Seamounts
The three lines of evidence for Plate Tectonics are: 1) the distribution of earthquakes and volcanoes along plate boundaries, 2) the matching shapes of continents on opposite sides of the Atlantic Ocean, known as continental drift, and 3) the patterns of magnetic striping on the ocean floor that provide evidence of seafloor spreading.
New crust forms on the ocean floor through seafloor spreading, where magma rises up from the mantle through mid-ocean ridges and solidifies into new crust as tectonic plates move apart.
The ocean floor topography includes features like mid-ocean ridges, trenches, abyssal plains, seamounts, and continental shelves. These features are shaped by processes such as plate tectonics, volcanic activity, and erosion. Mapping the ocean floor is crucial for understanding marine ecosystems, climate patterns, and natural hazards.
Technological methods used to prove plate tectonics include GPS to measure crustal movement, seafloor mapping to show oceanic spreading, satellite imagery to monitor surface changes, and seismic tomography to visualize Earth's interior structures. These methods provide evidence for plate motion and interactions, supporting the theory of plate tectonics.
Two topographic features of the ocean floor discovered with sonar are underwater mountain ranges known as mid-ocean ridges and deep ocean trenches. Sonar technology allowed scientists to map these submarine structures and gain insights into plate tectonics and the Earth's geology.
what material forms new pieces of ocean floor
They change its size and shape.
Plate tectonics and (river) erosion are responsible for the formation of ocean-floor features.
Plate tectonics and (river) erosion are responsible for the formation of ocean-floor features.
Plate Tectonics, to put it simply.
*of, sorry
they found fossils
New material forms on the ocean floor of the mid-ocean ridge due to plate tectonics and volcanic activity. Volcanic eruptions deposit cooled magma on the ocean floor.
New material forms on the ocean floor of the mid-ocean ridge due to plate tectonics and volcanic activity. Volcanic eruptions deposit cooled magma on the ocean floor.
Marie Tharp's contribution to plate tectonics was the creation of the first scientific map of the ocean floor that revealed the existence of a mid-ocean ridge and deep-sea trenches. Her mapping work provided critical evidence in support of the theory of continental drift and plate tectonics.
plate tectonics
The features of the ocean floor, such as mid-ocean ridges, deep-sea trenches, and underwater volcanoes, provide evidence for the theory of plate tectonics. These features are formed by processes like seafloor spreading, subduction, and volcanic activity, which are central to the movement of Earth's tectonic plates. Additionally, the magnetic striping pattern on the ocean floor supports the idea of seafloor spreading and plate movement over time.