Stop trying to cheat on ur homework
Midocean ridges are areas where continents broke apart. Midocean ridges are closest to the landmasses in younger oceans. One example where a midocean ridge intersected a landmass is the Arabian sea, which was formed by the pulling apart of the Arabian Peninsula and Africa.
Oceanic plates typically touch at mid-ocean ridges, where new oceanic crust is formed as magma rises from the mantle and solidifies. Additionally, oceanic plates can also interact at subduction zones, where one plate is forced beneath another, leading to the formation of deep ocean trenches and volcanic activity.
Yes, sonar and magnetometer data have been instrumental in the discovery of ocean ridges and deep-sea trenches. Sonar data is used to map the sea floor topography, revealing ocean ridges, while magnetometer data helps identify variations in the Earth's magnetic field caused by stripes of rock on the ocean floor, contributing to understanding plate tectonics and the formation of deep-sea trenches.
One of the midocean ridges is, but others are in other oceans, seas, and bays.
The floor of the ocean is called the seabed or ocean floor. It is made up of different features such as abyssal plains, trenches, ridges, and volcanoes.
Stop trying to cheat on ur homework
Midocean ridges are areas where continents broke apart. Midocean ridges are closest to the landmasses in younger oceans. One example where a midocean ridge intersected a landmass is the Arabian sea, which was formed by the pulling apart of the Arabian Peninsula and Africa.
At transform faults or transform zones.
Oceanic plates typically touch at mid-ocean ridges, where new oceanic crust is formed as magma rises from the mantle and solidifies. Additionally, oceanic plates can also interact at subduction zones, where one plate is forced beneath another, leading to the formation of deep ocean trenches and volcanic activity.
Yes, sonar and magnetometer data have been instrumental in the discovery of ocean ridges and deep-sea trenches. Sonar data is used to map the sea floor topography, revealing ocean ridges, while magnetometer data helps identify variations in the Earth's magnetic field caused by stripes of rock on the ocean floor, contributing to understanding plate tectonics and the formation of deep-sea trenches.
One of the midocean ridges is, but others are in other oceans, seas, and bays.
They are called oceanic trenches.
The floor of the ocean is called the seabed or ocean floor. It is made up of different features such as abyssal plains, trenches, ridges, and volcanoes.
realate the high tempertures measured at the mid-ocean to the formation of basalt at the ridges
Older, as it moves away from the mid-ocean ridge the sediment gets thicker and older
Mid-ocean ridges are the birthplace of oceanic crust. Trenches represent the destruction and burial of oceanic crust. They are at opposite ends of the Earth's convection currents that move through the asthenosphere.
Two geological features that can occur at plate boundaries are mountain ranges, formed from the collision of two plates, and deep ocean trenches, formed at subduction zones where one plate is forced beneath another.