A bluff or bank.
the oak ridges
An eskers
An esker is formed by the deposition of sediments carried by meltwater from a retreating glacier. As the glacier melts, the sediment is deposited in a sinuous ridge-like formation. Eskers are typically composed of sand and gravel.
The youngest sediments found near the Mid-Atlantic Ridge are typically associated with the oceanic crust formed at the ridge itself, which is less than a few million years old. These sediments primarily consist of pelagic clay, biogenic material, and volcanic ash, accumulating as the seafloor spreads. The rate of sedimentation is relatively low, meaning that the youngest sediments are generally found closest to the ridge and become progressively older with distance from it.
Sediments become thicker away from the mid ocean ridge. This is because the oceanic crust away from the mid ocean ridge is older than the crust close to it, so sediment has had more time to accumulate.
Moraine.
Yes, an esker is a sinuous ridge formed by sediment deposited by meltwater flowing through a channel or tunnel within glacial ice. As the glacier retreats, the meltwater carries sand and gravel, which accumulate in the channel. Once the glacier has melted away, the remaining ridge of sediment is exposed, creating the distinctive landform known as an esker.
yes
The sediments found on the ridge of the ocean floor are primarily known as "pillow lavas" and "basaltic sediments." These sediments are formed from volcanic activity, where magma erupts and cools rapidly upon contact with seawater, creating pillow-shaped formations. Additionally, hydrothermal vent deposits and other sediment types, such as biogenic and pelagic sediments, can also be present in these regions.
Such ridges are referred to as lateral moraines. As a glacier moves, it shears debris, such as rock and soil, on both sides, and this unsorted sediment forms ridges along the edges of the glacier.
It is known as moraine.
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