Actually when the flow emerges from the throat area of venturi to enter into the diverging section, their is a negative pressure gradient i.e, in layman terms fluid is trying to flow from low pressure region to high pressure region according to Bernoulli equation. In this adverse pressure gradient, there is boundary layer separation, in simple terms, the fluid leaves the surface of the wall. Due to this there can be energy loss or the fluid can't recover the pressure fully leading to head loss. So if divergent section is long that means more gradual diverging section, due to which the adverse pressure gradient is less so less chance of boundary separation and hence less loss. Also large diverging section will ensure proper development of flow, i.e. fluid sticking to the wall back after separation.
The Ol Doinyo Lengai volcano is located in Tanzania near the East African Rift, which is a divergent boundary where tectonic plates are moving away from each other. This rift is part of the larger East African Rift System, where new crust is being formed as the African Plate splits into the Nubian Plate and the Somali Plate.
At a constructive (divergent) plate boundary, new crust is being created to infill the gaps caused by spreading plates. At a destructive (subduction-convergent) plate boundary, old, dense oceanic crust is diving into, and becoming part of the mantle.
Divergent is another word for coming apart. If something diverges it comes a part.
It is a transform boundary.
Subduction
Some similarities between convergent and divergent boundaries are that both create faults that are capable of producing earthquakes; both are tectonic plates; and both are part of the lithosphere.
The Ol Doinyo Lengai volcano is located in Tanzania near the East African Rift, which is a divergent boundary where tectonic plates are moving away from each other. This rift is part of the larger East African Rift System, where new crust is being formed as the African Plate splits into the Nubian Plate and the Somali Plate.
Mount Pelee is located on a convergent plate boundary. The volcano is part of the Lesser Antilles volcanic arc, which is formed by the subduction of the North American Plate beneath the Caribbean Plate.
At a constructive (divergent) plate boundary, new crust is being created to infill the gaps caused by spreading plates. At a destructive (subduction-convergent) plate boundary, old, dense oceanic crust is diving into, and becoming part of the mantle.
Divergent means to divert away from the main stream. To think in a divergent way would be to think outside of the box. Differently, part ways, be different.
convergent
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Divergent is another word for coming apart. If something diverges it comes a part.
a constructive (divergent) plate boundary, new crust is being created to infill the gaps caused by spreading plates. At a destructive (subduction-convergent) plate boundary, old, dense oceanic crust is diving into, and becoming part of the mantle.Read more: What_is_the_difference_between_a_constructive_plate_boundary_and_a_destructive_plate_boundary
They are where mid-ocean ridges occur. Island arcs are common features of convergent boundaries where two ocean plates meet. The boundary where two plates slide past each other, is a transform boundary. The density of the plates, is important at subduction zones, where the denser plate sinks below the less-dense plate, which is also a feature of convergent plates. Tectonic plates are part of the lithosphere, which floats on the asthenosphere.
It is a transform boundary.
By center slit I assume that you mean a mid ocean ridge which is a divergent boundary and the sea floor is very young there. Then be side slit I am assuming that you mean a trench which is a convergent boundary or subduction zone which would be the oldest part of the sea floor.