Glossopteris
i nned the answer to
i nned the answer to
Alfred Wegener. Hope this helps.
Fossils found on different continents that were once connected support the idea of continental drift. The similarities in fossilized plants and animals found on separate continents suggest these landmasses were once part of the same supercontinent. This evidence helps corroborate the hypothesis of continental drift proposed by Alfred Wegener.
How seafloor spreading helps to explain the theory of continental drift is that wegener couldn't explain why and waht force caused the continents to move and so seafloor spreading helps to explain the theory of continental drift because it shows the force that made the continents move and that was te only thing that wagener needed to prove his theory of continental drift............thanks
Plate tectonics helps us to explain continental drift.
The continental drift is important because we get to understand more about the structure of the earth and understand how it became to be what it's today. Because without it we wouldn't understand why the lands split apart and became seperate continents.
The trilobite fossil is found on all continents, suggesting they were once connected in a supercontinent called Pangaea about 300 million years ago. The distribution of trilobite fossils across land masses helps support the theory of continental drift, which states that continents were once joined together before drifting apart due to tectonic plate movements.
Seafloor spreading and continental drift are linked through the theory of plate tectonics. Seafloor spreading occurs at mid-oceanic ridges, where new crust is formed and pushes apart the plates on either side. This process helps drive the movement of continents, as the newly formed crust pushes older crust away from the ridges and towards the continents, contributing to the overall process of continental drift.
One example is the development of GPS technology. By using GPS to measure the movement of tectonic plates, scientists have been able to gather data supporting the theory of continental drift. This technology has provided evidence of plate movement and helped refine our understanding of Earth's geological processes.
The discovery of seafloor spreading and magnetic striping on the ocean floor in the 1960s provided compelling evidence for Alfred Wegener's theory of continental drift. This process showed how new oceanic crust is formed at mid-ocean ridges and helps move the continents apart, supporting the idea that continents are not fixed but can drift over time.
Seafloor spreading is the process where new oceanic crust is formed at mid-ocean ridges and then moves apart, while continental drift refers to the movement of continents on the Earth's surface. Seafloor spreading is one mechanism that helps drive the movement of continents as part of plate tectonics.