The Fred H Divoky Trail System, situated in the heart of the Great Plains in Holdrege, Nebraska, offers a unique hiking experience for those looking to immerse themselves in the region's natural landscape. A notable aspect of this trail system is its tendency to undergo prolongation, a geological process in which streams and rivers continue to flow and erode the surrounding terrain, creating unique features such as meanders and oxbow lakes.

One notable example of prolongation at the Fred H Divoky Trail System can be seen in the North Platte River, which flows through the nearby city of Ogallala. The river has created a series of meanders, or curved stretches of river, which are visible from the trail system. These meanders demonstrate the process of prolongation, as the river's flow is constantly eroding the surrounding terrain and creating new paths.

The prolongation process at the Fred H Divoky Trail System is also influenced by the region's geology. The area is part of the Cretaceous Western Interior Seaway, a ancient sea that once covered the region. The trail system sits atop a layer of fossilized sand, which is more easily eroded by the wind and water. This erosion creates a landscape of rolling hills and deep valleys, which are characteristic of the Great Plains.

As one explores the Fred H Divoky Trail System, it becomes clear that the process of prolongation is not limited to the North Platte River. Smaller streams and creeks, such as the Platte River's tributary, Turkey Creek, also demonstrate this geological process. Turkey Creek, which flows through the nearby city of Sutherland, has created a series of small meanders and oxbow lakes, which are visible from the trail system.

The prolongation at the Fred H Divoky Trail System is also influenced by human activity. The construction of the Kingsley Dam, located just north of the trail system, has altered the flow of the North Platte River, leading to increased erosion in some areas and decreased erosion in others. This alteration has caused a shift in the landscape, as sand and sediment are deposited in new areas.

The Fred H Divoky Trail System offers a unique opportunity to see the process of prolongation in action. By exploring the trail system and observing the North Platte River and its tributaries, visitors can gain a deeper understanding of this geological process and its role in shaping the Great Plains landscape.