losing, and bulk-reducing.

Citing passages from a text is one way to provide elaboration in an essay.

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Provided it is done to show your research results or in fair criticism, and not merely to plagiarise!

Name a fossil that was found on different continents and was used to support the theory of continental drift.

How to Drift on "Mario Kart."

1. Select your kart and stuff

2. Don't select "Automatic" instead select "Manual"

3. When going around corners hold the "B" button until blue sparks appear at the back at your Kart/Bike (If you want a bigger boost hold "B" until the sparks go to yellow)

This isn't important but if you just tap the "B" button your Kart/Bike it will hop.