Mountain chains are formed by the action of different tectonic plates drifting into and colliding with each other. When they collide one plate rides over the top of the other creating a mountain or mountain range.
Fossil evidence of plants and animals that were once distributed across continents and matching geological formations such as mountain ranges or rock layers on different continents provide clues supporting the continental drift hypothesis. Additionally, evidence of past climates, such as ancient glacial deposits in regions that are now far from the poles, further support the idea of continental drift.
Fossil evidence, such as similar plant and animal species found across distant continents, supports the theory of continental drift. Additionally, matching geological features, like mountain ranges or rock formations, that line up when continents are brought together provide further evidence. Magnetic striping on the ocean floor also points towards seafloor spreading and the movement of continents.
Two forms of evidence used to support continental drift are fossil evidence, where similar plant and animal fossils are found on different continents that were once connected, and geological evidence, such as matching rock formations and mountain ranges across separate continents. These pieces of evidence provide support for the idea that continents were once joined together and have since drifted apart.
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.
Scientists use the magnetic properties of some minerals as evidence of past changes in Earth's magnetic field. These changes can provide insight into the Earth's geological history, including continental drift and past climates.
Is there a list? Continental drift is real, so religious fanatics don't provide evidence for continental drift.
i dont now now go ask Google
Yes
It is any trace of an ancient organism that has been preserved in rock.Fossils provided evidence for continental drift by Wegener's hypothesis. Wegener studied land features, fossils, and evidence of climate change.
Fossil evidence of plants and animals that were once distributed across continents and matching geological formations such as mountain ranges or rock layers on different continents provide clues supporting the continental drift hypothesis. Additionally, evidence of past climates, such as ancient glacial deposits in regions that are now far from the poles, further support the idea of continental drift.
Fossil evidence, such as similar plant and animal species found across distant continents, supports the theory of continental drift. Additionally, matching geological features, like mountain ranges or rock formations, that line up when continents are brought together provide further evidence. Magnetic striping on the ocean floor also points towards seafloor spreading and the movement of continents.
Rock types can provide evidence of continental drift by matching on opposite sides of current oceans, showing that the continents were once connected. For example, the Appalachian Mountains in North America align with the Caledonian Mountains in Scotland, indicating they were once part of the same mountain range before continental drift occurred. Additionally, similar fossils and rock formations found on different continents support the theory of continental drift.
Continental location refers to the position of a place or region on a continent. It helps identify the broad area that a place is located within, such as North America or Europe. Understanding the continental location can provide insight into the climate, culture, and geopolitical relationships of the area.
You can not DECIDE where to move continents, the movement of continents is a natural geological process, nothing man does can affect it.
Evidence for continental drift includes matching geological formations on different continents, such as mountain ranges and sedimentary layers. Additionally, the fit of the continents like puzzle pieces, similarities in fossil records on separate continents, and matching glacial evidence provide support for the theory. Paleoclimatic evidence, such as the distribution of ancient flora and fauna, also contributes to the case for continental drift.
Evidence supporting the hypothesis of continental drift includes the fit of continents like South America and Africa, matching geological features and rock formations across continents, and similar fossil records found on separate continents. Additionally, the presence of ancient glacial deposits and the alignment of mountain ranges between continents provide further support for the movement of continents over time.
Two forms of evidence used to support continental drift are fossil evidence, where similar plant and animal fossils are found on different continents that were once connected, and geological evidence, such as matching rock formations and mountain ranges across separate continents. These pieces of evidence provide support for the idea that continents were once joined together and have since drifted apart.