The shapes of continents appearing on the map clearly show similar shapes and how the continents might fit together.
Four pieces of evidence used by Alfred Wegener to support his theory of continental drift were the fit of the continents, matching geological formations across continents, similar fossil distributions, and glacial evidence in tropical regions.
Climate patterns and fossil evidence can help support continental drift theory. For example, matching rock formations and fossils across continents suggest they were once connected. Additionally, similarities in climate types and geological features between distant landmasses also provide evidence for past continental connections.
Other evidence to support Alfred Wegener's theory of continental drift includes matching geological formations and rock types on different continents, similar fossil collections on continents that are now separated by oceans, and the fit of the continents' coastlines like pieces of a jigsaw puzzle. Additionally, the discovery of mid-ocean ridges and the study of paleomagnetism has further bolstered the theory.
Two things that supports the continental drift theory are; 1. Fossil. 2. Continent Shapes.
It supports the theory because it can be found on all of the continents.
the age of the rocks in the sea floor is all the same
he used fossils, glacial indentations, and different types of rock.
The Continental Drift theory is a theory because there is no evidence to support it. Alfred Wegener developed the Continental Drift theory in the 1800's.
Alfred Wegener looked for several lines of evidence to support his theory of continental drift, including the fit of the continents like puzzle pieces, matching geological formations across continents, similarities in fossils and plants, and evidence from paleoclimate data such as glacial deposits.
Four pieces of evidence used by Alfred Wegener to support his theory of continental drift were the fit of the continents, matching geological formations across continents, similar fossil distributions, and glacial evidence in tropical regions.
Scientists use evidence such as matching fossil records, rock formations, and geological structures across continents, as well as the fit of the continents themselves, to support the theory of continental drift. Additionally, studies of oceanic crust age and magnetic patterns on the seafloor provide further evidence for plate tectonics and continental movement.
Evidence of ancient climates, such as glacial deposits in regions that are now near the equator, support continental drift theory because they suggest that these regions were once located at higher latitudes where glaciers were common. This is consistent with the idea that continents were once joined together in different configurations and have since drifted to their current positions. Additionally, similarities in fossil distributions and rock formations across continents also support the theory of continental drift.
Alfred Wegener used several lines of evidence to support his theory of continental drift, including the jigsaw-like fit of the continents, similarities in rock formations and fossil remains across continents, and the matching geological features along coastlines of different continents, such as mountain ranges and ancient glacial deposits.
Alfred Wegener used evidence such as the fit of the continents, matching geological formations across continents, identical fossil species found on different continents, and similarities in rock types and mountain ranges as support for his theory of continental drift.
Climate patterns and fossil evidence can help support continental drift theory. For example, matching rock formations and fossils across continents suggest they were once connected. Additionally, similarities in climate types and geological features between distant landmasses also provide evidence for past continental connections.
they couldn't agree on how it separated or what made it separate.
Other evidence to support Alfred Wegener's theory of continental drift includes matching geological formations and rock types on different continents, similar fossil collections on continents that are now separated by oceans, and the fit of the continents' coastlines like pieces of a jigsaw puzzle. Additionally, the discovery of mid-ocean ridges and the study of paleomagnetism has further bolstered the theory.