The distribution of mountains on different continents provided evidence for Wegener's theory of continental drift. He observed that mountain ranges on separate continents, such as the Appalachians in North America and the Caledonian mountains in Scotland, lined up when the continents were reconstructed into a single landmass (Pangaea). This alignment suggested that the continents were once connected and had drifted apart over time.
The distribution of similar rock types and geological structures across distant mountain ranges supported Alfred Wegener's idea of continental drift. This suggested that the mountains were connected before the continents drifted apart, explaining their shared characteristics. Additionally, the alignment of mountain ranges on different continents provided evidence for the theory of plate tectonics, which explains how mountains form at convergent plate boundaries.
The distribution of mountain ranges across different continents, such as the Appalachian Mountains in North America and the Caledonian Mountains in Europe, supports Wegener's idea of continental drift. These mountain ranges were once connected when the continents were part of a supercontinent, and their alignment provides evidence for the movement of land masses over time. Additionally, the presence of similar geological features and rock formations on separate continents suggests a shared history of mountain building.
The distribution of mountain ranges worldwide aligns with Wegener's idea of continental drift and plate tectonics. For example, the Appalachian Mountains in North America connect with the Caledonian Mountains in Europe, suggesting that the continents were once connected. Additionally, the occurrence of similar rock formations and fossils on separate continents supports the theory that these landmasses were once joined together.
Some historical landmarks in the Mountains and Basins region include Fort Davis National Historic Site, Guadalupe Mountains National Park, and Hueco Tanks State Park. These sites offer insights into the region's Native American history, Spanish colonization, and frontier military presence.
Wegener's theory of continental drift proposed that the continents were once joined together in a single supercontinent called Pangaea. Over time, the continents drifted apart to their current positions. This idea eventually led to the development of the theory of plate tectonics, which explains the movement of Earth's lithosphere on the underlying asthenosphere.
mountains usually occur in narrow bands along the edges of continents
mountains usually occur in narrow bands along the edges of continents
Mountains have usually formed on the edges of continents in narrow bands, where continents have collided in the past.
The distribution of mountain ranges across different continents supports Wegener's idea of continental drift. Mountains on different continents were once part of the same supercontinent, Pangaea, and have since drifted apart, explaining why similar mountain ranges can be found on separate continents. This evidence suggests that the movement of tectonic plates over time has led to the formation of mountains.
this is Fatima b. on wikianswers dot com; i don't know if this OK with my mom Don't listen to the answer above The real answer is that they support his idea because mountains are usually found by the coast of a continent.
this is Fatima b. on wikianswers dot com; i don't know if this OK with my mom Don't listen to the answer above The real answer is that they support his idea because mountains are usually found by the coast of a continent.
hello
The distribution of similar rock types and geological structures across distant mountain ranges supported Alfred Wegener's idea of continental drift. This suggested that the mountains were connected before the continents drifted apart, explaining their shared characteristics. Additionally, the alignment of mountain ranges on different continents provided evidence for the theory of plate tectonics, which explains how mountains form at convergent plate boundaries.
The distribution of mountain ranges across different continents, such as the Appalachian Mountains in North America and the Caledonian Mountains in Europe, supports Wegener's idea of continental drift. These mountain ranges were once connected when the continents were part of a supercontinent, and their alignment provides evidence for the movement of land masses over time. Additionally, the presence of similar geological features and rock formations on separate continents suggests a shared history of mountain building.
mountains usually occur in narrow bands along the edges of continents
The distribution of mountain ranges across different continents supports Wegener's idea of continental drift. He suggested that mountains form when two continents collide, pushing land masses upward. The presence of similar mountain ranges on different continents that were once joined together provides evidence for this theory.
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.