The stream at Karnala Bird Sanctuary in India can be considered constructive, as it plays a vital role in sustaining the local ecosystem. It provides essential water resources for flora and fauna, supports biodiversity, and contributes to the overall health of the sanctuary. Additionally, the stream enhances the scenic beauty of the area, attracting visitors and promoting eco-tourism, which can further aid conservation efforts.
No, a flood can not be destructive and constructive, but it can be destructive.I think Egyptians would disagree. The country of Egypt flourished for millennia because the annual flooding of the Nile deposited fertile soil on top of the Saharan sand.A small flood, like a river one, will only damage basements. Things stored there will get wet and waterlogged, the floors will get really really yucky. Big things like tsunamis make people drown and destroy houses.
The jet stream
Stream gradient, or the slope of the stream channel, affects stream velocity by influencing the speed at which water flows downstream. A steeper stream gradient typically results in a faster water flow velocity, as the force of gravity pulls water downhill more strongly. Conversely, a gentler stream gradient leads to slower water flow velocity.
The mouth of a stream is where it meets a larger body of water, such as a lake, ocean, or another stream. It is where the stream's water flows out and mixes with the water of the larger body.
A continental jet-stream travels parallel to the equator - a polar jet-stream travels in a north/south direction.
No, a flood can not be destructive and constructive, but it can be destructive.I think Egyptians would disagree. The country of Egypt flourished for millennia because the annual flooding of the Nile deposited fertile soil on top of the Saharan sand.A small flood, like a river one, will only damage basements. Things stored there will get wet and waterlogged, the floors will get really really yucky. Big things like tsunamis make people drown and destroy houses.
When Hurricane Hugo hit the Gulf Stream in 1989, it intensified due to the warm waters of the current. The storm's wind speeds and size increased, leading to more destructive impacts along the U.S. East Coast.
Once a cave passage is abandoned by its formative stream, it can become: - Choked with sediments deposited by the dying floods of that stream or brought in by glacial thaw (Gaping Gill, in NW England, holds vast quantities of glacial till out of erosive reach of the present stream). - Richly decorated with stalagmites and stalactites (these won't grow under water). - Filled with boulders falling from roof and walls as ground-water seeping through the joints in thelimestone above it, dissolves the rock enough to weaken the structure: a destructive rather than constructive act of the same process that initiated the cave.
Interference in light waves occurs when two or more waves overlap and combine. Constructive interference happens when the waves align to increase the amplitude, resulting in a brighter light. Destructive interference occurs when the waves are out of phase and cancel each other out, leading to a darker area called a node.
A mature stream.
A stream bed is the bottom (floor) of the stream.
Art stream
The stream reach is the length of the stream you have selected for monitoring.
The Limpid Stream was created in 1935.
It is occasionally called a sinking stream or a disappearing stream, but geographers and geologists normally call it a stream, just like another stream.
Lowering a stream's base level will cause the stream to do what?
an old stream is a deep wide and curvy river stream