Sand Creek (Wyoming)

In this article, we will delve into the exciting world of Sand Creek (Wyoming), exploring its multiple facets, meanings and relevance in today's society. Sand Creek (Wyoming) has been the subject of interest and debate throughout history, being a topic that has resonated in different areas and contexts. From its origins to its influence today, we will examine its impact on different aspects of life, from the personal to the global level. Through a detailed and rigorous analysis, we will seek to understand in depth what Sand Creek (Wyoming) is and why it is so important, offering a panoramic vision that invites reflection and knowledge.

Sand Creek
Physical characteristics
Source 
 • locationLaramie Mountains
 • coordinates40°49′46″N 105°47′04″W / 40.82944°N 105.78444°W / 40.82944; -105.78444
Mouth 
 • location
Confluence with Laramie
 • coordinates
41°12′56″N 105°43′52″W / 41.21556°N 105.73111°W / 41.21556; -105.73111
 • elevation
7,185 ft (2,190 m)
Designated1984

Sand Creek is a stream noted for the "most spectacular examples of cross-bedded sandstone and topple blocks in North America". Sand Creek flows from the Laramie Mountains in Larimer County, Colorado into Albany County, Wyoming where it joins the Laramie River.

The area where Sand Creek crosses the border between Colorado and Wyoming (40°59′49″N 105°46′14″W / 40.99694°N 105.77056°W / 40.99694; -105.77056) was designated a National Natural Landmark in 1984.

See also

References

  1. ^ a b "Sand Creek". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2011-01-26.
  2. ^ a b "National Registry of Natural Landmarks" (PDF). National Park Service. June 2009. p. 109. Retrieved 2011-08-04.

External links

"Sand Creek National Natural Landmark". National Park Service.