Fossil evidence: the discovery of identical fossils on continents separated by vast oceans supports the idea that these landmasses were once joined together.
Matching geological features: the alignment of mountain ranges and rock formations on different continents, such as the Appalachian Mountains in North America and the Caledonian Mountains in Europe, provide evidence of past connections.
There are several pieces of evidence from land features which support Wegener's idea of continental drift. One example is that if you line up the maps of South America and Africa you will see that the mountain ranges line up, which is strong evidence that the two continents were once one.
The discovery of mid-ocean ridges and the process of seafloor spreading in the 1960s caused scientists to rethink Wegener's theory of continental drift. This new evidence provided a mechanism for how continents could move apart and lent support to the concept of plate tectonics as the driving force behind the movement of Earth's lithospheric plates.
Alfred Wegener used fossil evidence, geological evidence, and paleoclimatic evidence to support his theory of Continental Drift. Fossils of the same species found on different continents, similar rock formations and mountain ranges across continents, and matching ancient climate patterns were key pieces of evidence that he presented.
Which type of evidence was NOT used by Alfred Wegener to support his continental drift hypothesis human remains
Fossils found on separate continents that are now far apart provide evidence for continental drift. Similar fossil species found on continents that were once connected suggest that these landmasses were once united. Additionally, matching rock formations and paleoclimate evidence from fossils support the hypothesis of continental drift.
Fossils support his hypothesis.
yes it does.
Which type of evidence was NOT used by Alfred Wegener to support his continental drift hypothesis human remains
New evidence supporting Alfred Wegener's theory of continental drift began to emerge in the late 1940s and early 1950s, approximately 30 years after he first proposed the theory in 1912. The development of plate tectonics, particularly the discovery of seafloor spreading and paleomagnetism, provided crucial evidence that validated Wegener's ideas. This shift in understanding revolutionized geosciences and established a comprehensive framework for explaining the movement of continents.
There are several pieces of evidence from land features which support Wegener's idea of continental drift. One example is that if you line up the maps of South America and Africa you will see that the mountain ranges line up, which is strong evidence that the two continents were once one.
The discovery of mid-ocean ridges and the process of seafloor spreading in the 1960s caused scientists to rethink Wegener's theory of continental drift. This new evidence provided a mechanism for how continents could move apart and lent support to the concept of plate tectonics as the driving force behind the movement of Earth's lithospheric plates.
human remains
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 used fossil evidence, geological evidence, and paleoclimatic evidence to support his theory of Continental Drift. Fossils of the same species found on different continents, similar rock formations and mountain ranges across continents, and matching ancient climate patterns were key pieces of evidence that he presented.
Which type of evidence was NOT used by Alfred Wegener to support his continental drift hypothesis human remains
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.
Fossils found on separate continents that are now far apart provide evidence for continental drift. Similar fossil species found on continents that were once connected suggest that these landmasses were once united. Additionally, matching rock formations and paleoclimate evidence from fossils support the hypothesis of continental drift.