the three puzzling occurrences that helped to support the theory was when the southern tips of south american and Africa do not touch
2 they did not touch in the past
over time earths continents have changed shape and traveled great distances
i was looking at a wks in class on this but hey im in seventh grade so you can trust me or not on this but here u go
The three possible combinations of plate collisions at convergent boundaries are oceanic-oceanic, oceanic-continental, and continental-continental. In each case, one plate is subducted beneath the other due to the difference in density, leading to the formation of features such as trenches, volcanic arcs, and mountain ranges.
Each of the plates may be oceanic or continental. That gives three possibilities:oceanic - oceanicoceanic - continentalcontinental - continental.
Oceanic-continental: Oceanic plate is subducted beneath continental plate, creating volcanic arcs and mountain ranges. Oceanic-oceanic: One oceanic plate is subducted beneath another, forming deep ocean trenches and volcanic island arcs. Continental-continental: Collision of two continental plates, leading to intense folding and faulting, creating high mountain ranges.
The three stems of traditional organizational theory are classical, neoclassical, and modern. Classical theory emphasizes rationality, efficiency, and hierarchy. Neoclassical theory focuses on the importance of human behavior and motivation within organizations. Modern theory includes various perspectives such as contingency theory, systems theory, and organizational ecology.
Oceanic-Oceanic, Oceanic-Continental, and Continental-Continental are all sub types of convergent plate boundaries.
The distribution of fossils of the same species across continents provided evidence of past connections between continents, supporting Wegener's theory of continental drift. The matching geological features on opposite coastlines of continents suggested they were once connected and later drifted apart, which aligns with Wegener's theory. The jigsaw-like fit of the continents' coastlines, particularly on the Atlantic Ocean, offered a strong visual representation of how continents could have been joined and later separated, supporting Wegener's theory of continental drift.
Wegener used evidence from fossils, rock formations, and the fit of the continents as key components to develop his theory of continental drift. By studying these factors, he proposed the idea that all continents were once part of a single supercontinent called Pangaea.
The three parts of the continental margins are the Continental shelf, the Continental slope, and the Continental rise.
wheathering,erosion and cementing
The three parts of the continental margins are the Continental shelf, the Continental slope, and the Continental rise.
The three possible combinations would be continental-continental, continental-oceanic, and oceanic-oceanic.
the three date theory is a theory that after 3 dates the girl will put out.
The theory of plate tectonics has succumbed to the newer theory of continental drift. Scientists believe this theory today due to three main factors. First, the continents appear to fit together. When the continental shelves, as opposed to just the continents, are placed together, the fit appears uncanny. Second, the distribution of fossils is consistent with continental drift. Lastly, glacial deposits once covered parts of the earth that are currently tropical.ANSWER: The plate tectonics theory is relatively new and formulated only in the 1960s. The evidence listed above in the first answer can only support the continental drift theory which was developed by Alfred Wegener in 1912. Evidence that can support the plate tectonics theory are the age, depth of oceanic sediments, volcanic activity, geothermal gradient, gravity anomalies, paleomagnetism and seismologic evidence. If you are answering an exam question on evidence supporting plate tectonics, evidence supporting continental drift theory should only come later in your answer and should not be given too much emphasis, for the plate tectonics theory involves more than just the continental crust drifting around and cannot support the main hypotheses of the plate tectonics theory.
the three date theory is a theory that after 3 dates the girl will put out.
The three parts of the continental margin are the continental shelf, continental slope, and continental rise. The continental shelf is the gently sloping, submerged platform of a continent that extends from the shoreline to the shelf break. The continental slope is a steeper zone that descends from the shelf break to the deep ocean floor. The continental rise is the final gently sloping seafloor region at the base of the continental slope.
Continental shelf, continental slope, continental rise and abyssal plain. The first three make up the continental margin.
Yes, the Himalayas are located on a convergent boundary.There are three types of convergent boundaries:-Oceanic-Oceanic-Oceanic-Continental-Continental-ContinentalOf the three types, the Himalayas are considered to be Continental-Continental. Meaning, it's a collision between two continental plates.