A deep sea fan
sedimentary
A good example would be the ones in Death Valley, California. An alluvial fan is basically a fan-like structure formed from the mouth of a flattened and spread out stream (it looks like a fan).
it's purpose is for partying and farting in your mouth when you least expect it
Their mouth because of suliva left in it.
According to a documentary done by National Geographic on the Lower Congo River Basin, there are recorded depths of over 755 ft (230 meters) in the deepest trench of the Congo River. The lead scientist that headed this team said that it is well over the deepest river in the world.
yes a mouth can be a sea feature .
"head" is where it starts, the mouth is the outlet.
No. The mouth is the feature, a smile is an "expression".
A general deep area of the ocean will be called an abyssal deep, but a canyon-like structure will also be called a submarine canyon. e.g. the Clutha Submarine Canyonoff the mouth of the Clutha River on the east of New Zealand's South Island.Off the Kaikoura Peninsula, however is the Hikurangi Trench, a cleft-like canyon which has a relationship with subduction processes, not riverine. This Trench is over 3000 m deep.This structure continues broadly northwards to become the Tonga Trench in that vicinity.
Submarine canyons are steep-sided valleys cut into the continental slope, often by turbidity currents, while deep-ocean trenches are long, narrow, and deep troughs formed at subduction zones where tectonic plates collide. Submarine canyons are typically shallower and closer to the continental shelf, while deep-ocean trenches are deeper and associated with seafloor subduction.
Mr.Mull has 3 children living by a canyon mouth in Alaska.
no
A "holler" is Appalachian-Mountain dialect for "hollow," or a deep mountain canyon. Most mountain dwellers lived in the hollows instead of on the windy peaks, and you'd go "up the holler" to visit your neighbors. The "mouth" of a hollow would be the broad entrance to the canyon.
sedimentary
Delta
The Grand Canyon was formed mainly due to the Colorado river, and also due to uplift pronouncing the scale of the canyon; it is not formed due to a delta, as deltas are only formed at the mouth of the river, not in its middle course.
A good example would be the ones in Death Valley, California. An alluvial fan is basically a fan-like structure formed from the mouth of a flattened and spread out stream (it looks like a fan).