Jump to content

Cape Krusenstern National Monument: Difference between revisions

Coordinates: 67°20′N 163°35′W / 67.333°N 163.583°W / 67.333; -163.583
From Wikipedia, the free encyclopedia
Content deleted Content added
m refine category structure
(42 intermediate revisions by 30 users not shown)
Line 1: Line 1:
{{Short description|U.S. National Monument and National Historic Landmark}}
{{other uses|Krusenstern (disambiguation)}}
{{other uses|Krusenstern (disambiguation)}}
{{Use mdy dates|date=August 2023}}
{{Infobox protected area
{{Infobox protected area
| name = Cape Krusenstern National Monument
| name = Cape Krusenstern National Monument
| photo = CapeKrusensternNM.jpg|thumb|Cape Krusenstern
| photo = Tundra River (20258476344).jpg
| photo_width = 280
| photo_width = 280
| iucn_category = VI
| iucn_category = V
| map = USA Alaska |relief=1
| map = USA Alaska |relief=1
| map_caption =
| map_caption =
| location = [[Northwest Arctic Borough, Alaska]], United States
| location = [[Northwest Arctic Borough, Alaska]], United States
| nearest_city = [[Kotzebue, Alaska]]
| nearest_city = [[Kotzebue, Alaska]]
| coordinates = {{coord|67|20|N|163|35|W|region:US-AK|display=inline, title}}
| lat_d = 67 | lat_m = 20 | lat_s = 0 | lat_NS = N
| area_acre = 649,082
| long_d = 163 | long_m = 35 | long_s = 0 | long_EW = W
| area_ref = <ref name="area">{{NPS area |year=2011 |accessdate=2012-03-23}}</ref>
| region = US-AK
| coords_ref =
| area = {{convert|649082|acre}}<ref name="area">{{NPS area |year=2011 |accessdate=2012-03-23}}</ref>
| created = {{start date|1980|December|2}}
| created = {{start date|1980|December|2}}
| visitation_num = 24,950
| visitation_num = 15,087
| visitation_year = 2012
| visitation_year = 2018
| visitation_ref = <ref name="visits">{{NPS visitation |accessdate=2013-02-21}}</ref>
| visitation_ref = <ref name="visits">{{NPS visitation |accessdate=2019-10-26}}</ref>
| governing_body = [[National Park Service]]
| governing_body = [[National Park Service]]
| website = [http://www.nps.gov/cakr/ Cape Krusenstern National Monument]
| website = [http://www.nps.gov/cakr/ Cape Krusenstern National Monument]
| embedded1 = {{designation list | embed = yes
|embedded1 = {{Infobox NRHP
| embed = yes
| designation1 = nhl
| name = Cape Krusenstern Archeological District National Monument
| designation1_offname = Cape Krusenstern Archeological District<ref name="nhlsum">{{cite web|url=http://tps.cr.nps.gov/nhl/detail.cfm?ResourceId=1321&ResourceType=Site|title=Cape Krusenstern Archeological District|accessdate=February 21, 2013}}</ref>
| nrhp_type = nhl
| designation1_date = November 7, 1973<ref name="nris">{{NRISref|2009a}}</ref>
| image =
| designation1_number = 73000378
| caption =
}}
| location = {{Address Restricted}}
| nearest_city = [[Kotzebue, Alaska]]
| coordinates = <!-- address restricted -->
| locmapin =
| architect OR builder =
| architecture =
| added = November 7, 1973
| area =
| refnum = 73000378<ref name="nris">{{NRISref|version=2010a}}</ref>
| designated_nrhp_type = November 7, 1973<ref name="nhlsum">{{cite web|url=http://tps.cr.nps.gov/nhl/detail.cfm?ResourceId=1321&ResourceType=Site |title=Cape Krusenstern Archeological District |access-date=February 21, 2013 |url-status=dead |archive-url=https://web.archive.org/web/20121007141605/http://tps.cr.nps.gov/nhl/detail.cfm?ResourceId=1321&ResourceType=Site |archive-date=October 7, 2012 }}</ref>
| designated_other1 = Alaska Heritage Resources Survey
| designated_other1_name = Alaska Heritage Resources Survey
| designated_other1_color = #A8EDEF
| designated_other1_abbr = AHRS
| designated_other1_number = NOA-042
| designated_other1_num_position = bottom
}}
}}
}}


'''Cape Krusenstern National Monument''' and the colocated '''Cape Krusenstern Archeological District''' is a [[U.S. National Monument]] and a [[National Historic Landmark]]<ref>[http://www.nps.gov/akso/CR/AKRCultural/CulturalMain/2ndLevel/NHL/NHLCapeKrusenstern.htm NHL Documentation]</ref> centered on [[Cape Krusenstern]] in northwestern [[Alaska]]. The national monument is one of fifteen new [[National Park Service]] units designated by the [[Alaska National Interest Lands Conservation Act]] (ANILCA) of 1980. It was initially declared a [[National Monument (United States)|national monument]] under the authority of the [[Antiquities Act]] by President [[Jimmy Carter]] on December 1, 1978.
'''Cape Krusenstern National Monument''' and the colocated '''Cape Krusenstern Archeological District''' is a [[U.S. National Monument]] and a [[National Historic Landmark]]<ref>[http://www.nps.gov/akso/CR/AKRCultural/CulturalMain/2ndLevel/NHL/NHLCapeKrusenstern.htm NHL Documentation]</ref> centered on [[Cape Krusenstern]] in northwestern [[Alaska]]. The national monument was one of fifteen new [[National Park Service]] units designated by the [[Alaska National Interest Lands Conservation Act]] (ANILCA) of 1980. It was initially declared a [[National monument (United States)|national monument]] under the authority of the [[Antiquities Act]] by President [[Jimmy Carter]] on December 1, 1978.


Cape Krusenstern is primarily a coastal plain, containing large [[lagoons]] and rolling hills of [[limestone]]. The bluffs record thousands of years of change in the shorelines of the [[Chukchi Sea]], as well as evidence of some 9,000 years of human habitation. The park's central features, 114 beach ridges at the eponymous cape, alternate between sandy and gravelly ridges and narrow ponds. Located entirely above the [[Arctic Circle]] in a region of [[permafrost]], the monument's lands include typical [[thermokarst]] features.
Cape Krusenstern is primarily a coastal plain, containing large [[lagoons]] and rolling hills of [[limestone]]. The bluffs record thousands of years of change in the shorelines of the [[Chukchi Sea]], as well as evidence of some 9,000 years of human habitation. The park's central features, 114 beach ridges at the eponymous cape, alternate between sandy and gravelly ridges and narrow ponds. Located entirely above the [[Arctic Circle]] in a region of [[permafrost]], the monument's lands include typical [[thermokarst]] features.


==Description==
==Description==
Cape Krusenstern National Monument comprises the coast of the [[Chukchi Sea]] from the opening of the [[Hotham Inlet]] at the mouth of the Kobuk River, extending northwards along the coast to a point just short of Imikruk Lagoon. It extends inland toward the Kobuk Valley about {{convert|20|mi|km}}, with a high point in the north at [[Kikmiksot Mountain]] ({{convert|2285|ft|m}}) in the [[Mulgrave Hills]] and in the south at [[Mount Noak]] ({{convert|2010|ft|m}}) in the [[Igichuk Hills]]. The coastline is marked by a series of lagoons separated from the sea by sandspits. The largest is the Krusenstern Lagoon at [[Cape Krusenstern]].Others include the [[Kotlik Lagoon]], [[Imik Lagoon]] and [[Aukulak Lagoon]].<ref name=npscakrmap1>{{cite map|title=Map of Cape Krusenstern National Monument|publisher=National Park Service}}</ref>
Cape Krusenstern National Monument comprises the coast of the [[Chukchi Sea]] from the opening of the [[Hotham Inlet]] at the mouth of the Kobuk River, extending northwards along the coast to a point just short of Imikruk Lagoon. It extends inland about {{convert|20|mi|km}}, with a high point in the north at Kikmiksot Mountain ({{convert|2285|ft|m}}) in the Mulgrave Hills and in the south at Mount Noak ({{convert|2010|ft|m}}) in the Igichuk Hills. The coastline is marked by a series of lagoons separated from the sea by sandspits. The largest is the Krusenstern Lagoon at [[Cape Krusenstern]]. Others include the Kotlik, Imik and Aukulak Lagoons.<ref name=npscakrmap1>{{cite map|title=Map of Cape Krusenstern National Monument|publisher=National Park Service}}</ref>


The local bedrock is composed of limestone, dolomite, phyllite and chert from the Precambrian through Devonian times. The land was glaciated during the [[Illinoian glaciation]], but was free of permanent ice during the [[Wisconsonian glaciation]]. [[Longshore current]]s have deposited beach ridges since the for 6,000 years.<ref name=npsakso1>{{cite web|title=Cape Krusenstern National Monument|url=http://www.nps.gov/akso/akarc/cr_cakr.htm|work=Prehistory of Alaska|publisher=National Park Service|accessdate=21 February 2013}}</ref>
The local bedrock is composed of limestone, dolomite, phyllite and chert from the Precambrian through Devonian times. The land was glaciated during the [[Illinoian glaciation]], but was free of permanent ice during the [[Wisconsonian glaciation]]. [[Longshore current]]s have deposited beach ridges since then for 6,000 years.<ref name=npsakso1>{{cite web|title=Cape Krusenstern National Monument|url=http://www.nps.gov/akso/akarc/cr_cakr.htm|work=Prehistory of Alaska|publisher=National Park Service|access-date=21 February 2013}}</ref>


===Archaeological district===
===Archaeological district===
The archeological district comprises 114 ancient beach ridges which formed approximately 60 years apart. They provide a sequential look at over 5000 years of habitation.<ref name="nhlsum"/> The area in the [[National Historic Landmark District]] is vast, making this one of the largest NHLs in the U.S., along with the [[Adirondack Park]].<ref name="expansion">{{cite web|url=http://www.montanastandard.com/articles/2006/04/27/newsbutte/hjjdjfhcjiibef.txt|title=Interior secretary approves district expansion |author=Roberta Forsell Stauffer |date=2007-04-27|accessdate=2007-11-01|work=Newspaper article on expansion of National Historic Landmark Butte-Anaconda Historic District|publisher=The Montana Standard (newspaper)}}</ref> The national historic landmark district was designated on November 7, 1973.<ref name="nhlsum"/>
The archeological district comprises 114 ancient beach ridges which formed approximately 60 years apart. They provide a sequential look at over 5000 years of habitation.<ref name="nhlsum"/> The area in the [[National Historic Landmark]] is vast, making this one of the largest NHLs in the U.S., along with the [[Adirondack Park]].<ref name="expansion">{{cite web|url=http://www.montanastandard.com/articles/2006/04/27/newsbutte/hjjdjfhcjiibef.txt|title=Interior secretary approves district expansion |author=Roberta Forsell Stauffer |date=2007-04-27|access-date=2007-11-01|work=Newspaper article on expansion of National Historic Landmark Butte-Anaconda Historic District|publisher=The Montana Standard (newspaper)}}</ref> The national historic landmark was designated on November 7, 1973.<ref name="nhlsum"/>


The beach ridges are the primary reason for the area's preservation, which serves to safeguard evidence of 5,000 years of occupation by the [[Inupiat people]],<ref name=npscakr9>{{cite web|title=History & Culture|url=http://www.nps.gov/cakr/historyculture/index.htm|work=Cape Krusenstern National Monument|publisher=National Park Service|accessdate=21 February 2013}}</ref> and more than 9,000 years of human occupation.<ref name=npscakr10>{{cite web|title=The Beach Ridges of the Cape|url=http://www.nps.gov/cakr/details.htm|work=Cape Krusenstern National Monument|publisher=National Park Service|accessdate=21 February 2013}}</ref> Initial investigations by archaeologist J. Louis Giddings in the late 1940s found campsites on the cape as much as 4,000 years old, and even older sites on the mainland.<ref name=npsakso1/> [[University of Washington]] researchers have undertaken several years of excavations to document about one third of the {{convert|9000|acre|ha|adj=on}} beach complex. Researchers found campsites, hearths and animal bones, with a few stone tools and pieces of pottery. In newer locations the team documented the remains of semi-subterranean houses built into the beach ridges.<ref name=npscakr11>{{cite web|title=Places|url=http://www.nps.gov/cakr/historyculture/places.htm|work=Cape Krusenstern National Monument|publisher=National Park Service|accessdate=21 February 2013}}</ref>
The beach ridges are the primary reason for the area's preservation, which serves to safeguard evidence of 5,000 years of occupation by the [[Inupiat people]],<ref name=npscakr9>{{cite web|title=History & Culture|url=http://www.nps.gov/cakr/historyculture/index.htm|work=Cape Krusenstern National Monument|publisher=National Park Service|access-date=21 February 2013}}</ref> and more than 9,000 years of human occupation.<ref name=npscakr10>{{cite web|title=The Beach Ridges of the Cape|url=http://www.nps.gov/cakr/details.htm|work=Cape Krusenstern National Monument|publisher=National Park Service|access-date=21 February 2013}}</ref> Initial investigations by archaeologist J. Louis Giddings in the late 1940s found campsites on the cape as much as 4,000 years old, and even older sites on the mainland.<ref name=npsakso1/> [[University of Washington]] researchers have undertaken several years of excavations to document about one third of the {{convert|9000|acre|ha|adj=on}} beach complex. Researchers found campsites, hearths and animal bones, with a few stone tools and pieces of pottery. In newer locations the team documented the remains of semi-subterranean houses built into the beach ridges, such as the [[Old Whaling site]].<ref name=npscakr11>{{cite web|title=Places|url=http://www.nps.gov/cakr/historyculture/places.htm|work=Cape Krusenstern National Monument|publisher=National Park Service|access-date=21 February 2013}}</ref><ref>{{Cite book |last=Giddings |first=J. Louis |url=http://worldcat.org/oclc/11519048 |title=Beach ridge archeology of Cape Krusenstern : Eskimo and pre-Eskimo settlements around Kotzebue Sound, Alaska |date=1986 |publisher=National Park Service, U.S. Dept. of the Interior |oclc=11519048}}</ref>


The oldest mainland sites such as Battle Rock, Rabbit Mountain and the Lower Bench date to the [[Paleo-Arctic Tradition]], about 10,000 to 7,000 years before present. Similar materials have been recovered in the Trail Creek caves of Bering Land Bridge National Preserve on the [[Seward Peninsula]]. The Palisades site has yielded materials from the Northern [[Archaic period in North America|Archaic period]] dating to about 6,000 years before the present. Later periods described in the region include the [[Arctic Small Tool tradition]] and the Northern Maritime tradition. The western [[Thule people|Thule culture]], which used dogs and seal oil extended from 950 AD to 1400, and was succeeded by the Kotzebue culture from about 1400 to about 1850, when Europeans began to have an impact on native cultures. Kotzebue sites are widespread within the monument.<ref name=npsakso1/>
The oldest mainland sites such as Battle Rock, Rabbit Mountain and the Lower Bench date to the [[Paleo-Arctic tradition]], about 10,000 to 7,000 years before present. Similar materials have been recovered in the Trail Creek caves of Bering Land Bridge National Preserve on the [[Seward Peninsula]]. The Palisades site has yielded materials from the Northern [[Archaic period in North America|Archaic period]] dating to about 6,000 years before the present. Later periods described in the region include the [[Arctic Small Tool tradition]] and the Northern Maritime tradition. The western [[Thule people|Thule culture]], which used dogs and seal oil extended from 950 AD to 1400, and was succeeded by the Kotzebue culture from about 1400 to about 1850, when Europeans began to affect native cultures. Kotzebue sites are widespread within the monument.<ref name=npsakso1/>


===Later history===
===Later history===
[[File:Eskimo family on spring ice of Krusenstern Lagoon on an egg hunting trip (33509512556).jpg|thumb|Family on spring ice of Krusenstern Lagoon on an egg hunting trip, 1973]]
Europeans visited the Cape Krusenstern region to pursue whales beginning in the 1850s. During the [[American Civil War]] the Confederate raider ''[[CSS Shenandoah]]'' captured whalers in the area.<ref name=npsakso1/>
Europeans visited the Cape Krusenstern region to pursue whales beginning in the 1850s. During the [[American Civil War]] the Confederate raider ''[[CSS Shenandoah]]'' captured whalers in the area.<ref name=npsakso1/>


In early modern times the Kotzebue area was the site of an Iqatngut," a kind of trade fair for the region's native people. The Iqatngut tradition died out with the foundation of [[Nome, Alaska|Nome]] as the region's principal town in the early 20th century. A short-lived [[gold rush]] brought prospectors to the Seward Peninsula and Kotzebue in the 1890s. A few 20th century structures exist in the monument, including an [[Alaska Road Commission]] cabin at [[Anigaaq, Alaska|Anigaaq]] that has been evaluated for historic significance.<ref name=npsakso1/> In the 1950s the area's lack of good natural harbors, a desire to develop the Alaskan frontier facing the Soviet Union and the [[Operation Plowshare]] drive for the peaceful use of nuclear weapons brought proposals for [[Operation Chariot (1958)|Operation Chariot]], a proposed deepwater harbor at [[Cape Thompson]] {{convert|50|mi|km}} northwest of the monument, to be excavated using [[nuclear explosion|nuclear devices]]. The project, though popular elsewhere in Alaska, was opposed by native leaders and was discarded.<ref name=npsakso1/>
In early modern times the Kotzebue area was the site of Qatnut, a kind of trade fair for the region's native people. Qatnut is still celebrated in modern times in the city of [[Kotzebue, Alaska]] every other summer. A short-lived [[gold rush]] brought prospectors to the Seward Peninsula and Kotzebue in the 1890s. A few 20th century structures exist in the monument, including an [[Alaska Road Commission]] cabin at [[Anigaaq, Alaska|Anigaaq]] that has been evaluated for historic significance.<ref name=npsakso1/> In the 1950s the area's lack of good natural harbors, a desire to develop the Alaskan frontier facing the Soviet Union and the [[Operation Plowshare]] drive for the peaceful use of nuclear weapons brought proposals for [[Operation Chariot (1958)|Operation Chariot]], a proposed deepwater harbor at [[Cape Thompson]] {{convert|50|mi|km}} northwest of the monument, to be excavated using [[nuclear explosion|nuclear devices]]. The project, though popular elsewhere in Alaska, was opposed by native leaders and was discarded.<ref name=npsakso1/>


==Ecology and environment==
==Ecology and environment==
[[File:Muskox and Geese.jpg|thumb|Muskox at Cape Krusenstern]]
[[File:Muskox and Greater White-fronted Geese on vegetated beach ridges in front of the Igichuk Hills. (92e7aa72-1dd8-b71c-07d9-7fb3eabf6e60).jpg|thumb|Muskoxen at Cape Krusenstern]]
The lands within the monument, which lies entirely above the [[Arctic Circle]], are all [[tundra]] in which the [[permafrost]] dominates soils and vegetation.<ref name=npscakr5>{{cite web|title=Nature and Science|url=http://www.nps.gov/cakr/naturescience/index.htm|work=Cape Krusenstern National Monument|publisher=National Park Service|accessdate=21 February 2013}}</ref> The monument is in a [[permafrost]] region. In the lowland areas the land is shaped by [[thermokarst]] forces. Typical thermokarst features seen in the monument include [[pingo]]s, polygon [[ice wedge]]s and thaw ponds.<ref name=npsakso1/> Low vegetation covers the land, mainly in tussocks of [[cottongrass]], with shrubby growth of willow, [[Labrador tea]], dwarf birch, [[Alnus incana|mountain alder]] and other species in moist tundra areas. Wetter aras in the southern part of the monument feature grasses and sedges. Upland regions are Arctic tundra, with lichen, [[saxifrage]], willow and heather. Few trees grow, and the [[white spruce]] that do grow are confined to the southeastern corner of the monument.<ref name=npsakso1/>
The lands within the monument, which lies entirely above the [[Arctic Circle]], are all [[tundra]] in which the [[permafrost]] dominates soils and vegetation.<ref name=npscakr5>{{cite web|title=Nature and Science|url=http://www.nps.gov/cakr/naturescience/index.htm|work=Cape Krusenstern National Monument|publisher=National Park Service|access-date=21 February 2013}}</ref> The monument is in a [[permafrost]] region. In the lowland areas the land is shaped by [[thermokarst]] forces. Typical thermokarst features seen in the monument include [[pingo]]s, polygon [[ice wedge]]s and thaw ponds.<ref name=npsakso1/> Low vegetation covers the land, mainly in tussocks of [[cottongrass]], with shrubby growth of willow, [[Labrador tea]], dwarf birch, [[Alnus incana|mountain alder]] and other species in moist tundra areas. Wetter areas in the southern part of the monument feature grasses and sedges. Upland regions are Arctic tundra, with lichen, [[saxifrage]], willow and heather. Few trees grow, and the [[white spruce]] that do grow are confined to the southeastern corner of the monument.<ref name=npsakso1/>


The coastal region supports a variety of large terrestrial and marine mammals. The abundant [[caribou]] are part of the West. Large predators include [[brown bear]]s and [[gray wolf|gray wolves]].<ref name=npscakr5/> Smaller mammals include [[snowshoe hare|snowshoe]] and [[Arctic hare|Arctic]] hares, weasels, mink, otters, porcupines and a few [[wolverine]]s. Marine mammals in or near monument waters include [[fin whale|fin]], [[bowhead whale|bowhead]], [[gray whale|gray]] and [[beluga whale|beluga]] whales. Seal species include [[ringed seal|ringed]], [[spotted seal|spotted]], [[bearded seal|bearded]] and [[ribbon seal|ribbon]] seals, with occasional [[walrus]]es. Ringed seals are hunted by native subsistence hunters, and occasionally beluga whales and walrus are hunted as well.<ref name=npsakso1/>
The coastal region supports a variety of large terrestrial and marine mammals. The abundant [[Porcupine caribou|caribou]] are part of the West. Large predators include [[brown bear]]s and [[northwestern wolf|wolf]] packs.<ref name=npscakr5/> Smaller mammals include [[snowshoe hare|snowshoe]] and [[Arctic hare|Arctic]] hares, [[weasel]]s, [[American mink|mink]]s, otters, [[North American porcupine|porcupine]]s and a few [[wolverine]]s. Marine mammals in or near monument waters include [[fin whale|fin]], [[bowhead whale|bowhead]], [[gray whale|gray]] and [[beluga whale|beluga]] whales. Seal species include [[ringed seal|ringed]], [[spotted seal|spotted]], [[bearded seal|bearded]] and [[ribbon seal|ribbon]] seals, with occasional [[walrus]]es. Ringed seals are hunted by native subsistence hunters, and occasionally beluga whales and walrus are hunted as well.<ref name=npsakso1/>


Fish species include five species of salmon, [[burbot]], several species of [[whitefish (fisheries term)|whitefish]], [[Arctic char]], [[Dolly Varden trout]], herring and [[northern pike]].<ref name=npsakso1/>
Fish species include five species of salmon, [[burbot]], several species of [[whitefish (fisheries term)|whitefish]], [[Arctic char]], [[Dolly Varden trout]], herring and [[northern pike]].<ref name=npsakso1/>


Water birds of all kinds nest in the monument. Nesting species include [[tundra swan]], [[mallard]], [[green-winged teal]], [[common eider]], [[Canada goose]], and [[horned grebe|horned]] and [[red-necked grebe|red-necked]] grebes. [[Sandhill crane]]s also nest on the tundra, with [[common loon|common]], [[black-throated loon|Arctic]] and [[yellow-billed loon|yellow-billed]] loons. Seabirds include [[glaucous gull]]s, [[Arctic tern]]s, [[long-tailed jaeger]]s and [[common murre]]s. Landbirds include [[willow ptarmigan|willow]] and [[rock ptarmigan|rock]] ptarmigans. Predatory landbirds include [[peregrine falcon]]s, [[snowy owl]]s and [[goshawk]]s.<ref name=npsakso1/> Endangered species at Cape Krusenstern include the possibly extinct [[Eskimo curlew]], and threatened [[spectacled eider]] and [[Steller's eider]].<ref name=npscakr6>{{cite web|title=Frequently Asked Questions|url=http://www.nps.gov/cakr/faqs.htm|work=Cape Krusenstern National Monument|publisher=National Park Service|accessdate=21 February 2013}}</ref>
Water birds of all kinds nest in the monument. Nesting species include [[tundra swan]], [[mallard]], [[green-winged teal]], [[common eider]], [[Canada goose]], and [[horned grebe|horned]] and [[red-necked grebe|red-necked]] grebes. [[Sandhill crane]]s also nest on the tundra, with [[common loon|common]], [[black-throated loon|Arctic]] and [[yellow-billed loon|yellow-billed]] loons. Seabirds include [[glaucous gull]]s, [[Arctic tern]]s, [[long-tailed jaeger]]s and [[common murre]]s. Landbirds include [[willow ptarmigan|willow]] and [[rock ptarmigan|rock]] ptarmigans. Predatory landbirds include [[peregrine falcon]]s, [[snowy owl]]s and [[goshawk]]s.<ref name=npsakso1/> Endangered species at Cape Krusenstern include the possibly extinct [[Eskimo curlew]], and threatened [[spectacled eider]] and [[Steller's eider]].<ref name=npscakr6>{{cite web|title=Frequently Asked Questions|url=http://www.nps.gov/cakr/faqs.htm|work=Cape Krusenstern National Monument|publisher=National Park Service|access-date=21 February 2013}}</ref>


Weather in the coastal monument is subject to extremes. Average low temperatures in January are {{convert|5|F|C}}, and can reach nighttime lows of {{convert|-50|F|C}}. Summer temperatures average around {{convert|55|F|C}}, and can reach {{convert|70|F|C}}. Since the park is above the Arctic Circle, the sun does not set from June 3 to July 9, and the sun is visible for only 1-1/2 hour on the winter solstice, with long periods of twilight on either side of sunrise and sunset. As is the case over all of northern Alaska, the [[aurora borealis]] is often visible on winter nights when solar activity is high. Snow can happen at any time of the year. The coast can be stormy, with winds of {{convert|50|mph|kph}} to {{convert|70|mph|kph}}. Visitors must take care against [[hypothermia]] in the cool, damp environment.<ref name=npscakr8>{{cite web|title=Weather|url=http://www.nps.gov/cakr/planyourvisit/weather.htm|work=Cape Krusenstern National Monument|publisher=National Park Service|accessdate=21 February 2013}}</ref>
Weather in the coastal monument is subject to extremes. Average low temperatures in January are {{convert|5|F|C}}, and can reach nighttime lows of {{convert|-50|F|C}}. Summer temperatures average around {{convert|55|F|C}}, and can reach {{convert|70|F|C}}. Since the park is above the Arctic Circle, the sun does not set from June 3 to July 9, and the sun is visible for only {{frac|1|1|2}} hours on the winter solstice, with long periods of twilight on either side of sunrise and sunset. As is the case over all of northern Alaska, the [[aurora borealis]] is often visible on winter nights when solar activity is high. Snow can happen at any time of the year. The coast can be stormy, with winds of {{convert|50|mph|kph}} to {{convert|70|mph|kph}}. Visitors must take care against [[hypothermia]] in the cool, damp environment.<ref name=npscakr8>{{cite web|title=Weather|url=http://www.nps.gov/cakr/planyourvisit/weather.htm|work=Cape Krusenstern National Monument|publisher=National Park Service|access-date=21 February 2013}}</ref>


===Mining===
===Mining===
The [[Red Dog mine]] is the world's largest [[zinc]] mine. The mine opened in 1989, located about {{convert|30|mi|km}} northeast of the monument, close to Noatak National Preserve on land owned by the [[NANA Regional Corporation]], an Alaskan native corporation.The mine is operated by Teck Cominco Alaska. A haul road from the mine crosses monument lands to a small port facility on the monument's shore a few miles south of the northern boundary, from which the concentrated lead and zinc powder is shipped during the 100 ice-free days of the year. About {{convert|20|mi|km}} of the {{convert|55|mi|km|adj=on}} road are within the monument.<ref name=adec1>{{cite web|title=Red Dog Mine|url=http://www.dec.state.ak.us/spar/csp/sites/reddog.htm|publisher=Alaska Department of Environmental Conservation|accessdate=22 February 2013}}</ref> A 2006 study measured high lead and cadmium concentrations in voles and birds sampled near the road compared to those at a control location. The animal sample was a follow-up to an earlier study that found elevated lead and cadmium levels in mosses near the road. The contamination is attributed to dust blown from trucks on the haul road. Following the first study changes were made to the trucks to contain dust and a sampling program was put into effect to monitor dust release.<ref name=repanshek1>{{cite news|last=Repanshek|first=Kurt|title=Heavy Metals Detected in Wildlife of Cape Krusenstern National Monument|url=http://www.nationalparkstraveler.com/2009/02/heavy-metals-detected-wildlife-cape-krusenstern-national-monument|accessdate=22 February 2013|newspaper=National Parks Traveler|date=February 13, 2009}}</ref>
The [[Red Dog mine]] is the world's largest [[zinc]] mine. The mine opened in 1989, located about {{convert|30|mi|km}} northeast of the monument, close to Noatak National Preserve on land owned by the [[NANA Regional Corporation]], an Alaskan native corporation. The mine is operated by Teck Cominco Alaska. A haul road from the mine crosses monument lands to a small port facility on the monument's shore a few miles south of the northern boundary, from which the concentrated lead and zinc powder is shipped during the 100 ice-free days of the year. About {{convert|20|mi|km}} of the {{convert|55|mi|km|adj=on}} road are within the monument.<ref name=adec1>{{cite web|title=Red Dog Mine|url=http://www.dec.state.ak.us/spar/csp/sites/reddog.htm|publisher=Alaska Department of Environmental Conservation|access-date=22 February 2013|archive-url=https://web.archive.org/web/20130330141259/https://www.dec.state.ak.us/spar/csp/sites/reddog.htm|archive-date=30 March 2013|url-status=dead}}</ref> A 2006 study measured high lead and cadmium concentrations in voles and birds sampled near the road compared to those at a control location. The animal sample was a follow-up to an earlier study that found elevated lead and cadmium levels in mosses near the road. The contamination is attributed to dust blown from trucks on the haul road. Following the first study changes were made to the trucks to contain dust and a sampling program was put into effect to monitor dust release.<ref name=repanshek1>{{cite news|last=Repanshek|first=Kurt|title=Heavy Metals Detected in Wildlife of Cape Krusenstern National Monument|url=http://www.nationalparkstraveler.com/2009/02/heavy-metals-detected-wildlife-cape-krusenstern-national-monument|access-date=22 February 2013|newspaper=National Parks Traveler|date=February 13, 2009}}</ref>


==History and administration==
==History and administration==
[[File:Muskoxen with mountains and rainbow sky in the distance.jpg|thumb|Muskoxen with rainbow]]
Cape Krusenstern National Monument was established as one of fifteen new [[National Park Service]] properties established by the [[Alaska National Interest Lands Conservation Act]] (ANILCA) of 1980. It was first declared a [[national monument (United States)|national monument]] by President [[Jimmy Carter]] on December 1, 1978 using his authority under the [[Antiquities Act]] when Congressional negotiations on the proposed ANILCA bill were stalled. ANILCA was finally passed in 1980, and signed by Carter on December 2, 1980. As is the case in most national park lands in Alaska, subsistence hunting by local residents is permitted. No part of the monument is designated as a [[national preserve]], which would allow sport hunting.<ref name=npscakr2>{{cite web|title=Things to Know Before You Come|url=http://www.nps.gov/cakr/planyourvisit/things2know.htm|work=Cape Krusenstern National Monument|publisher=National Park Service|accessdate=21 February 2013}}</ref> About 19% of monument lands are owned by native corporations.<ref name=npsakso1/>
Cape Krusenstern National Monument was established as one of fifteen new [[National Park Service]] properties established by the [[Alaska National Interest Lands Conservation Act]] (ANILCA) of 1980. It was first declared a [[national monument (United States)|national monument]] by President [[Jimmy Carter]] on December 1, 1978 using his authority under the [[Antiquities Act]] when Congressional negotiations on the proposed ANILCA bill were stalled. ANILCA was finally passed in 1980, and signed by Carter on December 2, 1980. As is the case in most national park lands in Alaska, subsistence hunting by local residents is permitted. No part of the monument is designated as a [[national preserve]], which would allow sport hunting.<ref name=npscakr2>{{cite web|title=Things to Know Before You Come|url=http://www.nps.gov/cakr/planyourvisit/things2know.htm|work=Cape Krusenstern National Monument|publisher=National Park Service|access-date=21 February 2013}}</ref> About 19% of monument lands are owned by native corporations.<ref name=npsakso1/>


The monument's headquarters are at the Northwest Arctic Heritage Center in [[Kotzebue, Alaska|Kotzebue]], across the Hotham Inlet from Cape Krusenstern.<ref name=npscakr1>{{cite web|title=Operating Hours and Seasons|url=http://www.nps.gov/cakr/planyourvisit/hours.htm|work=Cape Krusenstern National Monument|publisher=National Park Service|accessdate=21 February 2013}}</ref> Offices and visitor services for [[Kobuk Valley National Park]] and [[Noatak National Preserve]] are in the same facility.<ref name=npsnoat100>{{cite web|title=Operating Hours and Seasons|url=http://www.nps.gov/noat/planyourvisit/hours.htm|work=Noatak National Preserve|publisher=National Park Service|accessdate=21 February 2013}}</ref><ref name=npskova12>{{cite web|title=Northwest Arctic Heritage Center, Kotzebue, Alaska|url=http://www.nps.gov/kova/parknews/nwahc.htm|work=Kobuk Valley National Park|publisher=National Park Service|accessdate=21 February 2013}}</ref> The units are managed together as the [[Western Arctic National Parklands]], with a single Park Service superintendent in charge.<ref name=npskova101>{{cite web|last=Quinley|first=John|title=Superintendent Named for Western Arctic National Parklands|url=http://www.nps.gov/kova/parknews/new_superintendent.htm|work=Kobuk Valley National Park|publisher=National Park Service|accessdate=21 February 2013}}</ref>
The monument's headquarters are at the Northwest Arctic Heritage Center in [[Kotzebue, Alaska|Kotzebue]], across the Hotham Inlet from Cape Krusenstern.<ref name=npscakr1>{{cite web|title=Operating Hours and Seasons|url=http://www.nps.gov/cakr/planyourvisit/hours.htm|work=Cape Krusenstern National Monument|publisher=National Park Service|access-date=21 February 2013}}</ref> Offices and visitor services for [[Kobuk Valley National Park]] and [[Noatak National Preserve]] are in the same facility.<ref name=npsnoat100>{{cite web|title=Operating Hours and Seasons|url=http://www.nps.gov/noat/planyourvisit/hours.htm|work=Noatak National Preserve|publisher=National Park Service|access-date=21 February 2013}}</ref><ref name=npskova12>{{cite web|title=Northwest Arctic Heritage Center, Kotzebue, Alaska|url=http://www.nps.gov/kova/parknews/nwahc.htm|work=Kobuk Valley National Park|publisher=National Park Service|access-date=21 February 2013}}</ref> The units are managed together as the [[Western Arctic National Parklands]], with a single Park Service superintendent in charge.<ref name=npskova101>{{cite web|last=Quinley|first=John|title=Superintendent Named for Western Arctic National Parklands|url=http://www.nps.gov/kova/parknews/new_superintendent.htm|work=Kobuk Valley National Park|publisher=National Park Service|access-date=21 February 2013}}</ref>

==See also==
*[[List of National Historic Landmarks in Alaska]]
*[[List of national monuments of the United States]]
*[[National Register of Historic Places listings in Northwest Arctic Borough, Alaska]]


==References==
==References==
Line 76: Line 100:


== External links ==
== External links ==
{{Wikivoyage}}
*[http://www.nps.gov/cakr/index.htm Cape Krusenstern National Monument] at the National Park Service
*[http://www.nps.gov/cakr/index.htm Cape Krusenstern National Monument] at the National Park Service
*[http://www.nps.gov/akso/akarc/cr_cakr.htm Cape Krusenstern National Monument] at the National Park Service Regional Office
*[http://www.nps.gov/akso/akarc/cr_cakr.htm Cape Krusenstern National Monument] at the National Park Service Regional Office


{{commons category|Cape Krusenstern National Monument}}
{{commons category|Cape Krusenstern National Monument}}

{{Registered Historic Places}}
{{Protected areas of Alaska}}
{{Protected areas of Alaska}}
{{National Monuments of the United States}}
{{NRHP in Alaska by borough and census area}}
{{National Register of Historic Places}}

{{authority control}}


{{DEFAULTSORT:Cape Krusenstern National Monument And Archeological District}}
{{DEFAULTSORT:Cape Krusenstern National Monument And Archeological District}}
Line 94: Line 124:
[[Category:Western Arctic National Parklands]]
[[Category:Western Arctic National Parklands]]
[[Category:National Register of Historic Places in Northwest Arctic Borough, Alaska]]
[[Category:National Register of Historic Places in Northwest Arctic Borough, Alaska]]
[[Category:Populated places on the National Register of Historic Places in Alaska]]

Revision as of 17:00, 13 September 2024

Cape Krusenstern National Monument
IUCN category V (protected landscape/seascape)
Map showing the location of Cape Krusenstern National Monument
Map showing the location of Cape Krusenstern National Monument
LocationNorthwest Arctic Borough, Alaska, United States
Nearest cityKotzebue, Alaska
Coordinates67°20′N 163°35′W / 67.333°N 163.583°W / 67.333; -163.583
Area649,082 acres (2,626.74 km2)[1]
CreatedDecember 2, 1980 (1980-December-02)
Visitors15,087 (in 2018)[2]
Governing bodyNational Park Service
WebsiteCape Krusenstern National Monument
Cape Krusenstern Archeological District National Monument
Alaska Heritage Resources Survey
LocationAddress restricted[4]
Nearest cityKotzebue, Alaska
NRHP reference No.73000378[3]
AHRS No.NOA-042
Significant dates
Added to NRHPNovember 7, 1973
Designated NHLNovember 7, 1973[5]

Cape Krusenstern National Monument and the colocated Cape Krusenstern Archeological District is a U.S. National Monument and a National Historic Landmark[6] centered on Cape Krusenstern in northwestern Alaska. The national monument was one of fifteen new National Park Service units designated by the Alaska National Interest Lands Conservation Act (ANILCA) of 1980. It was initially declared a national monument under the authority of the Antiquities Act by President Jimmy Carter on December 1, 1978.

Cape Krusenstern is primarily a coastal plain, containing large lagoons and rolling hills of limestone. The bluffs record thousands of years of change in the shorelines of the Chukchi Sea, as well as evidence of some 9,000 years of human habitation. The park's central features, 114 beach ridges at the eponymous cape, alternate between sandy and gravelly ridges and narrow ponds. Located entirely above the Arctic Circle in a region of permafrost, the monument's lands include typical thermokarst features.

Description

Cape Krusenstern National Monument comprises the coast of the Chukchi Sea from the opening of the Hotham Inlet at the mouth of the Kobuk River, extending northwards along the coast to a point just short of Imikruk Lagoon. It extends inland about 20 miles (32 km), with a high point in the north at Kikmiksot Mountain (2,285 feet (696 m)) in the Mulgrave Hills and in the south at Mount Noak (2,010 feet (610 m)) in the Igichuk Hills. The coastline is marked by a series of lagoons separated from the sea by sandspits. The largest is the Krusenstern Lagoon at Cape Krusenstern. Others include the Kotlik, Imik and Aukulak Lagoons.[7]

The local bedrock is composed of limestone, dolomite, phyllite and chert from the Precambrian through Devonian times. The land was glaciated during the Illinoian glaciation, but was free of permanent ice during the Wisconsonian glaciation. Longshore currents have deposited beach ridges since then for 6,000 years.[8]

Archaeological district

The archeological district comprises 114 ancient beach ridges which formed approximately 60 years apart. They provide a sequential look at over 5000 years of habitation.[5] The area in the National Historic Landmark is vast, making this one of the largest NHLs in the U.S., along with the Adirondack Park.[9] The national historic landmark was designated on November 7, 1973.[5]

The beach ridges are the primary reason for the area's preservation, which serves to safeguard evidence of 5,000 years of occupation by the Inupiat people,[10] and more than 9,000 years of human occupation.[11] Initial investigations by archaeologist J. Louis Giddings in the late 1940s found campsites on the cape as much as 4,000 years old, and even older sites on the mainland.[8] University of Washington researchers have undertaken several years of excavations to document about one third of the 9,000-acre (3,600 ha) beach complex. Researchers found campsites, hearths and animal bones, with a few stone tools and pieces of pottery. In newer locations the team documented the remains of semi-subterranean houses built into the beach ridges, such as the Old Whaling site.[12][13]

The oldest mainland sites such as Battle Rock, Rabbit Mountain and the Lower Bench date to the Paleo-Arctic tradition, about 10,000 to 7,000 years before present. Similar materials have been recovered in the Trail Creek caves of Bering Land Bridge National Preserve on the Seward Peninsula. The Palisades site has yielded materials from the Northern Archaic period dating to about 6,000 years before the present. Later periods described in the region include the Arctic Small Tool tradition and the Northern Maritime tradition. The western Thule culture, which used dogs and seal oil extended from 950 AD to 1400, and was succeeded by the Kotzebue culture from about 1400 to about 1850, when Europeans began to affect native cultures. Kotzebue sites are widespread within the monument.[8]

Later history

Family on spring ice of Krusenstern Lagoon on an egg hunting trip, 1973

Europeans visited the Cape Krusenstern region to pursue whales beginning in the 1850s. During the American Civil War the Confederate raider CSS Shenandoah captured whalers in the area.[8]

In early modern times the Kotzebue area was the site of Qatnut, a kind of trade fair for the region's native people. Qatnut is still celebrated in modern times in the city of Kotzebue, Alaska every other summer. A short-lived gold rush brought prospectors to the Seward Peninsula and Kotzebue in the 1890s. A few 20th century structures exist in the monument, including an Alaska Road Commission cabin at Anigaaq that has been evaluated for historic significance.[8] In the 1950s the area's lack of good natural harbors, a desire to develop the Alaskan frontier facing the Soviet Union and the Operation Plowshare drive for the peaceful use of nuclear weapons brought proposals for Operation Chariot, a proposed deepwater harbor at Cape Thompson 50 miles (80 km) northwest of the monument, to be excavated using nuclear devices. The project, though popular elsewhere in Alaska, was opposed by native leaders and was discarded.[8]

Ecology and environment

Muskoxen at Cape Krusenstern

The lands within the monument, which lies entirely above the Arctic Circle, are all tundra in which the permafrost dominates soils and vegetation.[14] The monument is in a permafrost region. In the lowland areas the land is shaped by thermokarst forces. Typical thermokarst features seen in the monument include pingos, polygon ice wedges and thaw ponds.[8] Low vegetation covers the land, mainly in tussocks of cottongrass, with shrubby growth of willow, Labrador tea, dwarf birch, mountain alder and other species in moist tundra areas. Wetter areas in the southern part of the monument feature grasses and sedges. Upland regions are Arctic tundra, with lichen, saxifrage, willow and heather. Few trees grow, and the white spruce that do grow are confined to the southeastern corner of the monument.[8]

The coastal region supports a variety of large terrestrial and marine mammals. The abundant caribou are part of the West. Large predators include brown bears and wolf packs.[14] Smaller mammals include snowshoe and Arctic hares, weasels, minks, otters, porcupines and a few wolverines. Marine mammals in or near monument waters include fin, bowhead, gray and beluga whales. Seal species include ringed, spotted, bearded and ribbon seals, with occasional walruses. Ringed seals are hunted by native subsistence hunters, and occasionally beluga whales and walrus are hunted as well.[8]

Fish species include five species of salmon, burbot, several species of whitefish, Arctic char, Dolly Varden trout, herring and northern pike.[8]

Water birds of all kinds nest in the monument. Nesting species include tundra swan, mallard, green-winged teal, common eider, Canada goose, and horned and red-necked grebes. Sandhill cranes also nest on the tundra, with common, Arctic and yellow-billed loons. Seabirds include glaucous gulls, Arctic terns, long-tailed jaegers and common murres. Landbirds include willow and rock ptarmigans. Predatory landbirds include peregrine falcons, snowy owls and goshawks.[8] Endangered species at Cape Krusenstern include the possibly extinct Eskimo curlew, and threatened spectacled eider and Steller's eider.[15]

Weather in the coastal monument is subject to extremes. Average low temperatures in January are 5 °F (−15 °C), and can reach nighttime lows of −50 °F (−46 °C). Summer temperatures average around 55 °F (13 °C), and can reach 70 °F (21 °C). Since the park is above the Arctic Circle, the sun does not set from June 3 to July 9, and the sun is visible for only 1+12 hours on the winter solstice, with long periods of twilight on either side of sunrise and sunset. As is the case over all of northern Alaska, the aurora borealis is often visible on winter nights when solar activity is high. Snow can happen at any time of the year. The coast can be stormy, with winds of 50 miles per hour (80 km/h) to 70 miles per hour (110 km/h). Visitors must take care against hypothermia in the cool, damp environment.[16]

Mining

The Red Dog mine is the world's largest zinc mine. The mine opened in 1989, located about 30 miles (48 km) northeast of the monument, close to Noatak National Preserve on land owned by the NANA Regional Corporation, an Alaskan native corporation. The mine is operated by Teck Cominco Alaska. A haul road from the mine crosses monument lands to a small port facility on the monument's shore a few miles south of the northern boundary, from which the concentrated lead and zinc powder is shipped during the 100 ice-free days of the year. About 20 miles (32 km) of the 55-mile (89 km) road are within the monument.[17] A 2006 study measured high lead and cadmium concentrations in voles and birds sampled near the road compared to those at a control location. The animal sample was a follow-up to an earlier study that found elevated lead and cadmium levels in mosses near the road. The contamination is attributed to dust blown from trucks on the haul road. Following the first study changes were made to the trucks to contain dust and a sampling program was put into effect to monitor dust release.[18]

History and administration

Muskoxen with rainbow

Cape Krusenstern National Monument was established as one of fifteen new National Park Service properties established by the Alaska National Interest Lands Conservation Act (ANILCA) of 1980. It was first declared a national monument by President Jimmy Carter on December 1, 1978 using his authority under the Antiquities Act when Congressional negotiations on the proposed ANILCA bill were stalled. ANILCA was finally passed in 1980, and signed by Carter on December 2, 1980. As is the case in most national park lands in Alaska, subsistence hunting by local residents is permitted. No part of the monument is designated as a national preserve, which would allow sport hunting.[19] About 19% of monument lands are owned by native corporations.[8]

The monument's headquarters are at the Northwest Arctic Heritage Center in Kotzebue, across the Hotham Inlet from Cape Krusenstern.[20] Offices and visitor services for Kobuk Valley National Park and Noatak National Preserve are in the same facility.[21][22] The units are managed together as the Western Arctic National Parklands, with a single Park Service superintendent in charge.[23]

See also

References

  1. ^ "Listing of acreage – December 31, 2011" (XLSX). Land Resource Division, National Park Service. Retrieved March 23, 2012. (National Park Service Acreage Reports)
  2. ^ "NPS Annual Recreation Visits Report". National Park Service. Retrieved October 26, 2019.
  3. ^ "National Register Information System". National Register of Historic Places. National Park Service. July 9, 2010.
  4. ^ Federal and state laws and practices restrict general public access to information regarding the specific location of this resource. In some cases, this is to protect archeological sites from vandalism, while in other cases it is restricted at the request of the owner. See: Knoerl, John; Miller, Diane; Shrimpton, Rebecca H. (1990), Guidelines for Restricting Information about Historic and Prehistoric Resources, National Register Bulletin, National Park Service, U.S. Department of the Interior, OCLC 20706997.
  5. ^ a b c "Cape Krusenstern Archeological District". Archived from the original on October 7, 2012. Retrieved February 21, 2013.
  6. ^ NHL Documentation
  7. ^ Map of Cape Krusenstern National Monument (Map). National Park Service.
  8. ^ a b c d e f g h i j k l "Cape Krusenstern National Monument". Prehistory of Alaska. National Park Service. Retrieved February 21, 2013.
  9. ^ Roberta Forsell Stauffer (April 27, 2007). "Interior secretary approves district expansion". Newspaper article on expansion of National Historic Landmark Butte-Anaconda Historic District. The Montana Standard (newspaper). Retrieved November 1, 2007.
  10. ^ "History & Culture". Cape Krusenstern National Monument. National Park Service. Retrieved February 21, 2013.
  11. ^ "The Beach Ridges of the Cape". Cape Krusenstern National Monument. National Park Service. Retrieved February 21, 2013.
  12. ^ "Places". Cape Krusenstern National Monument. National Park Service. Retrieved February 21, 2013.
  13. ^ Giddings, J. Louis (1986). Beach ridge archeology of Cape Krusenstern : Eskimo and pre-Eskimo settlements around Kotzebue Sound, Alaska. National Park Service, U.S. Dept. of the Interior. OCLC 11519048.
  14. ^ a b "Nature and Science". Cape Krusenstern National Monument. National Park Service. Retrieved February 21, 2013.
  15. ^ "Frequently Asked Questions". Cape Krusenstern National Monument. National Park Service. Retrieved February 21, 2013.
  16. ^ "Weather". Cape Krusenstern National Monument. National Park Service. Retrieved February 21, 2013.
  17. ^ "Red Dog Mine". Alaska Department of Environmental Conservation. Archived from the original on March 30, 2013. Retrieved February 22, 2013.
  18. ^ Repanshek, Kurt (February 13, 2009). "Heavy Metals Detected in Wildlife of Cape Krusenstern National Monument". National Parks Traveler. Retrieved February 22, 2013.
  19. ^ "Things to Know Before You Come". Cape Krusenstern National Monument. National Park Service. Retrieved February 21, 2013.
  20. ^ "Operating Hours and Seasons". Cape Krusenstern National Monument. National Park Service. Retrieved February 21, 2013.
  21. ^ "Operating Hours and Seasons". Noatak National Preserve. National Park Service. Retrieved February 21, 2013.
  22. ^ "Northwest Arctic Heritage Center, Kotzebue, Alaska". Kobuk Valley National Park. National Park Service. Retrieved February 21, 2013.
  23. ^ Quinley, John. "Superintendent Named for Western Arctic National Parklands". Kobuk Valley National Park. National Park Service. Retrieved February 21, 2013.

Bibliography

  • Giddings, J. Louis and Douglas D. Anderson (1986). Beach Ridge Archeology of Cape Krusenstern: Eskimo and Pre-Eskimo Settlements around Kotzebue Sound, Alaska Publications in Archeology vol 20. Washington D.C.: National Park Service.