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What is a long ridge of sediments deposited alongside a river channel called?
the oak ridges
What is it called when long ridges of sediments alongside the channel of a river?
I assume you mean levees, which are caused by deposition from successive floods.
What are long ridges of sediment alongside the channel of a river?
it is a levee
Long ridges of sediment alongside the channel of a river are called?
Levees. They are built up by the deposition of sediment during flood events, which causes the river channel to become elevated above the surrounding floodplain.
What are the ridges in cerebrum called?
The ridges in cerebrum are called
What are sediments at deep ocean ridges?
Sediments at deep ocean ridges primarily consist of fine-grained particles, including clays, silts, and biogenic materials like foraminifera and diatoms. These sediments accumulate slowly over time due to the low rates of sedimentation in the deep ocean environment. Additionally, hydrothermal activity at these ridges can influence sediment composition by altering minerals and introducing materials from the Earth's mantle. Overall, the sediments reflect both the biological activity and geological processes occurring in these dynamic underwater landscapes.
What are Ridges in the cerebrum?
The ridges in cerebrum are called
Ridge consisting of unsorted sediments deposited at the sides of a glacier?
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.
Does a milled coins have ridges?
Yes - the ridges are called milling, or reeding.
How are ridges formed on the ocean floor?
Ocean current paths of travel, underwater volcanoes, tectonic plate movement, depends which specific ridges you are talking about.
A dime has what kind of ridges around the edge?
The ridges around the edge of a dime is called reeding or milling. There are 118 ridges.
What are mounds or ridges of till?
Mounds or ridges of till are glacial landforms formed when glaciers deposit large quantities of unsorted sediments, called till, as they advance and retreat. These features can take various shapes and sizes and are typically found in areas where glaciers have recently melted or receded, highlighting the glacier's path of movement.
