Ron paul 2012!
The Gulf Stream ring is formed when Gulf Stream meanders break off the Stream to create independent circulatory systems. Because of the formation of this ring, the warm tropical water from south of the Gulf Stream can be moved to north of the Gulf Stream.
the headward erosion hat brings about the formation of a river valley is an important factor in a process called stream piracy.
When a stream slows down, sediment that was previously being carried by the flow may begin to settle and accumulate on the streambed. This can lead to the formation of bars and pools within the stream channel. Additionally, slower flow rates can reduce the stream's ability to transport particles and nutrients downstream, affecting the overall ecosystem of the stream.
A meander is a curve or bend in a stream or river.
the uplift of the surrounding landmass. The stream erodes downward, carving a V-shaped valley, while the landmass rises due to tectonic movement. Over time, this combination results in the formation of V-shaped stream valleys.
The absolute age of a stream can be estimated using radiometric dating of rocks found along its path. By analyzing the isotopic composition of these rocks, scientists can determine when they formed and thereby establish the age of the stream. This method allows for accurate dating of the stream's formation based on the age of the rocks in its vicinity.
As an Alluvial stream stream approaches its base level, the discharge decreases, causing a reduction in velocity. This reduction in velocity leads to sediment deposition and the formation of a delta near the base level.
As a stream leaves a mountain range, it may encounter flatter terrain and lower elevations. This can lead to the formation of valleys, plains, or even wetlands, depending on the local geography. The stream may also start to meander and slow down as it transitions from its mountainous origins.
When stream flow decreases below the critical settling velocity of a certain size particle, the particle will settle out of the flow and deposit on the streambed. This process is known as sedimentation and can lead to the formation of sediment layers along the stream channel. Over time, these deposits can alter the shape and depth of the stream channel.
Chemical weathering, esp. in carbonate rocks, aided to some extent as the conduit develops by mechanical erosion by the stream.
Hydro-logic condition of the watershed area, current river and stream levels and soil moisture levels is how you can predict floods.