In terms of divergence, a rift valley is comparable as it is formed by two areas moving apart, causing the land between them to fall (though this looks nothing like a ridge). This, however, does not directly resemble a ridge, but in principal it is similar.
In appearance, a mountain range like the Himalayas may be seen to resemble the shape and peaks of the ridge.
Oceanic ridge
Mid Ocean Ridge
mid ocean ridge
usually a rift or trench
mid ocean ridge
The prominent sea floor feature found in the central Atlantic ocean is called the Mid Atlantic Ridge.
A ridge is a geological feature that features a continuous elevational crest for some distance. If the ridge is under the ocean or sea, then it is called a submarine ridge.
The ocean floor feature that consist of chains of individual volcanoes is called mid ocean ridges. This ridge can rise from 1 to 3 kilometers above the ocean basin.
The Mid-Ocean Ridge is the longest topographic feature on Earth's surface, stretching over 65,000 kilometers around the globe. It is a continuous underwater mountain range that winds through all the major oceans.
A mid-ocean ridge is a crustal feature formed by divergent plate movement. This occurs when tectonic plates move apart, allowing magma to rise to the surface, creating new oceanic crust.
Feature B in figure 9-1 appears to be the "Power button" on the device.
Yes, there is a valley in the center of the mid-ocean ridge called the rift valley. It is formed due to tectonic plates diverging and magma rising to create new oceanic crust. The rift valley is a significant feature of the mid-ocean ridge system.