Drifting

Researchers can decrease observer drift by providing frequent training and feedback to observers, using standardized observation protocols, implementing inter-rater reliability checks, and maintaining consistency in data collection methods. Regular supervision and evaluation of observers can also help minimize drift and ensure data accuracy.

A prevailing north wind would generally bring colder temperatures to a region, especially if the wind originates from polar or arctic regions. It may also cause increased cloud cover and precipitation on the windward side of mountain ranges. Overall, it could result in cooler and potentially wetter conditions depending on the specific location and weather patterns.

One piece of evidence that does not support the continental drift theory is the lack of a mechanism to explain how continents could drift across the Earth's surface. Additionally, some geologists have suggested that the movement of the continents is due to other processes like subsidence and uplift rather than drifting. Finally, the theory of plate tectonics provides a more comprehensive explanation for the movement of the Earth's lithosphere compared to the original theory of continental drift.

Objects drift in space due to the lack of significant gravitational forces, which would normally keep them in place. Without these forces in space, objects such as spacecraft can drift freely, following their current trajectory until acted upon by another force, like a thruster or gravitational pull from a celestial body.

Sea floor spreading provides evidence for continental drift by showing that new oceanic crust is created at mid-ocean ridges, pushing the continents apart. As the crust spreads apart, it carries the continents along with it, supporting the idea that the continents were once part of a single landmass that has since drifted apart. This process also explains the distribution of ages of oceanic crust, with the youngest crust found at the mid-ocean ridges and getting progressively older as you move away from the ridges.

Island arcs and chains, sedimentary fossils at the top of the Himalayas, rift valleys, mid-oceanic ridge, ages of rocks in certain areas, co-existing fossils in now separated areas, faults, subduction volcanoes, GPS measurement data, earthquakes.

Mid-ocean ridges are underwater mountain ranges where new oceanic crust is formed through volcanic activity. As the magma rises, it creates new crust that pushes the existing plates apart, providing evidence for seafloor spreading and supporting the theory of plate tectonics. The movement of these plates at mid-ocean ridges helps explain how continents have drifted and repositioned over geological time scales.

Many geologists and scientists at the time made fun of Alfred Wegener's Drift Theory, dismissing it as implausible and unscientific. Wegener's theory of continental drift proposed that the continents were once connected and drifted apart over time, which was not widely accepted until much later when the theory of plate tectonics was formulated.

In addition to matching coastlines, Wegener used similarities in rock formations and mountain ranges across different continents as evidence for his theory of continental drift. He also noted similarities in the distribution of fossils on separate continents, suggesting that the same species were once connected when the continents were joined.

Alfred Wegener's theory of continental drift was supported by several lines of evidence, including the matching coastlines of different continents, similarities in rock formations and mountain ranges across continents, and the distribution of fossils of similar species on different continents. He also observed the fit of the continents like pieces of a jigsaw puzzle and the presence of ancient glacial deposits in regions that are now at different latitudes.

The fossil that was found on different continents and used to support the theory of continental drift is the Mesosaurus. This extinct freshwater reptile had limited swimming abilities, making it unlikely that it could have crossed vast oceans. Its distribution on both sides of the Atlantic Ocean provided evidence of land connections that later formed the basis for the theory of continental drift.

Yes, fossil evidence such as similar plant and animal species found on separate continents has been used to support the continental drift hypothesis. The distribution of fossils across continents suggests that these land masses were once connected and later moved apart.

Continental drift theory proposed that continents had drifted apart due to tectonic forces, while plate tectonic theory expanded this idea to include the concept of lithospheric plates moving over the Earth's mantle. Through advancements in technology and the accumulation of evidence from various scientific fields, the two theories were unified into plate tectonics, which explains the movement of Earth's lithosphere and the formation of features like mountains, earthquakes, and volcanoes.

Alfred Wegener's evidence for the theory of continental drift included matching coastlines on different continents, similar rock formations and mountain ranges across continents, and the presence of identical fossils on separate continents. He also noted the jigsaw-like fit of South America and Africa and the distribution of climatic zones in ways that made more sense if the continents were once connected.

The hypothesis of continental drift suggests that continents were once joined together in a single landmass called Pangaea and have since drifted apart to their current positions. This theory was proposed by Alfred Wegener in the early 20th century and is supported by evidence such as matching geological formations, fossils, and the fit of continental coastlines.

Alfred Wegener used fossil evidence (matching plant and animal species across continents), geological evidence (similar rock formations and mountain ranges on different continents), climate evidence (glacial deposits and ancient climate patterns that suggested continents were once connected), and fit of continents (the way the continents seem to fit together like a puzzle) to support his hypothesis of continental drift.

Plate tectonics was proven through continental drift using evidence such as the fit of the continents, similar rock formations and fossils on different continents, matching mountain ranges, and the presence of mid-ocean ridges and deep ocean trenches. These pieces of evidence supported the idea that continents were once connected and have since moved apart due to the movement of the tectonic plates.

The West Wind Drift if also know as the ACC

Alfred Wegener's evidence for continental drift included the fit of the continents like puzzle pieces, the distribution of plant and animal fossils across continents, similarities in rock formations and mountain ranges, and evidence of past glaciations in regions that are now tropical. These observations led him to propose the theory of Pangea and the idea that continents were once joined together in a supercontinent.

If one can prove that the sea floor spreads out from the mid oceanic ridges, then logically the continents must be moving apart to accommodate the spreading. Conversely there must also be places where sea floor is being destroyed if the Earth is to stay the same size.

People initially did not believe Alfred Wegener's continental drift theory because he lacked a mechanism to explain how continents could move across the Earth's surface. Additionally, there was insufficient evidence at the time to support his theory. It was not until the development of the theory of plate tectonics in the 1960s that Wegener's ideas gained widespread acceptance.

Cause you started with Pangaea a large super continent which slowly broke apart and each one started drifting. Now plate tectonics is how the collisions occur and when and WHY. WHY are they colliding?, because they have drifted away from each other and are now colliding back together again. And also each individual plate will break and come together again.

Wegener first noticed that it looked like South America coastline could "fit" into Africa's. After that he analysed both their continental shelve's and this showed an even closer fit. The thrid observation that brought about his theory of continental drift was that he found fossils of the same animals (can't remember any names off the top of my head sorry) in both Argentina and east Somalia, Africa.

The animal is the Mesosaurus, a fossil known to live 270 million years ago. This animal was very unlikely to swim across the ocean, so the continents had to conjoined one time in the past. Hope this helps :)

Europe is warmer than it should be given its latitude because of the N.A.D. The North Atlantic Drift is an underwater current that forces warm water from the Carribean, east all the way to the Western end of Eurasia. In addition, the N.A.D. brings with it prevailing winds which lose most of its heat when they cross Portugual. Another example of currency is Lake Michigan. Since water changes temperature slowly, the closer you are to the lake in the summer the cooler it is and the closer you are to the lake in the winter the warmer it is. Therefore, Europe is warmer than it should be due to climactic changes brought about by the N.A.D.