Evidence of continental drift includes matching Coastlines, geological similarities between continents, and the distribution of fossils and ancient species across continents that are now separated. Additionally, the discovery of mid-ocean ridges and the theory of plate tectonics further support this idea.
Evidence for continental drift includes the fit of continents like South America and Africa, similar rock formations and mountain ranges on different continents, and the distribution of fossils that were once found on now widely separated landmasses. These pieces of evidence suggest that the continents were once connected in a single landmass called Pangaea.
The supercontinent Pangaea connected all the continents about 300 million years ago. Over time, Pangaea split apart, leading to the formation of the continents as we know them today.
Wegener believed all continents had once been joined because of the similar shapes of coastlines, matching geological formations across continents, and evidence of past glaciation extending from multiple continents, suggesting they were once connected.
Early mapmakers thought the continents were once connected because they observed similarities in coastlines, geological formations, and fossil records across different continents. Additionally, the concept of continental drift and the theory of plate tectonics have since provided scientific explanations for the movement of continents over time.
One way we know that all the continents were connected at one point is through evidence of similar rock formations, fossils, and mountain ranges across different continents, indicating they were once part of a single landmass known as Pangaea.
The theory is called continental drift, proposed by Alfred Wegener. It suggests that continents were once part of a supercontinent called Pangaea and have since drifted to their current positions. This theory is supported by evidence such as matching coastlines and similar geological features on different continents.
The first evidence that led people to think that the continents were once connected because of earthquakes
If the continents were once connected, similarities in coastline features could include similar shapes, geological structures, and fossil evidence of past connections. Additionally, the coastlines might have similar trends or patterns that suggest common tectonic history.
Alfred wegener
I SAW IT in a book about the past all the continents were all hooked together but something broke it apart.
There are two main evidences for this: 1. The continents fit together like a puzzle 2. There are both extant and extinct animal and plant species present on several continents that are not connected
The theory is is that once all the continents were connected as 1 super continent. Later they split up to create the 7 we know now.
One piece of evidence that indicates the continents were once connected is the shape of the continents. Many of the continents look as if they fit together like a puzzle.
its is north America
Wegener proposed the theory of continental drift because he noticed how coastlines of continents seemed to fit together like pieces of a puzzle. He also observed similarities in rock formations, fossils, and climate across continents that suggested they were once connected. These observations led him to suggest that the continents had moved over time.
Wegener's theory was that all continents were once connected and are slowly drifting around.
Pangaea.