User:Nonkululeko Morgan/sandbox

I am interested in soil conditions and more specifically soil erosion and its affect on the landform via rejuvenation etc. I might be interested in exploring that for research paper/

I am also interested in weather and ways that it affects landform. extreme conditions as well as normal everyday weather like rain or drought and how they affect the form of the landscape

Week6

Building on these ideas of erosion and weathering I thought it would be really interesting to write an architecture on the process of rejuvenation which, briefly, is the process whereby changes in weather or sea level cause a drop in a rivers bed. This results in drastic vertical erosion, steeper valleys, and faster rivers. This affects the form of the landscape overtime. With this article, I am hoping to explore ways in which the rejuvenation process affects rivers and landscape form and function.

I found one short wikipedia article on the process but would use more contributions

In geomorphology a river is said to be rejuvenated when it is eroding the landscape in response to a lowering of its base level.

Signs
Rejuvenated terrains are usually have complex landscapes because remnants of older landforms are locally preserved. Parts of floodplains may be preserved as terraces along the downcutting stream channels. Meandering streams often become entrenched, so a product of older river systems is found with steep, very pronounced "V" shaped valleys - often seen with younger systems.

Example
One example of rejuvenation is the Nile, which was rejuvenated when the Mediterranean Sea dried up in the late Miocene. Its base level dropped from sea level to over 2 miles below sea level. It cut its bed down to several hundred feet below sea level at Aswan and 8000 feet below sea level at Cairo. After the Mediterranean re-flooded, those gorges gradually filled with silt.

Causes
Rejuvenation may result from causes which are dynamic, eustatic or isostatic in nature. All of these cause the river to erode its bed vertically (downcutting) faster as it gains gravitational potential energy. That causes effects such as incised meanders, steps where the river suddenly starts flowing faster, and fluvial terraces derived from old floodplains.

Dynamic rejuvenation
A region may be uplifted at any stage. This lowers the base level and streams begin active downward erosion again.

Dynamic rejuvenation may be caused by the epeirogenic uplift of a land mass. Warping or faulting of a drainage basin will steepen the stream gradient followed by the downcutting. The effect of seaward tilting can be felt immediately only when the direction of that stream is parallel to the direction of tilting.

Eustatic rejuvenation
Eustatic rejuvenation results from worldwide decrease in sea level, and two types of such rejuvenation are recognized. Diastrophic eustatism is the change in sea level due to variation in capacity of ocean basins, whereas glacio-eustatism is the change in sea level due to withdrawal or return of water into the oceans, due to the accumulation or melting of successive ice sheets.

Eustatic rejuvenation relocates the mouth of the stream. Regrading of a stream toward a new lower base level will proceed upvalley. The result may be an interrupted profile with the point of intersection of the old and new base levels.

Static rejuvenation
Three changes may bring static rejuvenation, to the stream. Rejuvenation due to decrease in load took place during post-glacial times along many valleys that formerly received large quantities of glacial outwash. With change to no glacier conditions stream load decreased and valley deepening ensued.
 * 1) decrease in load
 * 2) increase in runoff because of increased rainfall
 * 3) increase in stream volume through acquisition of new

Rejuvenation may result in a "knickpoint", as it appears on a river profile, which often appears as a rapids or a waterfall. An example is Seljalandsfoss in southern Iceland, where isostatic (dynamic) uplift has occurred as a result of both construction and deglaciation.

Static rejuvenation may also occur, in rare instances, when a downstream knickpoint erodes its way upstream to a lake which establishes base level for its tributaries. When the knickpoint reaches the lake, the lake drains, and the base level of upstream waters lowers rapidly from that of the (now former) lake to that of the river downstream of the knickpoint. At some point in the future, a quite dramatic example will appear when Niagara Falls cuts its way back to Lake Erie.