The fact that there are subduction zones where continental plates meet !
Wegener showed evidence of similar rock formations and mountain ranges on different continents, evidence of matching plant and animal fossils on different continents, evidence of matching glacial deposits on different continents, and evidence of matching ancient climates on different continents to support his theory of continental drift.
The evidence that the continents are moving today is actually just a theory, but is accepted to be true. This theory is known as Continental Drift and is described as the continents belonging to tectonic plates, which are basically floating on the Earth's surface. Evidence to prove such is that the continents all fit together like a jigsaw puzzle and related or the same plant or animal species are located on separated continents, suggesting that they were all once connected to allow the animals to roam and the plants to spread. If they have moved in the past, they must still be moving today, and there are projected paths the continents are taking.
Evidence such as the distribution of fossils, rock formations, and magnetic fields on different continents support the theory of continental drift and the breakup of Pangaea. The matching geological features, such as mountain ranges and coastlines, on opposite sides of the Atlantic Ocean provide further evidence that the continents were once connected. Additionally, the movement of tectonic plates and the ongoing process of plate tectonics help explain the separation of the continents from Pangaea.
Three pieces of evidence used to prove the theory of continental drift were the fit of the continents' coastlines, the distribution of fossils across continents, and the matching geological formations found on separate continents. These observations supported the idea that the continents were once joined together and had drifted apart over time.
Evidence to prove the existence of the supercontinent Pangaea includes fossil evidence of similar plant and animal species across continents, the matching shapes of coastlines and mountain ranges on different continents, and the distribution of ancient rock formations that line up when continents are fitted together. Additionally, geological evidence such as rock layers and paleoclimatic data also supports the theory of Pangaea's existence.
It seems to prove that these continents were once close enough to each other that animals and plants could easily move between them through land.
Evidence that may be cited to prove the existence of a supercontinent includes the fit of the coastlines of continents like South America and Africa, shared geological features across continents, distribution of similar fossils and rock formations, and the alignment of mountain ranges like the Appalachian Mountains in North America and the Caledonian Mountains in Europe. Additionally, the study of plate tectonics and the movement of continental plates provides further evidence for the existence of past supercontinents like Pangaea.
The sinking of mid-ocean ridges into ocean trenches does not directly prove the Continental Drift theory. However, it supports the theory by providing evidence of plate tectonics and the movement of tectonic plates. The theory of plate tectonics explains how continents move and interact with each other over time.
Alfred Wegener proposed the theory of Pangaea based on the fit of the continents, similarities in rock formations, and fossil evidence across continents. He also noted similarities in geological structures and climate data that suggested the continents were once connected before drifting apart. However, Wegener's theory was not widely accepted until much later when additional evidence and advancements in plate tectonics supported his ideas.
Two main pieces of evidence that support Wegner's theory of continental drift are the fit of the continents' coastlines, indicating they were once connected, and the distribution of similar fossils and rock formations across separate continents, suggesting a shared geological history.
Oceanic crust that was farther away from a mid-ocean ridge was older that crust closer to the ridge
1. Continents fit like puzzles 2. Fossil evidence 3. Past climate changes