The expanses of dry mud comprised of various mountainous features ( Kaliraj et al., 2015) . The Death valley, found in California is composed of dry mud was one of eh features that covered a larger percentage of the area. It was evident that the mud that was around the place was as a result of the infrequent rainfall patterns and extreme temperatures.
Additionally, the dry mud that was spread throughout the region was fine in nature with shallow tracks. The rock’s paths on the other hand were formed when the rainfall generated a shallow lake, which instead generated a thin layer of freezing ice ( Kaliraj et al., 2015) . Notably, the mud might also have been formed as a result of erosion of the bedrocks by the waves through the process known as abrasion.
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The area that we visited was characterized by various features that were majorly modified through the action of erosion, extreme temperatures and melting ice ( Kaliraj et al., 2015). There were remnants that come from the action soft the waves making the dispatch from a horizontal wave-cut platform. The remaining sediments lead to the formation of sea stacks that gives the Death Valley landscape a spectacular landform. However, the pinnacle that has been formed will not stay for a long time as smooth-cut wave surface because erosion is a continuous process and will eventually erode the feature with time until no traces of the feature will be evident ( Kaliraj et al., 2015 .
While still surveying the Death Valley as the chosen site, there was a delta that was formed at the mouth of a river that resulted from an accumulation of sediments ( Łabuz, 2015). The feature was formed because the actions of the waves were slower than the rate at which the sediments were deposited by the melting ice ( Łabuz, 2015) . Additionally, the area had a gently sloping continental shelf, a factor that facilitated the formation of the delta because the feature needs a shallow site to allow deposition of the sediments.
References
Kaliraj, S., Chandrasekar, N., & Magesh, N. S. (2015). Evaluation of coastal erosion and accretion processes along the southwest coast of Kanyakumari, Tamil Nadu using geospatial techniques. Arabian Journal of Geosciences , 8 (1), 239-253.
Łabuz, T. A. (2015). Environmental impacts—coastal erosion and coastline changes. In Second Assessment of Climate Change for the Baltic Sea Basin (pp. 381-396). Springer, Cham.
