GREAT EXPECTATIONS CAVE NATURE PRESERVE
|
|
| INTRODUCTION |
In January, 2003, the National Speleological Society (NSS) purchased 40acres of land in Big Horn County, Wyoming, that contains the upper entrance to Great Expectations Cave as well as Johnny Creek Cave. The Society acted on the opportunity to acquire access to a significant "world class" cave in the western United States and specifically to ensure that NSS members would continue to be able to visit this very special cave. This property and cave entrances make up the Great Expectations Cave Nature Preserve of the National Speleological Society ("the Preserve"). The Preserve Management Committee, chaired by the Great Expectations Preserve Manager, is responsible for effectively managing the Preserve as outlined in this Management Plan. The primary objective of this Plan is to establish processes and guidelines that will allow the Society to effectively manage the use of the Preserve, and to monitor and gauge the effects of this use. It is the intention of the Society that NSS members shall be ensured reasonable access and use of the cave and the surface property for recreation, exploration, science, and surveying. The Great Expectations Cave Management Committee is responsible for managing the Preserve according to this Management Plan.
|
| PRESERVE LOCATION AND DESCRIPTION | Permission
required
|
ACCESS |
Permission required
|
|
RESOURCES OF THE PRESERVE |
||
|
Underground Resources |
||
|
Caves |
The Great Expectations Cave Nature Preserve contains the upper entrance to Great Expectations Cave and Johnny Creek Cave. Johnny Creek Cave is a small cave located in Johnny Creek Drainage on the Preserve. |
|
|
Great Expectations contains almost 8 miles of surveyed passage with a vertical extent of over 1,400 feet. It is the third deepest limestone cave in the United States, the second deepest cave in Wyoming, and the second longest cave in Wyoming. Great Expectations Cave contains Wyoming’s largest room, The Great Hall, which is over 2,000 feet long and up to 100 feet high and wide. |
||
|
The cave has two entrances: an upper one located on the Preserve, and Great Exit, a small, lower entrance approximately four miles down Trapper Canyon from the upper entrance, on land managed by the U.S. Bureau of Land Management. Most of Great Expectations cave lies under Federal property. |
||
|
Trapper Creek and Johnny Creek, and their tributaries combine to form the Lost Worland River inside Great Expectations. |
||
|
A trip through Great Expectations is one of the most sporting and dangerous caving trips in the United States. It involves traversing the Great Hall and upper passages before dropping into the Lost Worland River. The trip through the river canyons includes descending next to several waterfalls, swimming through plunge pools, wading down sinuous water passages, and finally negotiating the Grim Crawl of Death, a 1500 foot long flat out belly crawl in quickly flowing water to the Great Exit. |
||
|
Although trip through the cave between the two entrances involves vertical alpine caving techniques, the upper portions of the cave are accessible to properly equipped and qualified cavers without using these specialized skills. Trips to this part of the cave include traversing the Great Hall and visiting the Cephalopod Malt Shop, a room where large slabs of sandstone covered with fossils are exposed beneath a ceiling full of soda straws. This trip involves wading in the cave streams, significant crawling, and scrambling over unstable breakdown and talus in the 39°F cave environment. |
||
|
Great Expectations and Johnny Creek are pristine caves. There is no graffiti inside the caves and no known damage caused by cavers other than minor trampling in some areas. In the lower parts of Great Expectations, the stream washes away most traces of passage through the cave.
|
||
|
Biological |
The biological resources of Great Expectations Cave and Johnny Creek Cave have not been inventoried. The only species observed are marmots in the Great Expectations entrance rock shelter, pack rats just inside the Great Expectations entrance, and lost trout in the streams and pools of the cave. Due to the cave’s cold temperature, cave life is probably very limited. Bats have not been observed in either cave.
|
|
|
Geological |
Both Great Expectations Cave and Johnny Creek Cave are developed in the Ordovician Bighorn Dolomite. As Trapper Creek and Johnny Creek cut into the dolomite near Trapper Fault, a portion of the stream flow was pirated into the fractures, starting the dissolution of the dolomite. Eventually all of the stream flow was diverted into the cave system that had formed. The main trend of Great Expectations Cave follows the dip of the Bighorn Dolomite, with the stream undulating between the dolomite and the underlying sandstone. When superimposed over the topographic map of the area, the cave passages of Great Expectations Cave follow the surface trend of the Trapper Creek Drainage. Most of the passages within Great Expectations Cave are vadose in nature, having been formed by the down cutting of underground streams. There are, however, a number of phreatic passages including the Great Hall. Dripstone formations are infrequently found in Great Expectations. With the exception of the Cephalopod Malt Shop, where soda straws cover the ceiling, and the formation passage in the lower cave containing six-foot long soda straws and one-inch diameter cave pearls, formations in the cave are few and far between. Numerous black chert ledges and nodules are seen throughout the cave, protruding from the bedding planes of the dolomite. Fingers of sharp rock, called "Cave Velcro," make travel through the cave difficult. There are numerous areas of granite boulders, cobbles, and gravel throughout the cave, as wells as breakdown and talus. There is no known significant damage to dripstone formations in the cave. No special measures are required to protect these resources other than encouraging careful and conscientious caving practices.
|
|
Hydrological |
Trapper Creek and Johnny Creek are the primary hydrologic resources of the cave system although Jack Creek and other unnamed tributary drainages provide input into the system during periods of high runoff. These combine to form the "Lost Worland River" within the cave. The Lost Worland River resurges approximately seven miles below the Sinks of Trapper Creek at a spring in the lower part of Trapper Canyon.
|
|
|
Paleontological |
Where the cave passage in Great Expectations Cave is incised into the underlying sandstone, numerous cephalopod fossils are exposed. In the Cephalopod Malt Shop large blocks of fossil-covered sandstone cover the floor. Mammal bones have been found in several places within the cave and are marked for protection.
|
|
|
Archeological |
No archeological resources are known to exist in the caves. Due to the nature of the entrances, the caves do not appear to have been visited or used by Native Americans. There is no evidence of exploration by early settlers or ranchers.
|
|
|
Historical |
No historical resources are known to exist within the caves.
|
|
|
SURFACE RESOURCES |
||
|
Biological |
Surface biological resources observed on the Preserve include large mammals, small mammals, fish, birds, and a variety of plants, from grasses to mature pine trees. There are no known endangered species on the Preserve. Large mammals include mule deer, elk, moose, and the occasional black bear, coyote, and mountain lion. Small mammals include rabbits, marmots (which may nest in the entrance to Great Expectations Cave), pack rats (which have been seen inside the Crisco Crack), and a variety of mice and other rodents. Although no bats have been seen in the cave, they may roost in trees on the Preserve and in the entrance rock shelter of Great Expectations. Fish, most likely common brook trout, have been observed in Trapper Creek, and a few have inadvertently ended up inside Great Expectations. It is possible that prairie rattlesnakes and other reptiles could be found on the Preserve but the high elevation would make this extremely rare. A variety of birds may be seen on the Preserve. Preserve flora includes grasses, wildflowers, sagebrush, shrubs, and several species of trees, typical of the sub-alpine mountainous environment. It is possible that non-native and weed species have been introduced to the Preserve through grazing There is no apparent need for trees to be harvested on the Preserve. Wildfire presents the greatest danger to the plant community on the Preserve, particularly to the wooded areas. The Forest Service, the BLM, and Big Horn County are responsible for suppression of wildfires in the area of the Preserve, even on private land. |
|
|
Geological |
Outcrops of Ordovician Bighorn Dolomite cover most of the Preserve. In the southeast corner of the Preserve, near the Great Expectations Cave entrance, the Trapper Fault is exposed. This fault has Bighorn Dolomite on the western up-thrown side and Madison Limestone on the eastern down-thrown side. The Trapper Creek Drainage and the Johnny Creek Drainage are partially filled with granite cobble alluvium that has washed down from the granitic core of the Bighorn Mountains to the east of the Preserve. Cambrian sandstones and granites that form the core of the Bighorn Mountains underlie the Ordovician rocks in which the caves are formed. The mineral rights to the Preserve are within the Federal mineral estate. Limestone and dolomite are the only economically recoverable mineral resources known to exist on or beneath the preserve. There has been no hard-rock mining activity on the Preserve or in the vicinity of the Preserve.
|
|
|
Hydrological |
Hydrological resources of the Preserve include Trapper Creek and the Johnny Creek Drainage. There are no water rights attached to the Preserve. North Trapper Creek and South Trapper Creek join to become Trapper Creek just east of the east boundary of the Preserve. The creek flows onto the Preserve and sinks within several hundred feet of the boundary. Trapper Creek flows year around with the greatest flows during spring runoff. Most of the year, Johnny Creek sinks before reaching the Preserve. During periods of high runoff, the flow reaches Johnny Creek Cave on the Preserve and goes underground at that point
|
|
|
Paleontological |
No paleontological resources are known to exist on the Preserve. There may be isolated marine fossils in the rock outcrops on the Preserve. |
|
|
Archeological |
There are no archeological sites known to exist on the Preserve. Native American hunting parties may have been visited the Preserve but there is no evidence of habitation.
|
|
|
Historical |
No historic structures or evidence of human habitation are evident on the Preserve. The two-track roads and fences are the only evidences of human impact
|
|
|
PRESERVE MANAGEMENT |
|
|
General Management |
|
|
|
|
The caves shall be managed to ensure use by NSS members, while promoting conservation practices to limit any decline in the condition of the caves and their contents. |
|||||||||||
|
Cave Resources | |||||||||||
|
|||||||||||
|
Environmental Resources | |||||||||||
|
| Visitors |
|
| |||||||
|
The surface property will be managed to ensure its use by NSS members, while limiting any changes in the condition of the land, and damage to its flora and fauna. |
|||
|
Access | |||
|
|||
|
Environmental | |||
|
|||
|
Visitors | |||
|
|||
|
Property | |||
|
|||
| Access Policy |
Access to the Preserve is somewhat self-restricting do to the high altitude of the cave, in combination with deep winter snows. Winter conditions will likely require visitors to use a snowmobile to access the Preserve. Therefore, caving in the winter will be discouraged due to limited rescue potential. The Bighorn National Forest road (FS 17) and the BLM Alkali road may be closed to traffic at various times throughout the year due to weather, mud, or snow conditions Access to Great Expectations Cave is self-restricting due to high water within the entrance passage series during spring runoff, and the potential for flooding in the cave. The ideal time frames in which to visit the cave are from mid to late summer and in early fall, when the potential for flooding is low, even during thunderstorms. To gain access to the upper entrance of Great Expectations Cave, every caver must sign a liability release and obtain a permit. A "Permitting Group" appointed by the Management Committee will be responsible for issuing caving and other use permits and ensuring compliance All individuals visiting the cave who have not signed the liability release will be considered to be in trespass for liability purposes. (Wyoming Law - Title 6 - Crimes and Offenses Section 6-3-303 Criminal Trespass covers this eventuality.) The permit application shall contain a brief description of the cave, its hazards and dangers, an explanation concerning the absence of rescue personnel within the region; importance of a self- and group rescue plan; and a description of necessary caving gear and clothing which are suitable for the nature of the cave. A web page on the NSS web site shall be maintained to facilitate the permit process. This the web page shall include: Information on the cave including maps; a map of the Preserve property; environmental assessment, monitoring, and visitation data; the Preserve publicity policy; a description of the permit process; through-trip information and requirements; all appropriate forms for completion; instructions for applying for a permit; available visitation dates; and appropriate Preserve Committee member contact information. Groups requesting to do a through trip in Great Expectations Cave are required to take several additional steps in the permitting process, which shall be explained on the web page. One of the steps is to secure written permission to cross the private lands required to reach the Great Exit, and to provide written proof of this to the permitting group. |
Appendix One – Trip/Liability Card
|
Trip Card Date & time in ___/___/___ _______ Date & time out ___/___/___ ______ Trip leader ______________________ Number in party _____ (Please list the trip members on the back.) Purpose of trip Was there anything unusual or any problem you noted on the property of which the manager should be aware? |
|
Liability Release I, the undersigned, do hereby release forever the NSS or anyone acting directly or indirectly on the part of the NSS, from all liability, damages and responsibilities of any nature whatsoever incurred by my hiking, educational or research activities on said property. I agree that any personal injuries, accidents, death, damage to my property, or health problems incurred by me on said property are my responsibility, not the NSS's. I promise to bind myself, my family, and my heirs to the aforementioned terms of this release. I have carefully read the foregoing release and indemnifying agreement and understand the contents thereof, and sign this document of our own free will. _____________________________________ _____________________________________ _____________________________________ _____________________________________ |