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Kenai Fjords National Park

Kenai Fjords National Park
IUCN category II (national park)
Bear Glacier Lake in Kenai Fjords National Park
Map showing the location of Kenai Fjords National Park
Location Kenai Peninsula Borough, Alaska, United States
Nearest city Seward
Coordinates
Area 669,984 acres (271,133 ha)[1]
Established December 2, 1980
Visitors 281,279 (in 2012)[2]
Governing body U.S. National Park Service

Kenai Fjords National Park is a United States National Park established in 1980 by the Alaska National Interest Lands Conservation Act. The park covers an area of 669,984 acres (1,046.85 sq mi; 2,711.33 km2)[1] on the Kenai Peninsula in southcentral Alaska, near the town of Seward. The park contains the Harding Icefield, one of the largest ice fields in the United States. The park is named for the numerous fjords carved by glaciers moving down the mountains from the ice field. The field is the source of at least 38 glaciers, the largest of which is Bear Glacier. The park lies just to the west of Seward, a popular port for cruise ships. Exit Glacier is reachable by road and is a popular tour destination. The remainder of the park is primarily accessible by boat. The fjords are glacial valleys that have been submerged below sea level by a combination of rising sea levels and land subsidence.

Kenai Fjords National Monument was initially designated by President Jimmy Carter on December 1, 1978, using the Antiquities Act, pending final legislation to resolve the allotment of public lands in Alaska. Establishment as a national park followed the passage of the Alaska National Interest Lands Conservation Act in 1980. The park protects the icefield, a narrow fringe of forested land between the mountains and the sea, and the deeply indented coastline. The park is home to a variety of terrestrial and marine mammals, including bears, whales, seals and moose.

Contents

  • History 1
    • Human habitation 1.1
    • Proposals for a Kenai Fjords park 1.2
    • National Park 1.3
    • Activities 1.4
  • Geography 2
    • Geology 2.1
  • Wildlife and ecology 3
    • Exxon Valdez oil spill 3.1
  • References 4
  • Bibliography 5
  • External links 6

History

Kenai Fjords National Park was established in 1980 by the Alaska National Interest Lands Conservation Act (ANILCA).[3] It is a relatively small and accessible park by Alaskan national park standards, about 88% as big as Yosemite National Park. It is the fifth most-visited park in Alaska, but the 11th of 13 Alaska parks in area, and is the closest national park to Anchorage. The park's headquarters is in Seward.[4] It is the only Alaska national park that did not originally allow subsistence use by native Americans, but native village corporations continue to have interests in inholdings within the park,[5] and have since established subsistence rights on those properties.[6]

Human habitation

At the time of the park's establishment, there were few permanent inhabitants.[7] Archeological surveys have altered the early view that the area was subject to only transient occupation as evidence has accumulated of long-term use. It is believed that coastal subsidence and rising water levels have inundated many sites, as the shoreline was the place richest in resources for early peoples.[8] A 1993 Park Service survey documented several village sites dated between 1200 AD and 1920. The survey also found evidence that an earthquake dating to about 1170 AD lowered the shoreline by at least 1.8 metres (5.9 ft), potentially inundating earlier sites. A 2003 follow-up survey indicated that one site was occupied between 950 AD and 1800. Another site was used from 1785 to 1820. A third site showed occupancy from 1850 to 1890.[8]

Several gold mines from historical times have been documented in the park.[7] Mining activity centered on Nuka Bay. Some sites had been active into the 1980s. Eleven mine sites have been documented and two of the mine sites have been determined to be eligible for the National Register of Historic Places.[9]

Proposals for a Kenai Fjords park

Early studies of possible new Park Service units in Alaska took place in the 1930s and 1940s. The first study, entitled Alaska - Its Resources and Development was centered on the development of tourism, despite a dissent from co-author

  • Kenai Fjords National Park National Park Service site

External links

  • Catton, Theodore (2010), A Fragile Beauty: An Administrative History of Kenai Fjords National Park, National Park Service
  • Cook, Linda; Norris, Frank (1998), A Stern and Rock-Bound Coast: Kenai Fjords National Park Historic Resource Study, National Park Service

Bibliography

  1. ^ a b "Listing of acreage as of December 31, 2011". Land Resource Division, National Park Service. Retrieved 2012-03-07. 
  2. ^ "NPS Annual Recreation Visits Report". National Park Service. Retrieved 2013-02-21. 
  3. ^ Catton, p. 2
  4. ^ Catton, pp. 3–4
  5. ^ Catton, p. 5
  6. ^ a b Catton, pp. 213–217
  7. ^ a b Catton, pp. 93–94
  8. ^ a b c Catton, pp. 197–198
  9. ^ Catton, pp. 201–203
  10. ^ Catton, p. 25
  11. ^ Catton, pp. 25–27
  12. ^ Catton, pp. 27–29
  13. ^ Catton, pp. 22–23
  14. ^ Catton, p. 32
  15. ^ Catton, pp. 33–35
  16. ^ Catton, p. 47
  17. ^ Catton, p. 55
  18. ^ Catton, pp. 58–59
  19. ^ Catton, pp. 59–60
  20. ^ Catton, pp. 66–67
  21. ^ Catton, pp. 73–74
  22. ^ Catton, p. 75
  23. ^ Catton, p. 219
  24. ^ Catton, p. 220
  25. ^ "Seward Basics". CruisePortInsider. Retrieved 11 February 2013. 
  26. ^ "Boat Tours". Kenai Fjords National Park. National Park Service. Retrieved July 11, 2009. 
  27. ^ Catton, pp. 135, 137–138
  28. ^ Catton, pp. 149–150
  29. ^ Catton, p. 208
  30. ^ "Kenai Fjords Map". Kenai Fjords National Park. National Park Service. 
  31. ^ "Exit Glacier". Kenai Fjords National Park. National Park Service. Retrieved July 11, 2009. 
  32. ^ "Harding Ice Field Trail". Kenai Fjords National Park. National Park Service. Retrieved July 11, 2009. 
  33. ^ a b "Fjord Estuary Ecosystem". Keai Fjords National Park. National Park Service. Retrieved 8 February 2013. 
  34. ^ "Geologic Formations". Kenai Fjords National Park. National Park Service. Retrieved 4 February 2013. 
  35. ^ "Kenai Fjords National Park". National Park Service. Retrieved 24 February 2013. 
  36. ^ "Glaciers/Glacial Features". Kenai Fjords National Park. National Park Service. Retrieved 8 February 2013. 
  37. ^ "The Harding Icefield". Kenai Fjords National Park. National Park Service. Retrieved 8 February 2013. 
  38. ^ "Nature & Science". Kenai Fjords National Park. National Park Service. Retrieved July 11, 2009. 
  39. ^ "Nature & Science". Kenai Fjords National Park. National Park Service. Retrieved 4 February 2013. 
  40. ^ "Ursus Arctos"Brown Bear - . Kenai Fjords National Park. National Park Service. Retrieved 11 February 2013. 
  41. ^ "Ursus americanus"Black Bear - . Kenai Fjords National Park. National Park Service. Retrieved 11 February 2013. 
  42. ^ "Alces alces gigas"Moose - . Kenai Fjords National Park. National Park Service. Retrieved 11 February 2013. 
  43. ^ "Oreamnos americanus"Mountain Goat - . Kenai Fjords National Park. National Park Service. Retrieved 11 February 2013. 
  44. ^ Catton, pp. 88-89
  45. ^ "Enhydra lutris"Sea Otter - . Kenai Fjords National Park. National Park Service. Retrieved 11 February 2013. 
  46. ^ "Phoca vitulina"Harbor Seal - . Kenai Fjords National Park. National Park Service. Retrieved 11 February 2013. 
  47. ^ a b "Eumetopias jubatus"Steller Sea Lion - . Kenai Fjords National Park. National Park Service. Retrieved 11 February 2013. 
  48. ^ Catton, pp. 91, 116
  49. ^ a b "Orcinus orca"Killer Whale - . Kenai Fjords National Park. National Park Service. Retrieved 11 February 2013. 
  50. ^ a b "Balaenoptera physalus"Fin Whale - . Kenai Fjords Nation al Park. National Park Service. Retrieved 11 February 2013. 
  51. ^ a b "Megaptera novaenglia"Humpback Whale - . Kenai Fjords National Park. National Park Service. Retrieved 11 February 2013. 
  52. ^ a b "Balaenoptera acutorostrata"Minke Whale - . Kenai Fjords National Park. National Park Service. Retrieved 11 February 2013. 
  53. ^ "Phocoenoides dalli"Dall's Porpoise - . Kenai Fjords National Park. National Park Service. Retrieved 11 February 2013. 
  54. ^ "Lagenorhynchus Obliquidens"Pacific White-Sided Dolphin - . Kenai Fjords National Park. National Park Service. Retrieved 11 February 2013. 
  55. ^ a b c "Fratercula corniculata and Fratercula cirrhata"Tufted Puffin and Horned Puffin - . Kenai Fjords National Park. National Park Service. Retrieved 13 February 2013. 
  56. ^ "Uria lomvia and Uria aalge"Common Murre and Thick-Billed Murre - . Kenai Fjords National Park. National Park Service. Retrieved 13 February 2013. 
  57. ^ "Marbled Murrelet". Kenai Fjords National Park. National Park Service. Retrieved 13 February 2013. 
  58. ^ "Plant Succession". Kenai Fjords National Park. National Park Service. Retrieved 11 February 2013. 
  59. ^ Catton, pp. 119–126
  60. ^ Catton, pp. 127–130

References

Archeological sites were also affected by the oil. A beach site near MacArthur Pass was discovered during cleanup operations. The site showed that contrary to earlier beliefs, portions of the park had been used over a long term by native peoples. The site proved to be particularly challenging to clean up without disturbing the area.[8]

The grounding of the oil tanker Exxon Valdez in Prince William Sound on March 24, 1989, produced extensive contamination of the Kenai Fjords coastline. By early April, Park Service personnel established oil containment boom lines across the mouths of salmon streams and conducted preliminary inventories of plants and animals that might be affected by the oil. The first oil arrived on April 10. In time, about 20 miles (32 km) of coastline was oiled, amounting to about 4% of the total coastline. Headlands were the most affected areas. The oil did not reach the fjords, repelled by heavy spring water flows from the land.[59] Clean-up was difficult, as the oil became a tarry emulsion that could not be skimmed, and had to be dredged. The first season's work stopped in September. Work resumed the next year and continued in 1991. That year Exxon settled with the federal and Alaskan governments, paying about $870 million into a restoration fund, some of which was earmarked for Kenai Fjords.[60]

Exxon Valdez oil spill

Harsh conditions at higher altitudes limit tree growth above the tree line, creating an alpine ecosystem. The tree line at Kenai Fjords is between 750 and 1,000 feet (230 and 300 m) above sea level. The alpine regions support shrubby grown to alders, devil's club, elderberry, lady fern, cow parsnip and other plants. Herbaceous plants can grow in areas with better soils, supporting grasses, Nootka lupine, fireweed and other perennial plants. Higher alpine regions support a dwarf shrub community less than 1 foot (30 cm) high, at a very slow rate of growth. Dwarf plants in this region include bog blueberry, partridgefoot, black crowberry and Aleutian mountainheath, all of which are vulnerable to damage from foot traffic.[55]

The plant communities at Kenai Fjords are shaped by glacial retreat. New lands exposed in former glacier beds are at first stony, lacking in soil. The first plants to appear in recently glaciated areas are lichens and mosses, with a few hardy plants such as dwarf fireweed and yellow dryas. These pioneers are followed by other plants as the moss and lichen break rock down into soil. In particular, Sitka alder is capable of fixing nitrogen, supporting itself and enriching the soil. Willows also appear at this stage. Willows and alders are followed by black cottonwoods, then Sitka spruce. The mature forest features Sitka spruce and mountain hemlocks, with an understory of devil's club, Alaska blueberry, elderberry, baneberry, watermelon berry and lady fern in the coniferous forest understory. A similar succession pattern is seen at the park's nunataks, exposed rock outcroppings in the Harding Icefield. Forested portions of the park are dominated by conifers, with deciduous forests confined to areas recently vacated by glaciers.[55][58]

Bird life at Kenai Fjords includes bald eagles,[49] the Peale's subspecies of peregrine falcon,[50] black-billed magpies,[52] and Steller's jays.[51] Maine birds include tufted and horned puffins,[55] common and thick-billed murres,[56] and marbled murrelets.[57]

Large terrestrial mammals in the park include Alaskan brown bears,[40] American black bears,[41] moose[42] and mountain goats.[43][44] Smaller mammals include beaver and river otter. Marine mammals include sea otters,[45] harbor seals[46] and Steller sea lions.[47][47][48] Cetaceans seen in park waters include orcas,[49] fin whales,[50] humpback whales,[51] minke whales,[52] Dall's porpoises[53] and Pacific white-sided dolphins.[54]

Kenai Fjords National Park is dominated by a glaciated landscape. The park's glaciers have retreated through the twentieth century, exposing new lands to colonization by plant and animal life. The park also features a significant marine environment.[39]

Harding Icefield
Fin whale in Kenai Fjords
Sea otter, Kenai Fjords

Wildlife and ecology

Kenai Fjords is extensively glaciated, with 51% of the park covered by ice. The Harding Icefield receives 60 feet (18 m) of snowfall per year.[36] More than thirty glaciers originate in the icefield, which first formed about 23,000 years ago. Icefield coverage has declined, with a 3% reduction in coverage over a 16-year study period.[37] The park's largest glacier is Bear Glacier. The most accessible glacier, and the only portion of the park accessible by road, is Exit Glacier.[38]

The park's landscape has been shaped by plate tectonics, with the Pacific Plate subducting beneath the North American Plate. The process has lowered the elevation of the Kenai Mountains, gradually pulling glacial features down into the sea, which is at the same time rising. The floors of the fjords can be from 600 to 1,000 feet (180 to 300 m) below the present sea level.[33] The motion of the North Pacific Plate has accreted a variety of terranes against the shoreline, so that the coastal region is a mixture of rocks that originated elsewhere, together with local igneous rock.[34] Predominant rock types include shale and graywacke, with greenstone, tuff and chert.[35] The erosive power of the glaciers produces sediment as rock flour coloring the waters around the toes of glaciers, carrying minerals into the ecosystem that support phytoplankton, which in turn sustain larger animals.[33]

Geology

The park can be reached from Seward, 130 mi (210 km) south of Anchorage at the southern terminus of the Seward Highway. It is only one of three national parks in Alaska that can be reached by road, via the Exit Glacier Nature Center. A network of trails from the Nature Center provide access to the glacier, and the 7.4-mile (11.9 km) Harding Icefield Trail.[31][32]

Map of Kenai Fjords National Park Also see resolution adjustable pdf map

The park lies on the southeastern side of the Kenai Peninsula, about 130 miles (210 km) south of Anchorage. The nearest large town is Seward, immediately to the east of the park on Resurrection Bay. The park includes the region's deeply indented glaciated coastline and its interior icefields. The most significant fjords include Aialik Bay, Harris Bay, McCarty Fjord and Nuka Bay. Much of the interior is covered by the Harding Icefield. The park's highest point is an unnamed peak of 6,450 feet (1,970 m) in the Kenai Mountains. The park is bordered on the west by Kenai National Wildlife Refuge and on the south by Kachemak Bay State Park.[30]

Geography

The park has established a cooperative relationship with the Alaska SeaLife Center, exchanging interpretive services.[29]

The park maintains public-use cabins and shelters in coastal areas and at the edge of the Harding Icefield. Some of these are on native corporation lands, with a portion of the use fee going to the native community.[28]

A sailboat near the mouth of Thumb Cove, in Resurrection Bay

Seward is a departure point and destination for large cruise ships from Celebrity Cruises, Holland America Line, Royal Caribbean International and others. Passenger traffic through Seward is projected at 68,000 for 2013.[25] Cruise tours originating from Seward provide access to the park via Resurrection Bay. Various companies offer tours, many guided by National Park Rangers. The tours provide views of land and marine wildlife, particularly Steller sea lions, puffins, Dall's porpoises, American black bear, Mountain goats, and humpback and orca whales, as well as natural sights such as the fjords and tidewater glaciers.[26] Seward is a destination for cruise ships. Bus tours from Seward visit Exit Glacier and boat tours visit other parts of the park[27]

Activities

Under the provisions of ANILCA the park included 119,000 acres (48,000 ha) of "native selected lands," property that was taken out of federal ownership and conveyed to Alaskan native corporations.[23] Most of the lands claimed were on the coastline. 30,295 acres (12,260 ha) were repurchased by the Park Service in the 1990s, retaining subsistence rights on about 9,000 acres (3,600 ha). This altered the original intent of the park to include subsistence claims, previously unrecognized.[6] A lodge was developed by the Port Graham community on Aialik Bay.[24]

On December 2, 1980, the ANILCA bill was signed into law by Jimmy Carter, converting Kenai Fjords to a national park.[19] The first park improvements focused on improving access to Exit Glacier.[20] In 1982 a general management plan for the park was finalized, designating Exit Glacier as "front-country," the fjords as "back-country," and the icefield as wilderness.[21] The park was initially administered by a small cadre of permanent and seasonal rangers and technicians who put considerable emphasis on community liaison.[22]

Exit Glacier

National Park

Legislation stalled in Congress during the Watergate scandal, and was not pursued again until the Carter administration. Secretary of the Interior Cecil D. Andrus proposed a 410,000-acre (170,000 ha) Kenai Fjords National Park.[16] Alaskan opposition to ANILCA prompted President Jimmy Carter to proclaim Kenai Fjords National Monument under the provisions of the Antiquities Act on December 1, 1978, pending final passage of an Alaskan lands bill.[17] No visitor facilities or full-time local management structure resulted from the monument's proclamation. A single ranger was assigned to Seward as a local liaison.[18]

The earliest proposals for a national park at the Kenai Fjords was raised in the 1970s. In 1971 the Seward National Recreation Area was proposed for the area between the head of Resurrection Bay and Turnagain Arm, extending east to Whittier and west to Exit Glacier. This proposal allowed logging and mining in the area. Although the proposal had support in Congress and from the US Forest Service and the Bureau of Land Management, it was overcome by difficulties with native land claims.[13] Internal Park Service documents envisioned an 800,000-acre (320,000 ha) park protecting the coast and the icefield, but this conflicted with the Seward National Recreation Area and a proposed expansion of the Kenai National Moose Range. Another proposal placed the Aialik Peninsula under US Fish and Wildlife Service jurisdiction. On March 15, 1972, four areas of the Kenai Peninsula were set aside under the ANCSA for federal protected areas.[14] The same day the National Park Service formed an Alaska Task Force to study proposed park lands. The Kenai Fjords region was designated Study Area 11. Negotiations between the Park Service, Forest Service, Fish and Wildlife Service and the Chugach Alaska Corporation resulted in a decision by the Department of the Interior to make the Park Service the lead agency for the Kenai Fjords area. In 1973 the Nixon administration proposed the Harding Icefield–Kenai Fjords National Monument as part of the ANILCA legislation. The proposed monument totaled 300,000 acres (120,000 ha) in three areas: the icefield and two island groups.[15]

Aialik Glacier

[12] (ACNSA). The Kenai Fjords area was not considered to be of the first priority for park designation under the ACNSA.Alaska Native Claims Settlement Act Follow-up action by Hartzog brought the Park Service into discussions over the [11]

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