The continents move.
Wegener's theory of continental drift was initially not widely accepted due to a lack of a plausible mechanism to explain how continents could move across the Earth's surface. His idea challenged established geological beliefs and was met with skepticism from many scientists. Additionally, the evidence he presented, such as fossil distribution and geological similarities, was not convincing enough to overcome the prevailing notions of fixed continents. It wasn't until the development of plate tectonics in the mid-20th century that his ideas gained the recognition they deserved.
Wegener's theory didn't explain how the continents could plow through the solid rock of the sea floor, and he was unable to give a convincing explanation of what force could move entire continents.
Shadows are caused by the sun's rays upon the earth. As the sun rotates and moves during the day, the rays move and so shadows also move during daytime
because he couldn't explain what forces caused the continents to move... :D yup that's why
Continents move during continental drift due to the movement of tectonic plates in the Earth's crust. Plate tectonics theory explains that the Earth's lithosphere is divided into large plates that float on the semi-fluid asthenosphere beneath them. As these plates move and interact with each other, they can carry continents along with them, causing the continents to drift apart or come together over geological time.
During the Paleozoic Era, the continents were mostly joined together as a supercontinent called Pangaea. In the Mesozoic Era, Pangaea began to break apart, leading to the formation of the modern continents. Throughout the Cenozoic Era, the continents continued to move to their current positions due to the process of plate tectonics.
True
A pole shift refers to a change in the Earth's rotational axis, which can affect the distribution of land and sea but does not cause the continents to physically move. Plate tectonics are responsible for the movement of continents over long geological timescales.
the continents fit together like a puzzle
Fossils found on different continents suggested that they were once connected due to similar species being found far apart. Mountain belts on different continents lined up when the continents were pieced together, indicating a shared geological history. These pieces of evidence helped in understanding continental drift and the movement of continents over time.
Pangaea came together over a period of time spanning the Carboniferous and Permian periods. It broke up mostly during the Jurassic period.
Alfred Wegener proposed the theory of continental drift in the early 20th century because he observed similar plant and animal fossils on continents that are now far apart, as well as matching geological formations and evidence of ancient climates that suggest the continents were once joined together and have since drifted apart.
Plate tectonics. Continents are the exposed (from the oceans) geological areas of tectonic plates. Continents can also be on top of more than one tectonic plate. When these plates move, continents move with them. Millions of years ago, continents were split apart and also created by tectonic plate movement.
I saw that yesterday, Gotta log on ZINGO! During plate movement, the plates under the continents moved apart. This caused the land to move in separate directions. When the continents were all put together, the land was known as Pangea. Plate movement also causes the land to move together, which forms mountains.
Sea-floor spreading is the process where new oceanic crust is formed at mid-ocean ridges, pushing the existing crust apart. As the crust spreads, it carries the continents on tectonic plates with it, causing the continents to move. This movement is called plate tectonics, and it is responsible for the shifting of continents over geological time scales.
The theory that states that the continents move over the surface of the Earth is called plate tectonics. It explains how the Earth's lithosphere is divided into several plates that float on the semi-fluid asthenosphere beneath them, causing the continents to move and interact with each other. These movements are responsible for various geological phenomena like earthquakes, volcanoes, and mountain formation.