This is an open space Park in Jefferson County with both geological and cultural importance to the whole nation. This park has offered great and wonderful views for a long time.
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Most hikers and other outside fanatics have fun in deer Creek Park. Within the park compound there are various types of wild flowers especially the rainy seasons. Attractive views of the plains and the beautiful flowers, create a good photographic opportunities for the visitors (Hall 345). Most of people have preferred to visit this park due to its wide range of facilities that fits different types of visitors.
To begin with, the park has a wonderful and comfortable restroom facilities. Within its compound, the secluded areas for picnic are well secured with barbecue wires to ensure safety for the visitors. Both hikers and bikers are provided by multi purpose trails while climbing the mountain.
Any visitor to this park gets a chance to go through the park information, as there are information places equipped with brochures. The parks cleanliness is maintained through provision of many trashcans all over the place, thus it’s hard to see litter within the compound (Lipker 89).
The visiting time is relatively enough as the park is opened an hour before sunrise and its closed one hour after sunset. There are also attractive shelters within the compound and more beauty to the natural environments. The center of attraction lies in the presence of scrub oak habitat that is uncommon within that locality. In the park, wild animals enjoy oak as their food and their shelter. The atmosphere of the park is made wonderful by sweet melodies of different types of birds.
The most powerful force that is recognized in the formation of this park is erosion by water and wind. Other minor forces include Colorado River, volcanism, and climatic changes. Although this park is located in the desert, water also has a great impact during its formation. During the rainy seasons, the park soils do not absorb water as it is hardened completely by the strong sun (Yanagihara and Denniston 103).
When raining the water flows with force making the situation worse. The plants in the park have got shallow roots enabling them to absorb as much water as possible during the rainy seasons. On the other hand, these roots cannot control soil erosion as they are very weak and cannot hold the soil together.
The deer creek park occupies a big space approximately 1881 acre. In the beginning, its fertile soils attracted activities like mining and farming. Currently, people around the park also do a lot of hunting especially the deer that are common wild animals in the region. In the park, there are several well-managed trails that one can choose which to use (Hall 530).
Hiking trails are traveling paths inside the park. Some of the trails that are mostly used are Plymouth creek trail, Plymouth mountain trail, scenic view trail, and red mesa loop trail among others. The commonly used trail in deer Creek Park is meadowlark trail. This trail is estimated to have a length of one and a half miles. It’s a trail for pedestrian only although there are other that bikers can use. Through the help of residents around the park, the deer creek park has been able to offer protection and maintenance of wild animals and trees.
People from outside have also gotten an opportunity to be educated and conservation (Hlawaty, 210). The main aim of the deer creek park is to make use of that open space land as well as preserving natural resources. Some of the recreational activities that are conducted in the park include, luxury and family traveling where people enjoy themselves through trekking or by use of bikes.
Different types of sports, running and marathons have for a long time being conducted here especially the winter sports. During vacations visitors come in this park for leisure with their friends or family. Boating and sailing is also a common activity in this park especially when there are no water sports in progress.
The red rocks formed by the wind and water erosion are estimated to be 335 million years. These red rocks are formed by marine limestone and dolomites among other components (Samelson, et al 93). These red rocks are about 400 to 500 feet going upwards separating the lower and the upper sides of the deer creek park.
A slope for climbing these rocks is created where there is a crack. The strong and admirable red color is as a result of iron oxides from other layers as the original color of these rocks is dark brown. Some marine fossils are seen on these red rocks for instance snails, and fish among others. On these red rocks too caves and arches are also available.
In conclusion, the geological and the cultural aspects of the park have made it of value. Through these two people have learned, have funs, and enjoyed their leisure time well in the deer creek park. A lot of recreational activities have been organized and taken place in this park bringing people together (Lipker 113).
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This has contributed in promoting the social aspect of people and unity among them. The most surprising thing I observed in the park is the presence of the rattlesnakes, thus one has to be very careful when making a visit there. Weather conditions are also to be observed keenly when visiting, as there are several eruptions of the rocks due to contraction and expansion.
Hall, Frank. History of the State of Colorado, Volume 2, ISBN1110812094, 9781110812097, BiblioBazaar, LLC, New York, 2009. Web.
Hlawaty, Stephen. Mountain Biking Colorado’s Front Range: From Fort Collins to Colorado Springs, ISBN0762725559, 9780762725557, Falcon, New York, 2003.
Lipker, Kim. 60 hikes within 60 miles, Denver and Boulder: including Colorado Springs, Fort Collins, and Rocky Mountain National Park, ISBN089732627X, 9780897326278, Menasha Ridge Press, Birmingham, 2006.
Samelson, Jenna, et al. Colorado Campgrounds: The 100 Best and All the Rest, (3rded), SBN156579334X, 9781565793347, Big Earth Publishing, Colorado, 200I.
Yanagihara, Wendy and Denniston, Jennifer. Grand Canyon National Park, (2nd ed), ISBN1741044839, 9781741044836, Lonely Planet, Adelaide, 2008.