Alfred Wegeners 1912 theory of Plate tectonics and continental drift.
Alfred Wegener's theory of continental drift suggested that continents move over time on Earth's surface. This theory provided support for the concept of seafloor spreading, which explains how new oceanic crust forms at mid-ocean ridges and spreads outward. Both theories contributed to the development of the theory of plate tectonics, which explains the large-scale movements of Earth's lithosphere.
Alfred Wegener's theory of continental drift initially faced significant skepticism from the scientific community when he proposed it in the early 20th century. Many scientists rejected his ideas due to a lack of a plausible mechanism for how continents could move. However, the theory gained acceptance in the mid-20th century with the development of plate tectonics, which provided the necessary geological and physical explanations for continental movement. Today, Wegener's ideas are recognized as foundational to our understanding of Earth's geological processes.
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.
yes it does.
Fossils support his hypothesis.
There was no evidence to prove it
Alfred Wegeners 1912 theory of Plate tectonics and continental drift.
plate tectonics
It was not excepted because they didn't believe him at all until it was proven!
Alfred Wegener's theory of continental drift suggested that continents move over time on Earth's surface. This theory provided support for the concept of seafloor spreading, which explains how new oceanic crust forms at mid-ocean ridges and spreads outward. Both theories contributed to the development of the theory of plate tectonics, which explains the large-scale movements of Earth's lithosphere.
why did other scientist not accpet Alfred Wegeners theory
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.
rekmr
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's theory of continental drift initially faced significant skepticism from the scientific community when he proposed it in the early 20th century. Many scientists rejected his ideas due to a lack of a plausible mechanism for how continents could move. However, the theory gained acceptance in the mid-20th century with the development of plate tectonics, which provided the necessary geological and physical explanations for continental movement. Today, Wegener's ideas are recognized as foundational to our understanding of Earth's geological processes.