Oregon Caves National Monument

Oregon Caves National Monument
Oregon Caves National Monument
U.S. National Monument
Flowstone in Oregon Caves
Country United States
State Oregon
County Josephine
City Cave Junction
Cave entrance About 20 miles (32 km) east of Cave Junction [1]
 - elevation 4,377 ft (1,334 m) [1]
 - coordinates 42°05′44″N 123°24′21″W / 42.09556°N 123.40583°W / 42.09556; -123.40583
Highest point
 - elevation 5,480 ft (1,670 m) [2]
Area 488 acres (197 ha) [3]
Geology Dissolution cave in marble
Established July 12, 1909 [4]
Management National Park Service
Visitation 80,894 [5]
Location of the cave in Oregon. Inset: Oregon in the United States
Website: Oregon Caves

Oregon Caves National Monument is a national monument in the northern Siskiyou Mountains of southwestern Oregon in the United States. The main part of the 488-acre (197 ha) park, including the marble cave and a visitor center, is located 20 miles (32 km) east of Cave Junction, on Oregon Route 46. A separate visitor center in Cave Junction occupies 4 acres (1.6 ha) of the total. Both parts of the monument, managed by the National Park Service, are in southwestern Josephine County, near the Oregon–California border. The climate is generally mild even at the cave's elevation of about 4,000 feet (1,200 m) above sea level, but icicles can form at the cave entrance, and winter snow sometimes blocks the park highway.

Elijah Davidson, a resident of nearby Williams, discovered the cave in 1874. Over the next two decades, private investors failed in efforts to run successful tourist ventures at the publicly owned site. After passage of the Antiquities Act by the United States Congress, President William Howard Taft established Oregon Caves National Monument, to be managed by the United States Forest Service, in 1909. The popularity of the automobile, construction of paved highways, and promotion of tourism by boosters from Grants Pass led to large increases in cave visitation during the late 1920s and thereafter. Among the attractions at the remote monument is the Oregon Caves Chateau, a six-story hotel built in a rustic style in 1934. The Park Service, which assumed control of the monument in 1933, offers tours of the cave from mid-April through early November.

Oregon Caves is a dissolution cave, with passages totaling about 15,000 feet (4,600 m), that formed in marble. The parent rock was originally limestone that metamorphosed to marble during the geologic processes that created the Klamath Mountains, including the Siskiyous. Although the limestone formed about 190 million years ago, the cave itself is no older than a few million years. Valued as a tourist cave, the cavern also has scientific value; sections of the cave that are not on tour routes contain fossils of national importance.

In addition to cave touring, activities at the park include hiking, photography, and wildlife viewing. One of the park trails leads through the forest to Big Tree, which at 13 feet (4.0 m) is the largest diameter Douglas-fir known in Oregon. Lodging and food are available at The Chateau and in Cave Junction. Camping is available at Forest Service campgrounds and private sites in the area.



Oregon Caves National Monument is located in the Siskiyou Mountains, a coastal range that is part of the Klamath Mountains of northwestern California and southwestern Oregon. The main part of the park consists of 484 acres (196 ha)[2] in the Rogue River – Siskiyou National Forest, about 6 miles (9.7 km) north of the Oregon–California border in Josephine County, Oregon.[6] An additional visitor center occupies 4 acres (1.6 ha) in the city of Cave Junction.[2] The city is in the Illinois River valley, about about 40 miles (64 km) east of the Pacific Ocean.[7] Elevations within the park range from 3,680 to 5,480 feet (1,120 to 1,670 m) in the mountains to 1,800 feet (550 m) in the city.[2]

By highway, Oregon Caves is 55 miles (89 km) southwest of Grants Pass, 300 miles (480 km) south of Portland and 450 miles (720 km) north of San Francisco.[8] The caves are 20 miles (32 km) west of Cave Junction via Oregon Route 46, which intersects U.S. Route 199 at Cave Junction.[2]

Despite the monument's name, the main cave is a single system[9] with known passages totaling about 15,000 feet (4,600 m) in length.[2] Eight separate smaller caves have also been discovered in the monument.[2]

Runoff from the heavily wooded monument forms small headwater streams of the Illinois River, a major tributary of the Rogue River. One of five small springs in the monument becomes Upper Cave Creek, which flows on the surface before disappearing into its bed and entering the cave. Supplemented by water entering the cave from above, the stream emerges from the main entrance as Cave Creek.[2]


Map of the Cave

Archeologists believe the first humans to inhabit the Rogue River region were nomadic hunters and gatherers.[10] Radiocarbon dating suggests that they arrived in southwestern Oregon at least 8,500 years ago.[10] At least 1,500 years before the first contact with whites, the natives established permanent villages along streams.[10] Even so, no evidence has been found to suggest that any of the native peoples, such as the Takelma who lived along the Rogue and Applegate rivers in the 19th century, used the cave.[4]

Largely bypassed by the early non-native explorers, fur traders, and settlers because of its remote location, the region attracted newcomers in quantity when prospectors found gold near Jacksonville in the Rogue River valley in 1851.[11] This led to the creation of Jackson County in 1852 and, after gold discoveries near Waldo in the Illinois River valley, to the creation of Josephine County, named for the daughter of a gold miner.[12] Even with an influx of miners and of settlers who farmed donation land claims, Josephine County's population was only 1,204 in 1870.[13]

Elijah Jones Davidson, who discovered the cave in 1874, emigrated from Illinois to Oregon with his parents, who eventually settled along Williams Creek in Josephine County.[14] Williams, as the community came to be called, is about 12 miles (19 km) northeast of the cave.[6]

Only a few people visited the cave during the next decade. Among them was Thomas Condon, professor of geology at the University of Oregon. Guided by Davidson's brother, in 1884 he and a group of students hiked from Williams to the cavern, which they inspected by candlelight.[15] Shortly thereafter, Walter Burch, an acquaintance of the Davidson family, tried to develop the cave as a business.[15] Burch and his partners opened what they called Limestone Caves and charged visitors $1 each for a guided cave trip, a camping spot, pasture for horses, and cave water they described as medicinal.[4] Although Burch and others hacked crude trails to the cave from Cave Junction and Williams, the trip was too difficult for most tourists, and Limestone Caves ceased operations in 1888.[16]

Flowstone in Oregon Caves

In the early 1890s, the Oregon Caves Improvement Company, headed by Alfonso B. Smith of San Diego and two men from Kerby, Oregon, tried to raise capital for a larger tourist business at Oregon Caves.[17] Smith made outlandish claims about the cave and its business potential, saying that it was 22 miles (35 km) long, that an ordinary horse and buggy could be driven through 10 miles (16 km) of it, that it had 600 separate chambers, and that the company planned to build something like a streetcar line from Williams to the cave.[17] Smith succeeded in wooing the The San Francisco Examiner, which twice sent reporters to the site. The second occasion involved a cave expedition that lasted about 10 days and involved "an orgy of destruction"[18] in which passages were widened, formations broken or deliberately removed, and directional arrows added to the cave walls.[17] After Smith spent had spent all the company's money and borrowed more in its name, he disappeared in 1894, and the business collapsed.[17]

Neither Burch nor Smith had owned the cave or the land around it, which belonged to the public.[19] Beginning in the 1890s, the Federal government began regulating the use of public lands like these.[20] In 1903, President Theodore Roosevelt designated millions of acres of forest lands for protection, including what became Siskiyou National Forest, which surrounds the cave. The United States Forest Service was created in 1905 to manage these reserves. Three years later, Congress passed the Antiquities Act, which allowed the President to designate protected areas called National Monuments on public lands. In 1909, President William Howard Taft established Oregon Caves National Monument, to be managed by the Forest Service. A year later the Forest Service employed men to guard the cave and to serve as tour guides.[4]

Isolated and difficult to reach, the monument attracted only 1,800 visitors in 1920.[4] The situation changed markedly when large numbers of Americans began to travel by automobile on roads paid for largely with government funds. One highway connected Grants Pass with the California coast at Crescent City.[21] Another new road, the Oregon Caves Highway, led from the Grants Pass – Crescent City highway to the cave.[21] Campaigns to attract car-driving tourists included those of the Cavemen, a booster group from Grants Pass that dressed in animal skins, posed along tour routes, and staged annual events to promote the monument.[n 1] By 1928, the number of visitors to the cave had risen to about 24,000 a year.[21]

The Chateau

The visitors' need for overnight lodging led to creation of public and private campsites and rustic cabins along highways near Cave Junction and the monument.[23] In 1923, the Forest Service signed a contract with the Oregon Caves Company, based in Grants Pass, to run the cave tours and improve the park accommodations.[4] The Chalet, a building with a kitchen, dining room, gift shop, ticket sales area, and a dormitory for women on the Oregon Caves Company staff, was completed later that year. Three years later, the company added seven two-bedroom cabins for tourists and a dormitory for male employees.[4] In 1928, an Oregon Caves bill written by the Forest Service and introduced by Senator Charles McNary of Oregon won Congressional approval.[24] It provided funds for electric lights, a power plant, a formation-washing system, and an artificial exit tunnel to eliminate the crowding that occurred when two groups on round-trip tours had to pass one another in the cave. The 500-foot (150 m) tunnel was completed in 1931.[24]

Management of the monument was transferred from the Forest Service to the National Park Service in 1933, and a six-story hotel, the Oregon Caves Chateau, was completed at the site in 1934.[4] Gust Lium, a builder from Grants Pass, oversaw construction of the Chateau and some of the park's other buildings, which he designed in a rustic style.[25] Mason Manufacturing of Los Angeles produced the Chateau's furniture in a style called Monterey, valued in 21st century at up to $5,000 for a single chair.[26] During the 1930s and early 1940s, the Civilian Conservation Corps (CCC) installed water and telephone lines, improved trails, and worked on landscaping at the park.[4] The Chalet was rebuilt in 1942 to include a third story and a larger dormitory for women.[27]

Although a flood in 1964 caused $100,000 in damage to the Chateau, it was repaired. By 1968, a total of one million people had visited the cave. In 1987, the Chateau was declared a National Historic Landmark. In 2001, the Park Service began running the cave tours formerly offered by private contractors, and two years later all the structures at the monument became public property managed by the Park Service. The Illinois Valley Community Development Organization, a non-profit based in Cave Junction, runs the monument's gift shop.[4]

Geology and paleontology

Stalactites and stalagmites in Miller's Chapel

Oregon Caves is unusual in that it was formed in marble. Most caves created by dissolving of rocks are formed in limestone or dolomite.[28] Of the more than 3,900 caves managed by the National Park Service, only those in Oregon Caves National Monument, Kings Canyon National Park, and Great Basin National Park have marble caves.[28][n 2]

The parent rock in which the cave developed was formed about 190 million years ago as limestone that was part of a tectonic plate beneath the Pacific Ocean.[31] Granitic plutons intruded upon this part of the ocean crust, the Applegate terrane, about 160 million years ago.[32] As the terrane subducted under the North American plate, the limestone was subjected to heat and pressure that metamorphosed it to marble.[31] Further tectonic movements eventually lifted the marble to about 4,000 feet (1,200 m) above sea level.[33] The marble block containing the cave is at least 1,080 feet (330 m) long, 490 feet (150 m) wide, and about 390 feet (120 m) high.[34]

The cave's creation took place long after the marble formed.[32] As groundwater seeped into cracks in the marble, it eventually dissolved enough rock to expand some of the cracks to the size of tunnels.[31] Generally, the age of a cave cannot be determined directly because the cave itself is an empty space.[35] However, scientists can sometimes determine the age of speleothems or sediments in a cave.[35] An early 21st-century study of speleothem development in Oregon Caves focused on the past 380,000 years.[36] Based on the available evidence, the cave is thought to be at least a million years old and "probably not much older than a few million" years.[37]

Marble has a more coarse-grained texture than limestone, but both are made of calcite (CaCO3).[38] Caves often develop when slightly acidic groundwater dissolves calcite along natural fractures in the rock.[39] A reversal of the dissolving process can create flowstone and dripstone such as stalactites, that hang from cave ceilings like icicles, and stalagmites, cone-shaped masses that form on cave floors, usually directly below stalactites.[39] These structures form when acidic groundwater with a high concentration of dissolved calcite drips slowly from the ceiling of an air-filled cave, becomes less acidic, and leaves some of its calcite behind as a solid precipitate.[39] Oregon Caves includes a variety of cave formations created through precipitation of calcite.[40][n 3] Although many of the speleothems in the public sections of the cave have been broken, discolored by human skin oils, or otherwise damaged, the narrow twisting passages of the "show cave" provide enduring tourist value.[41]

The cave is not pure marble. Dikes of diorite, an igneous rock that was part of a pluton, cut through the marble in places. Shales and sandstones, which are sedimentary rocks, are in places interbedded with the marble. In addition, streams have carried silts and gravels from the surface into the cave.[32]

The monument has more than 50 paleontological sites ranging in age from Late Pleistocene to Holocene.[42] A fossil of a grizzly bear more than 50,000 years old and a jaguar fossil between 40,000 and 20,000 years old have been found in the cave.[2] Other fossils include amphibians,[42] and rare finds of the mountain beaver, and the blue grouse.[2] The monument's mammalian fossils, found in non-public sections of the cave,[43] are of national significance.[2]


The main unit of the monument is located in the mountains at elevations varying from 3,680 to 5,480 feet (1,120 to 1,670 m) above sea level. The park's nearness to the ocean contributes to its relatively mild climate. Temperatures generally range between 20 and 40 °F (-7 and 4 °C) in winter and 50 and 90 °F (10 and 32 °C) in summer.[2] However, inside the cave, the temperature is always about 44 °F (7 °C).[44][n 4] Annual precipitation, arriving mostly as wet snow, averages 55 inches (1,400 mm). Moderate winds are common.[2]

The climate in Cave Junction, at 1,800 feet (550 m) above sea level,[2] is warmer and wetter than the climate at the main unit. December and January are the coldest months, when highs average about 46 °F (8 °C) and lows average 32 °F (0 °C).[46] July and August are the warmest months, with an average high of 92 °F (33 °C) and an average low of about 50 °F (10 °C).[46] The highest recorded temperature at Cave Junction was 112 °F (44 °C) in 2006, and the lowest was −6 °F (−21 °C) in 1972.[46] Annual precipitation averages about 63 inches (1,600 mm). November through February are the wettest, averaging about 10 to 11 inches (250 to 280 mm) each month.[46]

Climate data for Cave Junction, Oregon
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Average high °F (°C) 47
Average low °F (°C) 32
Precipitation inches (mm) 10.81
Source: The Weather Channel[46]

Flora and fauna

Located within the Klamath–Siskiyou region, known for its high biodiversity,[47] the monument supports 391 vascular plant species as well as many species of bryophyte, lichen, and macrofungi.[2] Trees in the monument include Douglas-fir, oak, white fir, and alder. Among the oldest trees is Big Tree, the largest diameter Douglas-fir known in Oregon.[2] It is 41 feet (12 m) in circumference near the base.[48] Its age is estimated at 600 to 800 years[48] and it was described in the 1930s as 14 feet (4.3 m) in diameter.[49][n 5] The monument contains no plants with special conservation status.[2]

Species lists for the park include about 50 mammals, 86 birds, 11 reptiles and amphibians, 8 bats, more than 200 arthropods, 8 snails and slugs, 75 butterflies, more than 55 moths, and 8 aquatic macroinvertebrates. Of these species, 160 are found inside the cave. Outside the cave, black-tailed deer, Stellar's Jay, Common Raven, and Townsend's chipmunk are among animals often seen in the park. Less commonly sighted are black bear, cougar, northern flying squirrel, and Pacific giant salamander. Springs and other wet places support flatworms, frogs, and snails.[2]

Animal species in the park with special conservation status are the Northern Spotted Owl, California mountain kingsnake, tailed frog, Del Norte salamander, Northern Goshawk, Olive-sided Flycatcher, Little Willow Flycatcher, Siskiyou gazelle beetle, and Pacific fisher. Five at-risk species are found in the cave: Townsend's big-eared bat, long-eared myotis, fringed myotis, long-legged myotis, and Yuma myotis.[2]


Map of trails in and near the monument. "P" identifies the parking lot for the hotel and visitor center, represented by the ranger and small hut icon.

Oregon Caves National Monument is open year-round, although snow sometimes blocks the road to the park. Cave tours are offered from mid-spring (mid-April) to late fall (early November), and the visitor center is open when the cave is open for tours. The schedule varies from season to season, but tours generally start no earlier than 9 a.m. and no later than 6 p.m. except for candlelight tours offered on Fridays and Saturdays at 6:30 p.m. between late May and early September.[50]

Cave-tour tickets are available only at the monument and are sold on a first-come, first-served basis. Tours are 0.5 miles (0.80 km) long and last 90 minutes, although visitors can choose to leave the cave about halfway through the tour. The route requires negotiating more than 500 steep and uneven stairs and passageways with as little as 45 inches (110 cm) between floor and ceiling. Not recommended by the Park Service for anyone with heart, lung, or mobility problems, the tour involves a total climb of 230 feet (70 m). Children less than 42 inches (110 cm) tall or who are unable to climb a set of test stairs on their own are not allowed on the full cave tour.[44] The Park Service offers a limited number of off-trail "Introduction to Caving" tours by advanced reservation only.[51]

Since the cave is only 44 °F (7 °C) inside regardless of the outdoor temperature, the Park Service recommends warm clothing for its tours. Good walking shoes are needed to negotiate slippery and uneven surfaces. Not allowed on the tours are flashlights, backpacks, large purses, tripods, or pets. To protect bats from white nose syndrome, visitors must not take any clothing or equipment into Oregon Caves that entered any cave in Europe or any cave, mine, or bat hibernation site east of the Rocky Mountains in North America after 2005.[44]

Several hiking trails wind through the monument and adjacent forest lands. Big Tree Trail, 3.3 miles (5.3 km) long, gains 1,100 feet (340 m) in elevation between the visitor center and Big Tree.[52] No Name Trail, 1.3 miles (2.1 km) long, begins behind the visitor center, follows Cave Creek, crosses it, and then climbs steeply to the west side of the monument. Two short side trails lead from the main trail to waterfalls along No Name Creek.[53] Cliff Nature Trail, passing over marble outcrops and through fir forests, winds for about 1 mile (1.6 km) from near the cave entrance past the cave exit to Big Tree Trail.[54] Old Growth Trail, 0.8 miles (1.3 km) long, links the Chateau and visitor center to the main parking lot.[55] Other named trails entering the park include Cave Creek, Mt. Elijah, and Limestone.[56]

Lodging is available in the monument at the six-story Chateau, which has 23 rooms to rent.[57] Hotels, bed and breakfasts, motels, and resorts in the vicinity offer a variety of accommodations.[58] Although no camping is allowed in the monument, the Forest Service maintains two campgrounds nearby, and there are private campgrounds and recreational vehicle parks in the vicinity.[59] The Chateau, generally open from early May to late October, has a restaurant, coffee shop, and delicatessen, and Cave Junction has several restaurants. The monument grounds include several picnic tables.[60]

Notes and references

  1. ^ In 1931, the Cavemen dedicated Caveman Bridge over the Rogue River in Grants Pass. The bridge marks the northern end of the Redwood Highway (U.S. Route 199), which connects Grants Pass with Cave Junction and the Oregon Caves Highway. Grants Pass High School uses "Cavemen" as its mascot name.[22]
  2. ^ Eighty one parks managed by the National Park Service have caves.[29] Not all are solution caves formed by dissolving of rock. Some are lava caves, others are talus caves formed by rocks falling atop narrow crevices, and some are sea caves.[30] Lava Beds National Monument alone has more than 450 separate lava caves.[29]
  3. ^ The chemical equation for the process is H2O + CO2 + CaCO3  \rightleftarrows  Ca++ + 2HCO3-; that is, water plus carbon dioxide plus calcite can yield calcium ions plus bicarbonate ions and vice versa. The carbon dioxide can either be acquired from the atmosphere (or soils), making the water more acidic, or it can be released to the atmosphere, making the water less acidic. The equation is read from left to right for cave formation (dissolution) and from right to left for flowstone and dripstone formation (precipitation).[39]
  4. ^ The transition zones near the cave's entrances are exceptions. For example, icicles sometimes form in below-freezing temperatures at the mouth of the main entrance.[45]
  5. ^ Calculated using a circumference, c, of 41 feet (12 m) in the formula c = π × d, where π is rounded to 3.14, the diameter, d, is about 13 feet (4.0 m).
  1. ^ a b "Oregon Caves National Monument". Geographic Names Information System (GNIS). United States Geological Survey. November 28, 1980. http://geonames.usgs.gov/pls/gnispublic/f?p=gnispq:3:::NO::P3_FID:1147260. Retrieved October 17, 2011. 
  2. ^ a b c d e f g h i j k l m n o p q r s "Appendix C" (PDF). Klamath Network Vital Signs Monitoring Plan. National Park Service. 2007. pp. 20–24. http://science.nature.nps.gov/im/units/klmn/monitoring/Documents/PhaseIII/Appendix_C_phase3_final_pdf.pdf. Retrieved August 17, 2011. 
  3. ^ "Listing of Acreage" (PDF). National Park Service. December 31, 2010. http://www.nature.nps.gov/stats/Acreage/acrebypark10cy.pdf. Retrieved October 17, 2011. 
  4. ^ a b c d e f g h i j "Timeline". National Park Service. 2007. http://www.nps.gov/orca/historyculture/timeline.htm. Retrieved August 19, 2011. 
  5. ^ National Park Service Public Use Statistics Office (2010). "NPS Stats". National Park Service. http://www.nature.nps.gov/stats/viewReport.cfm?selectedReport=SystemComparisonReport.cfm. Retrieved October 17, 2011.  This is the average for the years 2006–10.
  6. ^ a b Oregon Atlas & Gazetteer (7th ed.). Yarmouth, Maine: DeLorme. pp. 66–67. ISBN 978-0-89933-347-2. 
  7. ^ The Road Atlas (2008 ed.). Chicago: Rand McNally & Company. pp. 84–85. ISBN 978-0-5289-3961-7. 
  8. ^ "Frequently Asked Questions". National Park Service. 2009. http://www.nps.gov/orca/faqs.htm. Retrieved August 17, 2011. 
  9. ^ "Kilroy was there: Vandalism and graffiti really are nothing new". The Milwaukee Journal (Los Angeles Times Service): p. 41. October 21, 1983. http://news.google.com/newspapers?id=6m4aAAAAIBAJ&sjid=-ikEAAAAIBAJ&pg=6383,385203. Retrieved August 26, 2011. 
  10. ^ a b c Douthit, pp. 5–6
  11. ^ Mark, p. 17
  12. ^ Mark, p. 24
  13. ^ Mark, pp. 25–26
  14. ^ Mark, p. 28
  15. ^ a b Mark, p. 31
  16. ^ Mark, pp. 37–41
  17. ^ a b c d Mark, p. 37–41
  18. ^ Mark, p. 40
  19. ^ Mark, pp. 36–37
  20. ^ Mark, p. 43
  21. ^ a b c Mark, pp. 63–66
  22. ^ Mark, pp. 123–24
  23. ^ Mark, pp. 66–70
  24. ^ a b Mark, pp. 81–84
  25. ^ "Gust Lium". National Park Service. 2006. http://www.nps.gov/orca/historyculture/gustlium.htm. Retrieved August 30, 2011. 
  26. ^ "Great Lodges of the National Parks Pacific Northwest: Oregon Caves". Oregon Public Broadcasting. 2008. http://www.pbs.org/opb/greatlodges/nationalparks/pacific/caves.html. Retrieved November 6, 2011. 
  27. ^ Mark, p. 112
  28. ^ a b Schubert, Mary. "Study of a Karst-Geochemical Data Set from a Marble Cave: Oregon Caves National Monument" (PDF). 2007 National Cave and Karst Management Symposium. University of Texas. pp. 219–32. http://www.utexas.edu/tmm/sponsored_sites/biospeleology/nckms2007/Papers/schubert.pdf. Retrieved September 1, 2011. 
  29. ^ a b "The Cave and Karst Program". National Park Service. 2006. http://www.nature.nps.gov/geology/caves/program.htm. Retrieved September 1, 2011. 
  30. ^ "Cave & Karst Parks Tour". National Park Service. 2006. http://www.nature.nps.gov/geology/caves/tour.htm. Retrieved September 1, 2011. 
  31. ^ a b c Orr and Orr, pp. 70–71
  32. ^ a b c Bishop, pp. 50–52
  33. ^ "Environmental Factors". National Park Service. 2006. http://www.nps.gov/orca/naturescience/environmentalfactors.htm. Retrieved August 29, 2011. 
  34. ^ Palmer and Palmer, p. 298
  35. ^ a b Stock, Greg M.; Riihimaki, Catherine A.; Anderson, Robert S. "Age constraints on cave development and landscape evolution in the Bighorn Basin of Wyoming" (PDF). Journal of Cave and Karst Studies 68 (2): 76–84. http://www.caves.org/pub/journal/PDF/V68/v68n2-Stock.pdf. 
  36. ^ Ersek, Vasile, et al. (2009). "Environmental influences on speleothem growth in southwestern Oregon during the last 380,000 years". Earth and Planetary Science Letters (Elsevier) (279): 316–25. http://geo.orst.edu/files/geo/Ersek-2009-EPSL.pdf. 
  37. ^ Roth, John (September 2005). "Oregon Caves National Monument Subsurface Management Plan Environmental Assessment" (PDF). National Park Service. p. 22. http://www.caves.org/region/western/Docs/ea-subsuface-plan.9.05.releaseversion.pdf. Retrieved October 21, 2011. 
  38. ^ Plummer and McGeary, p. 136
  39. ^ a b c d Plummer and McGeary, pp. 247–50
  40. ^ "Cave Photographs". 2010. http://www.nps.gov/orca/photosmultimedia/Cave-Photographs.htm. Retrieved September 1, 2011. 
  41. ^ Oliphant and Oliphant, p. 56
  42. ^ a b Covington, Sid (September 10, 2004). "Oregon Caves National Monument Geologic Resources Management Issues Scoping Summary" (PDF). National Park Service. http://www.nature.nps.gov/geology/inventory/publications/s_summaries/ORCA_scoping_summary_20041025.pdf. Retrieved October 21, 2011. 
  43. ^ Oliphant and Oliphant, p. 51
  44. ^ a b c "General Cave Tours". National Park Service. 2011. http://www.nps.gov/orca/planyourvisit/cave_tours.htm. Retrieved October 14, 2011. 
  45. ^ Lachman, Phil (November 8, 2010). "Earth Science Picture of the Day: Ice Stalactites in Oregon Caves National Monument". National Aeronautics and Space Administration. http://epod.usra.edu/blog/2010/11/ice-stalactites-in-.html. Retrieved October 21, 2011. 
  46. ^ a b c d e "Monthly Averages for Cave Junction, Oregon". The Weather Channel Interactive, Inc. http://www.weather.com/outlook/health/allergies/wxclimatology/monthly/USOR0059. Retrieved August 17, 2011. 
  47. ^ "Geodiversity Increases Biodiversity". National Park Service. 2010. http://www.nps.gov/orca/naturescience/index.htm. Retrieved November 6, 2011. 
  48. ^ a b "The Big Tree Trail" (PDF). National Park Service. http://www.nps.gov/orca/forkids/upload/bigtree.pdf. Retrieved October 11, 2011. 
  49. ^ Mark, p. 102
  50. ^ "Operating Hours and Seasons". National Park Service. 2011. http://www.nps.gov/orca/planyourvisit/hours.htm. Retrieved October 15, 2011. 
  51. ^ "Off-Trail Caving Tours". 2011. http://www.nps.gov/orca/planyourvisit/off-trail-caving-tours.htm. Retrieved October 15, 2011. 
  52. ^ "The Big Tree Trail". National Park Service. 2011. http://www.nps.gov/orca/planyourvisit/bigtree.htm. Retrieved October 12, 2011. 
  53. ^ "No Name Trail". National Park Service. 2011. http://www.nps.gov/orca/planyourvisit/no_name_trail.htm. Retrieved October 12, 2011. 
  54. ^ "Cliff Nature Trail". National Park Service. 2011. http://www.nps.gov/orca/planyourvisit/cliff-nature-trail.htm. Retrieved October 12, 2011. 
  55. ^ "Old Growth Trail". National Park Service. 2011. http://www.nps.gov/orca/planyourvisit/old_growth_trail.htm. Retrieved October 12, 2011. 
  56. ^ "Hiking Trails" (PDF). National Park Service. 2010. http://www.nps.gov/orca/planyourvisit/loader.cfm?csModule=security/getfile&PageID=393958. Retrieved October 12, 2011. 
  57. ^ "Lodging". National Park Service. 2011. http://www.nps.gov/orca/planyourvisit/lodging.htm. Retrieved October 23, 2011. 
  58. ^ "Lodging Near the Monument". National Park Service. 2010. http://www.nps.gov/orca/planyourvisit/lodging_near_monu.htm. Retrieved October 23, 2011. 
  59. ^ "Camping and RV Parks in the Area". National Park Service. 2010. http://www.nps.gov/orca/planyourvisit/camping.htm. Retrieved October 23, 2011. 
  60. ^ "Where to Eat". National Park Service. 2010. http://www.nps.gov/orca/planyourvisit/wheretoeat.htm. Retrieved October 23, 2011. 

Works cited

  • Bishop, Ellen Morris (2004). Hiking Oregon's Geology, 2nd ed. Seattle: The Mountaineers Books. ISBN 0-89886-847-5.
  • Douthit, Nathan (2002). Uncertain Encounters: Indians and Whites at Peace and War in Southern Oregon. Corvallis, Oregon: Oregon State University Press. ISBN 0-87071-549-6.
  • Oliphant, Joe and Oliphant, Tina, eds.; Halliday, William R. (2006). "Geology of Oregon Cave Revisited" in Alpine Karst Volume 2. Dayton, Ohio: Cave Books. ISBN 978-0-939748-64-8.
  • Orr, Elizabeth L., and Orr, William N. (1999). Geology of Oregon, 5th ed. Dubuque, Iowa: Kendall/Hunt Publishing Company. ISBN 0-7872-6608-6.
  • Palmer, A.N and Palmer, M.V., eds.; Halliday, William R. (2009). "Oregon and Washington" in Caves and Karst of the USA. Huntsville, Alabama: National Speleological Society. ISBN 978-1-879961-28-9.
  • Plummer, Charles C., and McGeary, David (1988). Physical Geology, 4th ed. Dubuque, Iowa: Wm. C. Brown Publishers. ISBN 0-697-05092-0.

External links

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