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{{Infobox protected area
{{Infobox_protected_area | name = Lake Clark National Park and Preserve
| name = Lake Clark National Park and Preserve
| iucn_category = II
| iucn_category = VI
| image = US_Locator_Blank.svg
| photo = Lake Clark National Park.jpg
| caption =
| photo_caption = Lake Clark and the Chigmit Mountains
| locator_x = 27
| map = USA Alaska |relief=1
| locator_y = 165
| map_caption =
| location = [[Alaska]], [[United States|USA]]
| map_width = 250
| nearest_city = [[Anchorage, Alaska|Anchorage, AK]]
| location = [[Lake and Peninsula Borough, Alaska|Lake and Peninsula Borough]], [[Kenai Peninsula Borough, Alaska|Kenai Peninsula Borough]], [[Bethel Census Area, Alaska|Bethel Census Area]], and [[Matanuska-Susitna Borough, Alaska|Matanuska-Susitna Borough]], [[Alaska]], [[United States|USA]]
| lat_degrees = 60
| nearest_city = [[Anchorage, Alaska|Anchorage]]
| lat_minutes = 58
| lat_seconds = 0
| lat_d = 60
| lat_direction = N
| lat_m = 58
| long_degrees = 153
| lat_s = 00
| long_minutes = 25
| lat_NS = N
| long_seconds = 0
| long_d = 153
| long_direction = W
| long_m = 25
| long_s = 00
| area = 4,030,025 acres (16,308 km²)
| long_EW = W
| established = [[December 2]], [[1980]]
| area = {{convert|4,030,015|acre}}<ref name="area">{{NPS area|year=2011|accessdate=2012-03-07}}</ref>
| visitation_num = 4,906
| established = December 2, 1980
| visitation_year = 2004
| visitation_num = 11,639
| visitation_year = 2012
| visitation_ref = <ref name="visits">{{NPS Visitation|accessdate=2012-02-28}}</ref>
| governing_body = [[National Park Service]]
| governing_body = [[National Park Service]]
}}
}}
Established in [[1980]] by the [[Alaska National Interest Lands Conservation Act]], '''Lake Clark National Park and Preserve''' is a [[United States]] [[national park|National Park]] in southwestern [[Alaska]]. The park includes many streams and lakes vital to the [[Bristol Bay]] [[salmon]] fishery. The park allows a wide variety of recreational activities year-round.


'''Lake Clark National Park and Preserve''' is a [[United States]] [[national park|National Park]] in southwestern [[Alaska]]. It was first proclaimed a [[national monument (United States)|national monument]] in 1978, then established as a national park and preserve in 1980 by the [[Alaska National Interest Lands Conservation Act]]. The park includes many streams and lakes vital to the [[Bristol Bay]] [[salmon]] fishery, including its namesake [[Lake Clark (Alaska)|Lake Clark]]. A wide variety of recreational activities may be pursued in the park and preserve year-round. Located about {{convert|100|mi|km}} southwest of [[Anchorage, Alaska|Anchorage]], the park includes a variety of features not found together in any of the other Alaska Parks: the junction of three mountain ranges, a coastline with rainforests along the [[Cook Inlet]], a plateau with alpine tundra on the west, glaciers, glacial lakes, major salmon-bearing rivers, and two volcanoes, [[Mount Redoubt]] and [[Mount Iliamna]]. Redoubt is active, erupting in 1989 and 2009. The wide variety of ecosystems in the park mean that virtually all major Alaskan animals, terrestrial and marine, may be seen in and around the park. Salmon, particularity [[sockeye salmon]], play a major role in the ecosystem and the local economy. The [[Kvichak River]] is the world's most productive watershed for sockeye salmon.
[[Image:Lake Clark National Park.jpg|left|300px|thumb|Lake Clark]]<br clear=left>
Large populations of [[grizzly bear|brown bear]]s are attracted as a result, to feed on the spawning salmon in the [[Kijik River]] and at [[Silver Salmon Creek]], and as a result bear viewing is a common activity in the park.<ref name="Silver Salmon Creek">{{cite web|title=Silver Salmon Creek|url=http://www.nps.gov/lacl/planyourvisit/silver-salmon-creek.htm|work=Lake Clark National Park and Preserve|publisher=National Park Service|accessdate=December 7, 2013}}</ref>


No roads lead to the park and it can only be reached by boat or small aircraft, typically [[floatplane]]s. The major settled area in the park is [[Port Alsworth, Alaska|Port Alsworth]] on Lake Clark in the southwestern corner of the park. Five other settlements are within the park, populated mainly by Dena'ina natives. Prior to the park's establishment isolated cabins were scattered around the region, the most notable belonging to [[Richard Proenneke]], whose films documenting his solitary life at [[Twin Lakes (Alaska)|Twin Lakes]] were made into ''Alone in the Wilderness'' in 2003.
[[Lake Clark]] has been called "the essence of Alaska", for it concentrates in a relatively small area of the [[Alaska Peninsula]], Southwest of Anchorage, a variety of features not found together in any of the other Alaska Parks: the junction of three mountain ranges, (the Alaska Range from the North, the [[Aleutian Range]] from the South, and the park's own rugged [[Chigmit Mountains]]), two active volcanoes ([[Mount Iliamna|Iliamna]] and [[Mount Redoubt|Redoubt]]), a coastline with rainforests on the East (similar to South East Alaska), and a plateau with tundra on the West (similar to Arctic Alaska), and turquoise lakes.


Lake Clark was proclaimed a national monument by President [[Jimmy Carter]] using the [[Antiquities Act]] on December 1, 1978, Lake Clark's status was changed to national park and preserve in 1980 by Congress, and about two-thirds was designated wilderness. While both sport and subsistence hunting are permitted in the [[national preserve]] lands, only subsistence hunting by local residents is permitted within the [[national park]].
No roads lead to the park and it can only be reached by small aircraft, floatplanes being the best method. The park, one of the least visited in the [[National Park Service|National Park System]], averages fewer than 5,000 visitors per year.


==Geography==
== External links ==
[[File:Lake clark map.png|thumb|Map of Lake Clark National Park. Also see [http://www.nps.gov/pinn/planyourvisit/upload/PINNmap1-1.pdf resolution adjustable pdf map]]]
* [http://www.nps.gov/lacl Official NPS site]
Lake Clark National Park and Preserve covers {{convert|4030015|acre|ha}} at the base of the [[Alaska Peninsula]] in [[southcentral Alaska]], about {{convert|100|mi|km}} southwest of [[Anchorage, Alaska|Anchorage]]. Of the total area, about {{convert|2637000|acre|ha}} lie in the park and {{convert|1400000|acre|ha}} in the preserve. The park and associated [[national preserve]] extend from the [[Cook Inlet]] across the [[Chigmit Mountains]] and the [[Neacola Mountains]], on the northern end of the [[Aleutian Range]], and on into the Alaska interior. [[Lake Clark]] is the largest lake in the park, on the southwest corner of the park. The national preserve lands adjoin park lands on the west, offering both subsistence and sport hunting, in contrast to parklands, where only subsistence hunting by local residents is allowed. The extreme southwest section of the preserve includes Alaskan Native corporation lands, which are not open to the public. Most of the park section is designated as [[National Wilderness Preservation System|wilderness]]. The eastern part of the park near the Cook Inlet includes two active volcanoes, [[Mount Redoubt]] and [[Mount Iliamna]]. A third, [[Mount Spurr]], is just outside the park to the east. The chief river in the park is the [[Kvichak River]]. Another large river, the [[Tlikakila River|Tlikakita]], runs across the park from its source at Summit Lake to Lake Clark, emerging from the lake and the park as the [[Newhalen River]].<ref name=npslaclmap1>{{cite web|title=Lake Clark National Park map|url=http://www.nps.gov/lacl/planyourvisit/upload/Lake%20Clark%20Brochure%20Map%20Side.pdf|publisher=National Park Service|accessdate=28 February 2013}}</ref><ref name=npsakso1>{{cite web|title=Lake Clark National Park and Preserve|url=http://www.nps.gov/akso/akarc/cr_lacl.htm|publisher=National Park Service|accessdate=28 February 2013}}</ref>
* [http://www.photo-mark.com/articles/lakeclark/index.html Exploring the Sublime in Lake Clark National Park ]
* [http://www.terragalleria.com/parks/np.lake-clark.html Photos of Lake Clark National Park - Terra Galleria]


The park is not accessible by roads. Access is solely by air taxi or by boat along the Cook Inlet coast and Lake Clark.<ref name=npslacl1>{{cite web|title=Directions|url=http://www.nps.gov/lacl/planyourvisit/directions.htm|work=Lake Clark National Park and Preserve|publisher=National Park Service|accessdate=28 February 2013}}</ref> Since much of the movement in the area is by air, the mountains present a significant barrier to air traffic. [[Lake Clark Pass]], at {{convert|1050|ft|m}} provides a way through the mountains by air at low elevation, and is the main route between Anchorage and western Alaska.<ref name=npslacl15>{{cite web|title=Mountains|url=http://www.nps.gov/lacl/naturescience/mountains.htm|work=National Park Service|publisher=National Park Service|accessdate=1 March 2013}}</ref>
{{National parks of the United States}}


The main inhabited place in the park is [[Port Alsworth, Alaska|Port Alsworth]] on Lake Clark, with a Park Service visitor center and a number of privately operated lodges.<ref name=npslacl26>{{cite web|title=Operating Hours & Seasons|url=http://www.nps.gov/lacl/planyourvisit/hours.htm|work=Lake Clark National Park and Preserve|publisher=National Park Service|accessdate=2 March 2013}}</ref> Air taxis make regular trips between Port Alsworth and outside communities.<ref name=npslacl28>{{cite web|title=Things To Do|url=http://www.nps.gov/lacl/planyourvisit/things2do.htm|work=Lake Clark National Park and Preserve|publisher=National Park Service|accessdate=2 March 2013}}</ref> Other private lodges are scattered around the park.<ref name=npslacl29>{{cite web|title=Lodging|url=http://www.nps.gov/lacl/planyourvisit/lodging.htm|work=Lake Clark National Park and Preserve|publisher=National Park Service|accessdate=2 March 2013}}</ref>
{{Alaska-geo-stub}}{{Protected-area-stub}}


===Geology===
[[Category:Landmarks in Alaska]]
The park has four main physiographic regions. The upthrust granite Chigmit Mountains connect the Alaska Range to the Aleutian Range. Superimposed on these mountains and little to the east of the main range are the two [[stratovolcano]]es, Redoubt {{convert|10197|ft|m}} high, and Iliamna at {{convert|10016|ft|m}}. Glaciers have altered the mountains, carving cirques and U-shaped valleys into the range, which end abruptly on the east at the steep coast in deep bays or in outwash flats. On the west the glaciers have cut deeply enough to create lakes, dammed by terminal moraines at their downstream ends.<ref name=npsakso1/> Lake Clark, the largest, is the sixth largest lake in Alaska, {{convert|860|ft|m}} deep and {{convert|42|mi|km}} long.<ref name=npslacl14>{{cite web|title=Fresh Water Systems|url=http://www.nps.gov/lacl/naturescience/fresh-water-systems.htm|work=Lake Clark National Park and Preserve|publisher=National Park Service|accessdate=1 March 2013}}</ref>
[[Category:National Parks of the United States]]

[[Category:National parks in Alaska]]
The park includes a variety of unrelated rocks. The core of the Chigmit Mountains is a granite pluton forced upwards<ref name=npslacl11>{{cite web|title=Glaciers|url=http://www.nps.gov/lacl/naturescience/glaciers.htm|work=Lake Clark National Park and Preserve|publisher=National Park Service|accessdate=1 March 2013}}</ref> by the collision of the [[Pacific plate]] and the [[North American plate]]. Rocks in coastal areas are sedimentary in origin, and contain abundant fossils.<ref name=npslacl12>{{cite web|title=Fossils|url=http://www.nps.gov/lacl/naturescience/fossils.htm|work=Lake Clark National Park and Preserve|publisher=National Park Service}}</ref> Volcanic rocks intrude through these native rocks.
[[Category:National Preserves of the United States]]

===Volcanoes===
[[File:MtRedoubtedit1.jpg|thumb|Redoubt volcano in eruption]]
Redoubt is the park's active volcano. {{convert|10197|ft|m}} high, about {{convert|10|km|mi}} in diameter and with a volume of about 30 to 35 cubic kilometers, the stratovolcano rises through the Chigmit [[batholith]]. It has a {{convert|1.8|km|mi|adj=on}} wide summit crater. The [[Drift Glacier]] originates there and flows through a gap in the rim.<ref name=avo2>{{cite web|title=Redoubt Volcano description and information|url=http://www.avo.alaska.edu/volcanoes/volcinfo.php?volcname=Redoubt|publisher=Alaska Volcano Observatory|accessdate=1 March 2013}}</ref> Redoubt's most recent active phase began on December 14, 1989, with ash eruptions. The ash clouds affected air traffic, causing all four engines to fail on [[KLM Flight 867]] when it passed overhead at {{convert|25000|ft}}. The 747 was able to safely return to Anchorage. Four other airplanes were damaged in the same event, which brought greater awareness of the hazards associated with high-altitude volcanic ash.<ref name=npslacl17>{{cite web|title=Volcanoes|url=http://www.nps.gov/lacl/naturescience/volcanoes.htm|work=Lake Clark National Park and Preserve|publisher=National Park Service|accessdate=1 March 2013}}</ref><ref name=campbell1>{{cite news|last=Campbell|first=Larry|title=A look back at Alaska volcano’s near-downing of a 747|url=http://www.heraldnet.com/article/20100418/NEWS02/704189878|accessdate=1 March 2013|newspaper=Everett Daily herald|date=April 18, 2010}}</ref><ref name=avo3>{{cite web|title=About Alaska's Volcanoes|url=http://www.avo.alaska.edu/volcanoes/about.php|publisher=Alaska Volcano Observatory|accessdate=1 March 2013}}</ref> Redoubt was quiet after 1990 until March and April 2009 when it [[2009 Mount Redoubt eruptive activity|erupted]] with [[pyroclastic flows]] that melted ice, creating [[lahar]]s on the [[Drift River]],<ref name=npslacl17/> endangering the [[Drift River Terminal Facility]] to the east of the park.

[[File:Mount Iliamna.jpg|thumb|Iliamna volcano]]
Iliamna has not been recently active. Like Redoubt, it stands on Jurassic granite basement rock, but has been significantly altered by glacial activity that has cut away the slopes on the southern and eastern sides.<ref name=avo4>{{cite web|title=Iliamna Volcano description and information|url=http://www.avo.alaska.edu/volcanoes/volcinfo.php?volcname=Iliamna|publisher=Alaska Volcano Observatory|accessdate=1 March 2013}}</ref> The mountain has experienced seismic activity from time to time that has raised alert levels while the earthquake flurries have persisted. The peak has active [[fumarole]]s that occasionally produce visible vapor plumes.<ref name=avo5>{{cite web|title=Iliamna reported activity|url=http://www.avo.alaska.edu/volcanoes/activity.php?volcname=Iliamna&eruptionid=703&page=basic|publisher=Alaska Volcano Observatory|accessdate=1 March 2013}}</ref>

==Activities==
The park and preserve offer a variety of possible activities, including kayaking, rafting, hiking and camping.<ref name=npslacl2>{{cite web|title=Outdoor Activities|url=http://www.nps.gov/lacl/planyourvisit/outdooractivities.htm|work=Lake Clark National Park and Preserve|publisher=National Park Service|accessdate=28 February 2013}}</ref> Most of the large Alaskan animals are present and viewable in the park.<ref name=npslacl3>{{cite web|title=Wildlife Viewing|url=http://www.nps.gov/lacl/planyourvisit/wildlife-viewing.htm|work=Lake Clark National Park and Preserve|publisher=National Park Service|accessdate=28 February 2013}}</ref> Fishing is allowed in both the park and preserve,<ref name=npslacl5>{{cite web|title=Fishing|url=http://www.nps.gov/lacl/planyourvisit/fishing.htm|work=Lake Clark National Park and Preserve|publisher=National Park Service|accessdate=28 February 2013}}</ref> while sport hunting is permitted in the preserve.<ref name=npslacl6>{{cite web|title=Hunting|url=http://www.nps.gov/lacl/planyourvisit/hunting.htm|work=Lake Clark National Park and Preserve|publisher=National Park Service|accessdate=28 February 2013}}</ref>

==Ecology==
[[File:Kijik-fish-NPS1.jpg|thumb|Sockeye salmon in the Kijik River]]
Lake Clark preserves a wide variety of Alaskan landscapes and ecosystems, corresponding to its four main physiographic areas. The coastal sections running along the Cook Inlet from [[Tuxedni Bay]] to [[Chinitna Bay]] include coastline and marine ecosystems. The mountains of the Alaska, Aleutian and Chigmit Ranges with their glaciers form a second region. On either side of the mountains the valley, lake and foothill areas present a glacially altered landscape.<ref name=npslacl7>{{cite web|title=Natural Features and Ecosystems|url=http://www.nps.gov/lacl/naturescience/natural-features-and-ecosystems.htm|work=Lake Clark National Park and Preserve|publisher=National Park Service|accessdate=28 February 2013}}</ref> [[taiga|Boreal forest]] dominates the lower sections of the southwest part of the park, with [[white spruce|white]] and [[black spruce|black]] spruce making up most of the coniferous trees. White spruce have been affected by [[spruce bark beetle]] infestation, and [[Chrysomyxa ledi var. rhododendri|spruce needle rust]] outbreaks have been so heavy that the surface of Lake Clark has been colored orange by spores.<ref name=npslacl10>{{cite web|title=Forests|url=http://www.nps.gov/lacl/naturescience/forests.htm|work=Lake Clark National Park and Preserve|publisher=National Park Service|accessdate=1 March 2013}}</ref> Farther north and west lie the [[tundra]] regions,<ref name=npsakso1/> primarily the result of elevation. The tundra supports caribou and ptarmigans.<ref name=npslacl16>{{cite web|title=Tundra|url=http://www.nps.gov/lacl/naturescience/tundra.htm|work=Lake Clark National Park and Preserve|publisher=National Park Service|accessdate=1 March 2013}}</ref>

Salt marshes along the Cook Inlet represent one of the most productive ecosystems in the park. They account for under 1% of the park's area, but provide a source of food in early summer for both brown and black bears.<ref name=npslacl13>{{cite web|title=Coastal Salt Marshes|url=http://www.nps.gov/lacl/naturescience/coastal-salt-marshes.htm|work=Lake Clark National Park and Preserve|publisher=National Park Service|accessdate=1 March 2013}}</ref> Lake Clark's coastal areas are rated as some of the top bear viewing destinations in the world, along with the coast of [[Katmai National Park]]. Most bears are concentrated at Chinitna Bay or Silver Salmon Creek when the fish are running. Chinitna Bay is considered by some to be one of the top bear viewing destinations in Alaska.<ref name=npslacl20>{{cite web|title=Chinitna Bay|url=http://www.nps.gov/lacl/planyourvisit/chinitna-bay.htm|work=Lake Clark National Park and Preserve|publisher=National Park Service|accessdate=2 March 2013}}</ref><ref name=npslacl14/> [[Tuxedni Bay]], north of Chinitna Bay, also provides excellent bear viewing; up to 20 brown bears have been spotted feeding on [[clam]]s and [[sedge]]s at a time. Fewer people visit the bay and therefore it is easier to view bears in peace.<ref>{{cite web|title=Tuxedni Bay: Grizzy Viewing With Little Traffic|url=http://www.alaska.org/detail/tuxedni-bay|publisher=Alaska.org|accessdate=February 6, 2015}}</ref> Inland areas of the park also provide bear viewing. [[Crescent Lake (Alaska)|Crescent Lake]] provides excellent bear viewing in June, July and August. Both grizzly and black bears are present, but grizzly bears are more common and seen more often, since black bears are shier and are easily displaced by their larger cousins.<ref>{{cite web|title=Crescent Lake|url=http://www.nps.gov/lacl/planyourvisit/crescent-lake.htm|work=Lake Clark National Park and Preserve|publisher=National Park Service|accessdate=February 6, 2015}}</ref> On the other side of the park, the [[Kvichak River]] is the world's most productive watershed for [[sockeye salmon]], whose offspring account for 33% of the species' catch in the United States and 16% of world production. Salmon are so plentiful that a wolf pack at Lake Clark has been documented as the only salmon-dependent pack in the world.<ref name=npslacl14/>

Major terrestrial mammals in the park include brown bears, moose, caribou, [[Dall's sheep]] and [[gray wolf|gray wolves]]. Smaller mammals include martens, red fox, [[wolverine]]s, river otters, beaver and lynx. Marine mammals include sea lions, [[beluga whale]]s [[harbor seal]]s and porpoises.<ref name=npslacl19>{{cite web|title=Wildlife Viewing|url=http://www.nps.gov/lacl/planyourvisit/wildlife-viewing.htm|work=Lake Clark National Park and Preserve|publisher=National Park Service|accessdate=2 March 2013}}</ref> Both [[American black bear|black]] and [[grizzly bear|brown bear]]s are present in the park. Black bears use all areas of the park and preserve, except the higher elevations. Brown bears are most numerous along the coast. A recent survey found that about 219 bears graze in salt marshes during the summer in the coastal areas of the park.<ref name=Bears>{{cite web|title=Bears|url=http://www.nps.gov/lacl/naturescience/bears.htm|work=Lake Clark National Park and Preserve|publisher=National Park Service|accessdate=December 9, 2013}}</ref> [[Caribou]] have recently declined in population size from 200,000 to 30,000 due to an unknown cause.<ref name=Caribou>{{cite web|title=Caribou|url=http://www.nps.gov/lacl/naturescience/caribou.htm|work=Lake Clark National Park and Preserve|publisher=National Park Service|accessdate=December 9, 2013}}</ref>

Weather in the park is extremely variable. Marine air from the Pacific Ocean meets drier air of the continental airmass over the park. The average summer temperature is between {{convert|50|and|65|F|C}} with highs around {{convert|68|F|C}} and typical winter lows of {{convert|1|F|C}}. Snow can happen at any time.<ref name=npslacl18>{{cite web|title=Weather|url=http://www.nps.gov/lacl/planyourvisit/weather.htm|work=Lake Clark National Park and Preserve|publisher=National Park Service|accessdate=2 March 2013}}</ref>

==History==
[[File:Lake Clark.JPG|thumb|Lake Clark]]
The earliest human presence known in the area of Lake Clark was at Bristol Bay. People of the [[Paleo-Arctic Tradition]] lived there between 10,000 years before the present and 7500 BP. These people were followed by the [[Archaic period in North America|northern Archaic tradition]] between 6,000 BP and 4,000 BP. Two sites from this tradition have been documented in the park. The [[Arctic small tool tradition]] followed from about 5,000 BP to 3,000 BP. The [[Norton tradition]] came between 2,200 BP and 1,000 BP, concentrated around Bristol Bay. The [[Thule Tradition]] was established around 2,000 BP and lasted until historic times. The [[Northern Athabaskan languages|northern Athabaskan]] Dena'ina presently live in the area. [[Kijik, Alaska|Kijik]] village is the primary archaeological site in the park, inhabited by Dena'ina until the early 20th century.<ref name=npsakso1/> Settlements have also been documented around Chinitna Bay.<ref name=npslacl23>{{cite web|title=Chinitna Bay Prehistory|url=http://www.nps.gov/lacl/historyculture/chinitna-bay-prehistory.htm|work=Lake Clark National Park and Preserve|publisher=National Park Service|accessdate=2 March 2013}}</ref>

The Cook Inlet was surveyed by British Captain [[James Cook]] in 1778. In succeeding decades Russian traders established themselves in the region. The major settlement during the 19th century was at Kijik, with a population in the low hundreds. By the 1890s American traders had arrived in the area, meeting a native population that had been greatly reduced by imported diseases.<ref name=npsakso1/> Kijik has been designated a [[National Historic Landmark]] district.<ref name=npslacl25>{{cite web|title=Kijik|url=http://www.nps.gov/lacl/historyculture/kijik.htm|work=Lake Clark National Park and Preserve|publisher=National Park Service|accessdate=2 March 2013}}</ref>

In 1930 the first floatplane landed on Lake Clark. In 1942 the first air taxi service was provided to Lake Clark, run by Leon "Babe" Alsworth, Sr. to Port Alsworth.<ref name=npslacl30>{{cite web|title=The Age of Air Travel|url=http://www.nps.gov/lacl/historyculture/age-of-air-travel.htm|work=Lake Clark National Park and Preserve|publisher=National Park Service|accessdate=2 March 2013}}</ref> Apart from Port Alsworth, there are five other communities within the park: [[Lime Village, Alaska|Lime Village]], [[Nondalton, Alaska|Nondalton]], [[Iliamna, Alaska|Iliamna]], [[Newhalen, Alaska|Newhalen]] and [[Pedro Bay, Alaska|Pedro Bay]]. Most local residents are Dena'ina.<ref name=npslacl31>{{cite web|title=Who lives in the Lake Clark area today?|url=http://www.nps.gov/lacl/historyculture/who-lives-at-lake-clark.htm|work=Lake Clark National Park and Preserve|publisher=National Park Service}}</ref>

During the 20th century the future park area was lightly populated by people with a high tolerance for solitude. One such person was [[Richard Proenneke]], a former Iowan who came to Alaska in 1949. Proenneke lived at [[Twin Lakes (Alaska)|Twin Lakes]] from 1968 to 1999 in a cabin he built himself, feeding himself through subsistence hunting and by salvaging meat from animals left by sport hunters. In 1973 a friend published the book ''One Man's Wilderness: An Alaskan Odyssey'' based on his journals. Some of the movie footage shot by Proenneke of his life at the lake was compiled into the documentary, ''Alone in the Wilderness''. Produced posthumously, it has become popular on public television in the United States.<ref name=aitw1>{{cite web|title=Alone in the Wilderness|url=http://www.aloneinthewilderness.com/later_years.html|publisher=Bob Swerer Productions|accessdate=2 March 2013}}</ref><ref name=npslacl21>{{cite web|title=Richard L. Proenneke, Wilderness Steward|url=http://www.nps.gov/lacl/historyculture/richard-l-proenneke.htm|work=Lake Clark National Park and Preserve|publisher=National Park Service|accessdate=2 March 2013}}</ref> Proenneke's cabin is now owned by the park service and listed on the [[National Register of Historic Places]].<ref name=npslacl24>{{cite web|title=Proenneke's Cabin|url=http://www.nps.gov/lacl/historyculture/proennekes-cabin.htm|work=Lake Clark National Park and Preserve|publisher=National Park Service|accessdate=2 March 2013}}</ref>

Lake Clark was proclaimed a [[national monument (United States)|national monument]] on December 1, 1978, by President [[Jimmy Carter]], using his authority under the [[Antiquities Act]]. In 1980, Congress passed the [[Alaska National Interest Lands Conservation Act]] (ANILCA), which established the unit as a national park and preserve.<ref name=npsakso1/>

A large open-pit mine was proposed in 2007 near the western boundary of the park. The [[Pebble Mine]] is proposed to mine [[molybdenum]], gold and copper from an open pit about {{convert|2|mi|km}} across and thousands of feet deep. Another ore body is proposed to be exploited using underground mining. [[Tailings]] from the mine are to be stored behind dams on the site, and roads and a deepwater port will be required.<ref name=pebble1>{{cite web|title=Plan|url=http://www.pebblepartnership.com/plan.html|publisher=Pebble Partnership|accessdate=2 March 2013}}</ref> Concerns about the mine's relationship to the park center on dust contamination and on the mine's possible effect on the sockeye salmon population.<ref name=npsmine1>{{cite web|title=Concerns Regarding Large-scale Mining on the Western Boundary of the Park|url=http://www.nps.gov/lacl/parknews/upload/NPS-Concerns-Regarding-Mining-Adjacent-Lake-Clark-NPP-Feb-2013-Final.pdf|work=Lake Clark National Park and Preserve|publisher=National Park Service|accessdate=2 March 2013}}</ref>

The {{convert|2619550|acre|ha|adj=on}} Lake Clark Wilderness covers much of the park's area, excluding preserve lands and the Cook Inlet coast. The area includes three [[Wild and Scenic Rivers]]: the [[Chilikadrotna River]], the [[Mulchatna River]] and the [[Tlikakila River]].<ref name=wilderness1>{{cite web|title=Lake Clark Wilderness|url=http://www.wilderness.net/NWPS/wildView?WID=307|publisher=wilderness.net|accessdate=2 March 2013}}</ref>

==See also==
{{Portal|Alaska}}
* [[National Register of Historic Places listings in Lake Clark National Park and Preserve]]

== References ==
{{reflist|2}}

==Bibliography==
* Gaul, Karen (2007) [http://www.nps.gov/lacl/historyculture/nanutset.htm ''Nanutset ch'u Q'udi Gu (Before Our Time and Now)''] National Park Service, ISBN 978-0-9796432-3-1

== External links ==
{{Commons category|Lake Clark National Park}}
* [http://www.nps.gov/lacl Lake Clark National Park and Preserve] National Park Service website
* [http://www.nps.gov/akso/akarc/cr_lacl.htm Lake Clark National Park and Preserve] at the National Park Service Alaska Regional Office
*[http://lakeclarkinn.com/lake-clark-national-park-maps / A satellite view of Lake Clark NP with points of interest]

{{National parks of the United States}}
{{Protected Areas of Alaska}}


[[de:Lake-Clark-Nationalpark]]
[[Category:Lake Clark National Park and Preserve| ]]
[[Category:Alaska Range]]
[[fr:Lake Clark National Park]]
[[Category:Protected areas of Bethel Census Area, Alaska]]
[[hu:Lake Clark Nemzeti Park]]
[[Category:Protected areas of Kenai Peninsula Borough, Alaska]]
[[Category:Protected areas of Lake and Peninsula Borough, Alaska]]
[[Category:Protected areas of Matanuska-Susitna Borough, Alaska]]
[[Category:Protected areas established in 1980]]

Revision as of 04:12, 4 October 2015

Lake Clark National Park and Preserve
IUCN category VI (protected area with sustainable use of natural resources)
Lake Clark and the Chigmit Mountains
Map showing the location of Lake Clark National Park and Preserve
Map showing the location of Lake Clark National Park and Preserve
LocationLake and Peninsula Borough, Kenai Peninsula Borough, Bethel Census Area, and Matanuska-Susitna Borough, Alaska, USA
Nearest cityAnchorage
Area4,030,015 acres (1,630,889 ha)[1]
EstablishedDecember 2, 1980
Visitors11,639 (in 2012)[2]
Governing bodyNational Park Service

Lake Clark National Park and Preserve is a United States National Park in southwestern Alaska. It was first proclaimed a national monument in 1978, then established as a national park and preserve in 1980 by the Alaska National Interest Lands Conservation Act. The park includes many streams and lakes vital to the Bristol Bay salmon fishery, including its namesake Lake Clark. A wide variety of recreational activities may be pursued in the park and preserve year-round. Located about 100 miles (160 km) southwest of Anchorage, the park includes a variety of features not found together in any of the other Alaska Parks: the junction of three mountain ranges, a coastline with rainforests along the Cook Inlet, a plateau with alpine tundra on the west, glaciers, glacial lakes, major salmon-bearing rivers, and two volcanoes, Mount Redoubt and Mount Iliamna. Redoubt is active, erupting in 1989 and 2009. The wide variety of ecosystems in the park mean that virtually all major Alaskan animals, terrestrial and marine, may be seen in and around the park. Salmon, particularity sockeye salmon, play a major role in the ecosystem and the local economy. The Kvichak River is the world's most productive watershed for sockeye salmon. Large populations of brown bears are attracted as a result, to feed on the spawning salmon in the Kijik River and at Silver Salmon Creek, and as a result bear viewing is a common activity in the park.[3]

No roads lead to the park and it can only be reached by boat or small aircraft, typically floatplanes. The major settled area in the park is Port Alsworth on Lake Clark in the southwestern corner of the park. Five other settlements are within the park, populated mainly by Dena'ina natives. Prior to the park's establishment isolated cabins were scattered around the region, the most notable belonging to Richard Proenneke, whose films documenting his solitary life at Twin Lakes were made into Alone in the Wilderness in 2003.

Lake Clark was proclaimed a national monument by President Jimmy Carter using the Antiquities Act on December 1, 1978, Lake Clark's status was changed to national park and preserve in 1980 by Congress, and about two-thirds was designated wilderness. While both sport and subsistence hunting are permitted in the national preserve lands, only subsistence hunting by local residents is permitted within the national park.

Geography

Map of Lake Clark National Park. Also see resolution adjustable pdf map

Lake Clark National Park and Preserve covers 4,030,015 acres (1,630,889 ha) at the base of the Alaska Peninsula in southcentral Alaska, about 100 miles (160 km) southwest of Anchorage. Of the total area, about 2,637,000 acres (1,067,000 ha) lie in the park and 1,400,000 acres (570,000 ha) in the preserve. The park and associated national preserve extend from the Cook Inlet across the Chigmit Mountains and the Neacola Mountains, on the northern end of the Aleutian Range, and on into the Alaska interior. Lake Clark is the largest lake in the park, on the southwest corner of the park. The national preserve lands adjoin park lands on the west, offering both subsistence and sport hunting, in contrast to parklands, where only subsistence hunting by local residents is allowed. The extreme southwest section of the preserve includes Alaskan Native corporation lands, which are not open to the public. Most of the park section is designated as wilderness. The eastern part of the park near the Cook Inlet includes two active volcanoes, Mount Redoubt and Mount Iliamna. A third, Mount Spurr, is just outside the park to the east. The chief river in the park is the Kvichak River. Another large river, the Tlikakita, runs across the park from its source at Summit Lake to Lake Clark, emerging from the lake and the park as the Newhalen River.[4][5]

The park is not accessible by roads. Access is solely by air taxi or by boat along the Cook Inlet coast and Lake Clark.[6] Since much of the movement in the area is by air, the mountains present a significant barrier to air traffic. Lake Clark Pass, at 1,050 feet (320 m) provides a way through the mountains by air at low elevation, and is the main route between Anchorage and western Alaska.[7]

The main inhabited place in the park is Port Alsworth on Lake Clark, with a Park Service visitor center and a number of privately operated lodges.[8] Air taxis make regular trips between Port Alsworth and outside communities.[9] Other private lodges are scattered around the park.[10]

Geology

The park has four main physiographic regions. The upthrust granite Chigmit Mountains connect the Alaska Range to the Aleutian Range. Superimposed on these mountains and little to the east of the main range are the two stratovolcanoes, Redoubt 10,197 feet (3,108 m) high, and Iliamna at 10,016 feet (3,053 m). Glaciers have altered the mountains, carving cirques and U-shaped valleys into the range, which end abruptly on the east at the steep coast in deep bays or in outwash flats. On the west the glaciers have cut deeply enough to create lakes, dammed by terminal moraines at their downstream ends.[5] Lake Clark, the largest, is the sixth largest lake in Alaska, 860 feet (260 m) deep and 42 miles (68 km) long.[11]

The park includes a variety of unrelated rocks. The core of the Chigmit Mountains is a granite pluton forced upwards[12] by the collision of the Pacific plate and the North American plate. Rocks in coastal areas are sedimentary in origin, and contain abundant fossils.[13] Volcanic rocks intrude through these native rocks.

Volcanoes

Redoubt volcano in eruption

Redoubt is the park's active volcano. 10,197 feet (3,108 m) high, about 10 kilometres (6.2 mi) in diameter and with a volume of about 30 to 35 cubic kilometers, the stratovolcano rises through the Chigmit batholith. It has a 1.8-kilometre (1.1 mi) wide summit crater. The Drift Glacier originates there and flows through a gap in the rim.[14] Redoubt's most recent active phase began on December 14, 1989, with ash eruptions. The ash clouds affected air traffic, causing all four engines to fail on KLM Flight 867 when it passed overhead at 25,000 feet (7,600 m). The 747 was able to safely return to Anchorage. Four other airplanes were damaged in the same event, which brought greater awareness of the hazards associated with high-altitude volcanic ash.[15][16][17] Redoubt was quiet after 1990 until March and April 2009 when it erupted with pyroclastic flows that melted ice, creating lahars on the Drift River,[15] endangering the Drift River Terminal Facility to the east of the park.

Iliamna volcano

Iliamna has not been recently active. Like Redoubt, it stands on Jurassic granite basement rock, but has been significantly altered by glacial activity that has cut away the slopes on the southern and eastern sides.[18] The mountain has experienced seismic activity from time to time that has raised alert levels while the earthquake flurries have persisted. The peak has active fumaroles that occasionally produce visible vapor plumes.[19]

Activities

The park and preserve offer a variety of possible activities, including kayaking, rafting, hiking and camping.[20] Most of the large Alaskan animals are present and viewable in the park.[21] Fishing is allowed in both the park and preserve,[22] while sport hunting is permitted in the preserve.[23]

Ecology

Sockeye salmon in the Kijik River

Lake Clark preserves a wide variety of Alaskan landscapes and ecosystems, corresponding to its four main physiographic areas. The coastal sections running along the Cook Inlet from Tuxedni Bay to Chinitna Bay include coastline and marine ecosystems. The mountains of the Alaska, Aleutian and Chigmit Ranges with their glaciers form a second region. On either side of the mountains the valley, lake and foothill areas present a glacially altered landscape.[24] Boreal forest dominates the lower sections of the southwest part of the park, with white and black spruce making up most of the coniferous trees. White spruce have been affected by spruce bark beetle infestation, and spruce needle rust outbreaks have been so heavy that the surface of Lake Clark has been colored orange by spores.[25] Farther north and west lie the tundra regions,[5] primarily the result of elevation. The tundra supports caribou and ptarmigans.[26]

Salt marshes along the Cook Inlet represent one of the most productive ecosystems in the park. They account for under 1% of the park's area, but provide a source of food in early summer for both brown and black bears.[27] Lake Clark's coastal areas are rated as some of the top bear viewing destinations in the world, along with the coast of Katmai National Park. Most bears are concentrated at Chinitna Bay or Silver Salmon Creek when the fish are running. Chinitna Bay is considered by some to be one of the top bear viewing destinations in Alaska.[28][11] Tuxedni Bay, north of Chinitna Bay, also provides excellent bear viewing; up to 20 brown bears have been spotted feeding on clams and sedges at a time. Fewer people visit the bay and therefore it is easier to view bears in peace.[29] Inland areas of the park also provide bear viewing. Crescent Lake provides excellent bear viewing in June, July and August. Both grizzly and black bears are present, but grizzly bears are more common and seen more often, since black bears are shier and are easily displaced by their larger cousins.[30] On the other side of the park, the Kvichak River is the world's most productive watershed for sockeye salmon, whose offspring account for 33% of the species' catch in the United States and 16% of world production. Salmon are so plentiful that a wolf pack at Lake Clark has been documented as the only salmon-dependent pack in the world.[11]

Major terrestrial mammals in the park include brown bears, moose, caribou, Dall's sheep and gray wolves. Smaller mammals include martens, red fox, wolverines, river otters, beaver and lynx. Marine mammals include sea lions, beluga whales harbor seals and porpoises.[31] Both black and brown bears are present in the park. Black bears use all areas of the park and preserve, except the higher elevations. Brown bears are most numerous along the coast. A recent survey found that about 219 bears graze in salt marshes during the summer in the coastal areas of the park.[32] Caribou have recently declined in population size from 200,000 to 30,000 due to an unknown cause.[33]

Weather in the park is extremely variable. Marine air from the Pacific Ocean meets drier air of the continental airmass over the park. The average summer temperature is between 50 and 65 °F (10 and 18 °C) with highs around 68 °F (20 °C) and typical winter lows of 1 °F (−17 °C). Snow can happen at any time.[34]

History

Lake Clark

The earliest human presence known in the area of Lake Clark was at Bristol Bay. People of the Paleo-Arctic Tradition lived there between 10,000 years before the present and 7500 BP. These people were followed by the northern Archaic tradition between 6,000 BP and 4,000 BP. Two sites from this tradition have been documented in the park. The Arctic small tool tradition followed from about 5,000 BP to 3,000 BP. The Norton tradition came between 2,200 BP and 1,000 BP, concentrated around Bristol Bay. The Thule Tradition was established around 2,000 BP and lasted until historic times. The northern Athabaskan Dena'ina presently live in the area. Kijik village is the primary archaeological site in the park, inhabited by Dena'ina until the early 20th century.[5] Settlements have also been documented around Chinitna Bay.[35]

The Cook Inlet was surveyed by British Captain James Cook in 1778. In succeeding decades Russian traders established themselves in the region. The major settlement during the 19th century was at Kijik, with a population in the low hundreds. By the 1890s American traders had arrived in the area, meeting a native population that had been greatly reduced by imported diseases.[5] Kijik has been designated a National Historic Landmark district.[36]

In 1930 the first floatplane landed on Lake Clark. In 1942 the first air taxi service was provided to Lake Clark, run by Leon "Babe" Alsworth, Sr. to Port Alsworth.[37] Apart from Port Alsworth, there are five other communities within the park: Lime Village, Nondalton, Iliamna, Newhalen and Pedro Bay. Most local residents are Dena'ina.[38]

During the 20th century the future park area was lightly populated by people with a high tolerance for solitude. One such person was Richard Proenneke, a former Iowan who came to Alaska in 1949. Proenneke lived at Twin Lakes from 1968 to 1999 in a cabin he built himself, feeding himself through subsistence hunting and by salvaging meat from animals left by sport hunters. In 1973 a friend published the book One Man's Wilderness: An Alaskan Odyssey based on his journals. Some of the movie footage shot by Proenneke of his life at the lake was compiled into the documentary, Alone in the Wilderness. Produced posthumously, it has become popular on public television in the United States.[39][40] Proenneke's cabin is now owned by the park service and listed on the National Register of Historic Places.[41]

Lake Clark was proclaimed a national monument on December 1, 1978, by President Jimmy Carter, using his authority under the Antiquities Act. In 1980, Congress passed the Alaska National Interest Lands Conservation Act (ANILCA), which established the unit as a national park and preserve.[5]

A large open-pit mine was proposed in 2007 near the western boundary of the park. The Pebble Mine is proposed to mine molybdenum, gold and copper from an open pit about 2 miles (3.2 km) across and thousands of feet deep. Another ore body is proposed to be exploited using underground mining. Tailings from the mine are to be stored behind dams on the site, and roads and a deepwater port will be required.[42] Concerns about the mine's relationship to the park center on dust contamination and on the mine's possible effect on the sockeye salmon population.[43]

The 2,619,550-acre (1,060,090 ha) Lake Clark Wilderness covers much of the park's area, excluding preserve lands and the Cook Inlet coast. The area includes three Wild and Scenic Rivers: the Chilikadrotna River, the Mulchatna River and the Tlikakila River.[44]

See also

References

  1. ^ "Listing of acreage – December 31, 2011" (XLSX). Land Resource Division, National Park Service. Retrieved 2012-03-07. (National Park Service Acreage Reports)
  2. ^ "NPS Annual Recreation Visits Report". National Park Service. Retrieved 2012-02-28.
  3. ^ "Silver Salmon Creek". Lake Clark National Park and Preserve. National Park Service. Retrieved December 7, 2013.
  4. ^ "Lake Clark National Park map" (PDF). National Park Service. Retrieved 28 February 2013.
  5. ^ a b c d e f "Lake Clark National Park and Preserve". National Park Service. Retrieved 28 February 2013.
  6. ^ "Directions". Lake Clark National Park and Preserve. National Park Service. Retrieved 28 February 2013.
  7. ^ "Mountains". National Park Service. National Park Service. Retrieved 1 March 2013.
  8. ^ "Operating Hours & Seasons". Lake Clark National Park and Preserve. National Park Service. Retrieved 2 March 2013.
  9. ^ "Things To Do". Lake Clark National Park and Preserve. National Park Service. Retrieved 2 March 2013.
  10. ^ "Lodging". Lake Clark National Park and Preserve. National Park Service. Retrieved 2 March 2013.
  11. ^ a b c "Fresh Water Systems". Lake Clark National Park and Preserve. National Park Service. Retrieved 1 March 2013.
  12. ^ "Glaciers". Lake Clark National Park and Preserve. National Park Service. Retrieved 1 March 2013.
  13. ^ "Fossils". Lake Clark National Park and Preserve. National Park Service.
  14. ^ "Redoubt Volcano description and information". Alaska Volcano Observatory. Retrieved 1 March 2013.
  15. ^ a b "Volcanoes". Lake Clark National Park and Preserve. National Park Service. Retrieved 1 March 2013.
  16. ^ Campbell, Larry (April 18, 2010). "A look back at Alaska volcano's near-downing of a 747". Everett Daily herald. Retrieved 1 March 2013.
  17. ^ "About Alaska's Volcanoes". Alaska Volcano Observatory. Retrieved 1 March 2013.
  18. ^ "Iliamna Volcano description and information". Alaska Volcano Observatory. Retrieved 1 March 2013.
  19. ^ "Iliamna reported activity". Alaska Volcano Observatory. Retrieved 1 March 2013.
  20. ^ "Outdoor Activities". Lake Clark National Park and Preserve. National Park Service. Retrieved 28 February 2013.
  21. ^ "Wildlife Viewing". Lake Clark National Park and Preserve. National Park Service. Retrieved 28 February 2013.
  22. ^ "Fishing". Lake Clark National Park and Preserve. National Park Service. Retrieved 28 February 2013.
  23. ^ "Hunting". Lake Clark National Park and Preserve. National Park Service. Retrieved 28 February 2013.
  24. ^ "Natural Features and Ecosystems". Lake Clark National Park and Preserve. National Park Service. Retrieved 28 February 2013.
  25. ^ "Forests". Lake Clark National Park and Preserve. National Park Service. Retrieved 1 March 2013.
  26. ^ "Tundra". Lake Clark National Park and Preserve. National Park Service. Retrieved 1 March 2013.
  27. ^ "Coastal Salt Marshes". Lake Clark National Park and Preserve. National Park Service. Retrieved 1 March 2013.
  28. ^ "Chinitna Bay". Lake Clark National Park and Preserve. National Park Service. Retrieved 2 March 2013.
  29. ^ "Tuxedni Bay: Grizzy Viewing With Little Traffic". Alaska.org. Retrieved February 6, 2015.
  30. ^ "Crescent Lake". Lake Clark National Park and Preserve. National Park Service. Retrieved February 6, 2015.
  31. ^ "Wildlife Viewing". Lake Clark National Park and Preserve. National Park Service. Retrieved 2 March 2013.
  32. ^ "Bears". Lake Clark National Park and Preserve. National Park Service. Retrieved December 9, 2013.
  33. ^ "Caribou". Lake Clark National Park and Preserve. National Park Service. Retrieved December 9, 2013.
  34. ^ "Weather". Lake Clark National Park and Preserve. National Park Service. Retrieved 2 March 2013.
  35. ^ "Chinitna Bay Prehistory". Lake Clark National Park and Preserve. National Park Service. Retrieved 2 March 2013.
  36. ^ "Kijik". Lake Clark National Park and Preserve. National Park Service. Retrieved 2 March 2013.
  37. ^ "The Age of Air Travel". Lake Clark National Park and Preserve. National Park Service. Retrieved 2 March 2013.
  38. ^ "Who lives in the Lake Clark area today?". Lake Clark National Park and Preserve. National Park Service.
  39. ^ "Alone in the Wilderness". Bob Swerer Productions. Retrieved 2 March 2013.
  40. ^ "Richard L. Proenneke, Wilderness Steward". Lake Clark National Park and Preserve. National Park Service. Retrieved 2 March 2013.
  41. ^ "Proenneke's Cabin". Lake Clark National Park and Preserve. National Park Service. Retrieved 2 March 2013.
  42. ^ "Plan". Pebble Partnership. Retrieved 2 March 2013.
  43. ^ "Concerns Regarding Large-scale Mining on the Western Boundary of the Park" (PDF). Lake Clark National Park and Preserve. National Park Service. Retrieved 2 March 2013.
  44. ^ "Lake Clark Wilderness". wilderness.net. Retrieved 2 March 2013.

Bibliography

External links