Consider the following statements: Obsequent streams flow in a dir...
Option (c) is the correct answer.
Under classification of streams:
Statement 1 is correct. Obsequent streams flow in a direction opposite to that of the original consequent slope.
A consequent river is one whose course is determined by the original course of the land.
Statement 2 is correct. Resequent rivers are those that flow in the same direction as the consequent stream but at a lower level.
Consider the following statements: Obsequent streams flow in a dir...
The correct answer is option C, which states that both statements 1 and 2 are correct.
1. Obsequent streams flow in a direction opposite to that of the original consequent slope:
- Obsequent streams refer to the tributaries that flow in a direction opposite to that of the main river or the consequent stream. These streams form when the main river cuts across a ridge or a mountain and the tributary streams flow away from the main river.
- This phenomenon occurs due to the difference in the geological structure of the area. When the main river erodes through a ridge, it creates a deep valley or a gorge. The tributary streams that develop on either side of the ridge flow in the opposite direction, away from the main river.
- Obsequent streams are commonly found in regions with complex geological features, such as mountainous areas or areas with folded or faulted rock formations.
2. Resequent rivers are those that flow in the same direction as the consequent stream but at a lower level:
- Resequent rivers are formed when the tributary stream joins the main river at a lower elevation, but still flows in the same direction as the main river or the consequent stream.
- This occurs when the tributary stream develops on a relatively lower slope or a lower order stream, and it eventually merges with the main river. However, the tributary stream maintains its direction of flow parallel to the main river.
- Resequent rivers are commonly found in areas with a gentle slope or in regions where the main river has already established its course.
In summary, obsequent streams flow in the opposite direction to the main river or consequent stream, while resequent rivers flow in the same direction but at a lower level. Both phenomena occur due to the geological characteristics of the area and are observed in different types of landscapes.