Traveling through Western Nebraska's Unique Badlands
Western Nebraska, part of the Great Plains region, boasts a unique and rugged area known as the Sandhills and the underlying Niobrara River's badlands. This region stretches across the northwestern part of the state, covering approximately 40 miles of rugged terrain near the Wyoming border, and approximately 50 miles from the town of Crawford, south to Ainsworth, within Brown County. The primary access point to this area is the Toadstool Geologic Park and the Hudson-Meng Bison Kill Site, operated by the University of Nebraska-Lincoln.
One of the most distinct aspects of this area is the unique geology. Formed as an eroded Pleistocene fossil lake bed known as the Ash Hollow Formation, this site has preserved a large assemblage of Pliocene and Pleistocene fossilized remains, including unique toadstool-shaped rock formations. Hudson-Meng, also within this unique geologic formation, showcases archaeological evidence of human hunting activities around 10,000 years ago. Excavations have led to the discovery of the butchered remains of hundreds of bison.
These sites serve not only as educational and research tools for archaeologists and geologists but also as an opportunity for visitors to observe this natural area. Visitors can participate in fossil hunting, exploring over 45 different distinct geological sites. It's imperative to keep in mind, several potential hazards lurk within the paths, due to weather conditions such as flooding and very rapid high winds.
One great risk of the formations near Crawford found within these badlands, is rapid evaporation after the heavy storms wash away minerals which leave relatively more erosive elements (mainly uncompressible granular sands with a very loose interlocking framework like coarse unsealed granular road surface). Human erosion management has led to attempts to reduce or manage habitat and surface degradation, thereby enabling an optimal experience for the observing visitor in safe environmental conditions.
Given that human settlements remain sparse within areas with such soil composition, the vegetation experienced much less intense, human-driven deforestation efforts in recent history and so conservation is relatively simple. However there exist some concerns that environmental risks need more stringent conservation management such as strict rules regulating trail off-roading, etc, many of which need further conservation solutions that manage environmental impact as well such as a risk profile that forewarned land manager responsibilities while always performing conservation value for important wildlife.
As you explore this distinct geologic setting, make certain to not forget the unique plant species located throughout this badlands area, mainly vegetation such as black oak trees (commonly Quercus velutina) the sideoats grama grass (Bouteloua curtipendula) shortgrasses, tallgrasses, and needlelike grass such as needle and thread (Hesperostipa comata) grasses. Rock formations, fossils of long-gone bison, other wildlife such as animals found were eventually replaced by roaming wolves, rodents etc have now been left to roam free as geologically adapted animals through shifting tectonic-plate activities being then understood through processes.
It therefore remains important to take necessary precautions when you explore the very unique area full of these beautiful sightseeing areas that may give significant educational insights that are geologically true but also incredibly beautiful with well-presented geologic rock patterns both in or out near the sand hill bad lands.
While you wander through long standing rock in scenic hilly and bad lands the hilly country can benefit greatly not from wildlife to this and related, large geological areas and natural outcroppings alike in rugged lands. Once you explore, ensure you practice safe hiking at an enjoyable pace without the need for extensive bad experience managing associated environmental risk thereby increasing comfort while making certain to travel well throughout this unique area.
This diverse bad lands presents specific insights which researchers have given to advance different public agendas aiming at various environmentally protective agendas on a per geologic value basis. That has seen very unique wildlife conservation such as the black footed ferret and burrowing owl to become a target species to enable the best possible appreciation of the fauna that can share wildlife agendas such as habitat conservation through nature-driven value determination methods thereby seen from environmental, historical conservation, tourism and economic multi benefit solution for badlands unique site that we find.
There therefore is relatively heightened and specific focus over these management aspects and especially given several reasons including historic sites through trails are significantly found all across but so can trail and monument construction in many area. Also knowing human development through unique conservation management to extend current area would determine through enabling land conservation and trails without conservation risks as a primary or important research value. Given recent risks there remains constant awareness to future efforts regarding not just wildlife risks but also with long lasting environmental issues where in and on wildlife agenda for that site.
One of the most distinct aspects of this area is the unique geology. Formed as an eroded Pleistocene fossil lake bed known as the Ash Hollow Formation, this site has preserved a large assemblage of Pliocene and Pleistocene fossilized remains, including unique toadstool-shaped rock formations. Hudson-Meng, also within this unique geologic formation, showcases archaeological evidence of human hunting activities around 10,000 years ago. Excavations have led to the discovery of the butchered remains of hundreds of bison.
These sites serve not only as educational and research tools for archaeologists and geologists but also as an opportunity for visitors to observe this natural area. Visitors can participate in fossil hunting, exploring over 45 different distinct geological sites. It's imperative to keep in mind, several potential hazards lurk within the paths, due to weather conditions such as flooding and very rapid high winds.
One great risk of the formations near Crawford found within these badlands, is rapid evaporation after the heavy storms wash away minerals which leave relatively more erosive elements (mainly uncompressible granular sands with a very loose interlocking framework like coarse unsealed granular road surface). Human erosion management has led to attempts to reduce or manage habitat and surface degradation, thereby enabling an optimal experience for the observing visitor in safe environmental conditions.
Given that human settlements remain sparse within areas with such soil composition, the vegetation experienced much less intense, human-driven deforestation efforts in recent history and so conservation is relatively simple. However there exist some concerns that environmental risks need more stringent conservation management such as strict rules regulating trail off-roading, etc, many of which need further conservation solutions that manage environmental impact as well such as a risk profile that forewarned land manager responsibilities while always performing conservation value for important wildlife.
As you explore this distinct geologic setting, make certain to not forget the unique plant species located throughout this badlands area, mainly vegetation such as black oak trees (commonly Quercus velutina) the sideoats grama grass (Bouteloua curtipendula) shortgrasses, tallgrasses, and needlelike grass such as needle and thread (Hesperostipa comata) grasses. Rock formations, fossils of long-gone bison, other wildlife such as animals found were eventually replaced by roaming wolves, rodents etc have now been left to roam free as geologically adapted animals through shifting tectonic-plate activities being then understood through processes.
It therefore remains important to take necessary precautions when you explore the very unique area full of these beautiful sightseeing areas that may give significant educational insights that are geologically true but also incredibly beautiful with well-presented geologic rock patterns both in or out near the sand hill bad lands.
While you wander through long standing rock in scenic hilly and bad lands the hilly country can benefit greatly not from wildlife to this and related, large geological areas and natural outcroppings alike in rugged lands. Once you explore, ensure you practice safe hiking at an enjoyable pace without the need for extensive bad experience managing associated environmental risk thereby increasing comfort while making certain to travel well throughout this unique area.
This diverse bad lands presents specific insights which researchers have given to advance different public agendas aiming at various environmentally protective agendas on a per geologic value basis. That has seen very unique wildlife conservation such as the black footed ferret and burrowing owl to become a target species to enable the best possible appreciation of the fauna that can share wildlife agendas such as habitat conservation through nature-driven value determination methods thereby seen from environmental, historical conservation, tourism and economic multi benefit solution for badlands unique site that we find.
There therefore is relatively heightened and specific focus over these management aspects and especially given several reasons including historic sites through trails are significantly found all across but so can trail and monument construction in many area. Also knowing human development through unique conservation management to extend current area would determine through enabling land conservation and trails without conservation risks as a primary or important research value. Given recent risks there remains constant awareness to future efforts regarding not just wildlife risks but also with long lasting environmental issues where in and on wildlife agenda for that site.