Which geological feature is primarily created by sea floor spreading?

Which geological feature is primarily created by sea floor spreading?

• A. Mid-ocean ridges
• B. Mountain ranges
• C. Volcanoes
• D. Continental shelves

Answer: (A)

Sea floor spreading is a geological process that occurs at mid-ocean ridges, where tectonic plates move apart, allowing magma from the mantle to rise and create new oceanic crust. This process is responsible for the formation of mid-ocean ridges, which are underwater mountain ranges characterized by volcanic activity and the presence of rift valleys. As the plates diverge, the continuous upwelling of magma results in the elongation and elevation of these ridges, contributing to the overall topography of the ocean floor. In contrast, while mountain ranges and volcanoes can result from tectonic activity, they are typically associated with continental collision or subduction zones rather than sea floor spreading itself. Similarly, continental shelves are the submerged edges of continents and are not directly formed by the mechanisms driving sea floor spreading. Thus, the unique formation of mid-ocean ridges is a direct consequence of the processes involved in sea floor spreading.

Sea floor spreading is a geological process that occurs at mid-ocean ridges, where tectonic plates move apart, allowing magma from the mantle to rise and create new oceanic crust. This process is responsible for the formation of mid-ocean ridges, which are underwater mountain ranges characterized by volcanic activity and the presence of rift valleys. As the plates diverge, the continuous upwelling of magma results in the elongation and elevation of these ridges, contributing to the overall topography of the ocean floor.

In contrast, while mountain ranges and volcanoes can result from tectonic activity, they are typically associated with continental collision or subduction zones rather than sea floor spreading itself. Similarly, continental shelves are the submerged edges of continents and are not directly formed by the mechanisms driving sea floor spreading. Thus, the unique formation of mid-ocean ridges is a direct consequence of the processes involved in sea floor spreading.