Katmai National Park and Preserve
|Katmai National Park and Preserve|
IUCN category VI (protected area with sustainable use of natural resources)
The summit crater lake of Mount Katmai
|Location||Lake and Peninsula, Kodiak Island, Kenai Peninsula, and Bristol Bay boroughs, Alaska, USA|
|Nearest city||King Salmon|
|Area||4,093,077 acres (1,656,409 ha)|
|Established||December 2, 1980|
|Visitors||39,818 (in 2012)|
|Governing body||National Park Service|
Katmai National Park and Preserve is a United States National Park and Preserve in southern Alaska, notable for the Valley of Ten Thousand Smokes and for its grizzly bears. The park and preserve covers 4,093,077 acres (6,395.43 sq mi; 16,564.09 km2), being roughly the size of Wales. Most of this is a designated wilderness area in the national park where all sport hunting is banned, including over 3,922,000 acres of land. The park is named after Mount Katmai, its centerpiece stratovolcano. The park is located on the Alaska Peninsula, across from Kodiak Island, with headquarters in nearby King Salmon, about 290 miles (470 km) southwest of Anchorage. The area was first designated a national monument in 1918 to protect the area around the major 1912 volcanic eruption of Novarupta, which formed the Valley of Ten Thousand Smokes, a 40-square-mile (100 km2), 100-to-700-foot-deep (30 to 213 m) pyroclastic flow. The park includes as many as 18 individual volcanoes, seven of which have been active since 1900.
Following its designation, the monument was left undeveloped and largely unvisited until the 1950s. Initially designated because of its violent volcanic history, the monument and surrounding lands became appreciated for their abundance of sockeye salmon, the grizzly bears that fed upon them, and a wide variety of other Alaskan wildlife and marine life. After a series of boundary expansions, the present national park and preserve were established in 1980 under the Alaska National Interest Lands Conservation Act in 1980.
Katmai occupies the Pacific Ocean side of the Alaska Peninsula, opposite Kodiak Island on the Shelikof Strait. The park's chief features are its coast, the Aleutian Range with a chain of fifteen volcanic mountains across the coastal southeastern part of the park, and a series of large lakes in the flatter western part of the park. The closest significant town to the park is King Salmon, where the park's headquarters is located, about 5 miles (8.0 km) down the Naknek River from the park entrance. The Alaska Peninsula Highway connects Naknek Lake near the entrance to King Salmon, continuing to the mouth of the river at Naknek. The road is not connected to the Alaska road system. Access to the park's interior is by boat on Naknek Lake. Another road runs from Brooks Camp to Three Forks, which overlooks the Valley of Ten Thousand Smokes. The 497-mile (800 km) long coastline is deeply indented, running from the entrance to the Cook Inlet at Kamishak Bay south to Cape Kubugakli. The mountains run from southwest to northeast, about 15 miles (24 km) inland.
The park includes McNeil River State Game Sanctuary and Refuge on Kamishak Bay. The Alagnak River, designated a wild river, originates within the preserve at Kukaklek Lake. The Naknek River, which empties into Bristol Bay, originates within the park. The park adjoins Becharof National Wildlife Refuge to the south. Of the park and preserve's acres, 3,922,529 acres (1,587,391 hectares) are in the national park where all sport and subsistence hunting is prohibited. 418,548 acres (169,380 ha) are preserve lands, where both sport and subsistence hunting are permitted. The most commonly hunted species in the preserve include grizzly bear, which has lead to some problems about bear hunting due to small preserve population sizes and stalking bears to close limits.
The foundation rocks on the Alaska Peninsula are divided by the Bruin Bay Fault into fossiliferous sedimentary rocks of Jurassic and Cretaceous age to the east and metamorphic and igneous rocks to the west. The granite Aleutian Range batholith has intruded through these rocks. The majority of the higher mountains in the park are of volcanic origin. The park has been extensively altered by glaciation, both in the high lands where the mountains have been sculpted by glaciers, and in the lowlands where lakes have been excavated. Outwash plains and terminal moraines are also featured in the park. Soil types vary from rock or volcanic ash of vary depth to deep, wet soils overlain with peat Although permafrost exists.at higher elevations, it is not present in the lowlands.
Two physiographic provinces cover the park. The Aleutian Range province is composed of the Shelikof Strait coastline, about 10 miles (16 km) deep along the coast, the Aleutian Mountain zone, and the lake, or Hudsonian zone. Farther west the Nushagak-Bristol Bay Lowlands province is separated from the Aleutian zone by the Bruin Bay Fault, occupying a small corner of the park.
The active volcanoes in the park are Mount Katmai, Novarupta, Trident Volcano, Mount Mageik, Mount Martin and Fourpeaked Volcano. Other volcanoes that have erupted in recent times in geological terms, but not in historical times, are Mount Cerberus, Falling Mountain, Mount Griggs, Snowy Mountain, Mount Denison, Mount Kukak, Devils Desk, Mount Kaguyak, Mount Douglas and Mount Kejulik. Martin and Mageik produce steam that can be seen from King Salmon, while Trident was active in 1957–1965 and 1968.
The most significant volcanic event in historical times was the simultaneous eruption of Mount Katmai and Novarupta in June 1912. Novarupta's eruption produced a pyroclastic flow that covered a nearby valley with ash as much as 300 feet (91 m) thick. At the same time the summit of Katmai collapsed into a caldera. As the valley deposits cooled, they emitted steam from fissures and fumaroles, earning the name "Valley of Ten Thousand Smokes." As heat has dissipated from the deposits the steam vents have subsided and the valley has been eroded. At present streams have cut canyons as much as 100 feet (30 m) deep, but only 5 feet (1.5 m) to 10 feet (3.0 m) wide. Katmai is a stratovolcano, 6,716 feet (2,047 m) in height, with a large summit caldera. Several glaciers originate from the mountain, and one in the caldera is the only glacier known to have formed in historical times. The caldera floor is about 250 metres (820 ft) below the rim. The mountain stands on Jurassic sedimentary rocks, and its volcanic components are less than 1,500 feet (460 m) thick. Apart from the 1912 eruption, no significant activity has occurred in historical times. Novarupta is described as a Plinian pyroclastic vent with a plug dome, a 2,000-metre (6,600 ft) diameter crater with a 65-metre (213 ft), 400-metre (1,300 ft) diameter dome in the middle. Its only historical activity was the 1912 eruption.
Trident is a complex of three stratovolcanoes, the highest of which is 3,599 feet (1,097 m) tall, standing up to 1,894 feet (577 m) above their base. Trident has been intermittently active in historical times, primarily between 1953 and 1974. During that time about 0.7 cubic kilometers of material was erupted to form a new peak called Southwest Trident from the former site of a large fumarolic pit. Mount Martin is 6,102 feet (1,860 m) high, standing on a 1,400-metre (4,600 ft) high ridge near Mount Mageik. The summit has a 300-metre (980 ft) diameter crater, containing fumaroles and sometimes a crater lake. A large lava flow extends from the mountain to fill the upper part of Angle Creek's valley with about five cubic kilometers of material. There have been no significant eruptions from Martin, but the summit emits steam and the volcano is the site of earthquake swarms. Mageik stands on the same sedimentary rocks as Martin. The composite structure has four vents, the highest at 7,103 feet (2,165 m) and three subsidiary vent cones. A small crater hold a lake and fumaroles on the highest cone's flank. Apart from steaming there has been no recent activity, but there was a large debris avalanche in 1912, probably associated with the eruption of Katmai, amounting to between 0.05 and 0.10 cubic kilometer in volcume. Fourpeaked Mountain is a stratovolcano with a probable vent at the summit. Much of the 6,903-foot (2,104 m) mountain is covered by Fourpeaked Glacier. Fourpeaked produced phreatic eruptions in September 2006.
Mount Griggs is a 7,602-foot (2,317 m) stratovolcano near Novarupta, and somewhat to the northwest of the otherwise straight line of volcanoes in Katmai. The flat-topped mountain has three concentric craters, the largest 1,500 metres (4,900 ft) wide. The mountain's geochemistry differs from its neighbors. Griggs has active sulfurous fumaroles. Snowy Mountain is a small volcano 7,090 feet (2,160 m) tall, with ten significant glaciers covering almost all of the mountain. Roughly a third to half of the mountain has been eroded by glacial action. The volcano has two vents about 4 kilometres (2.5 mi) apart, and active fumaroles at the tallest summit. Mount Denison is a 7,605-foot (2,318 m) peak with four related vents at the head of three glaciers, the tallest point in the park. Mount Kukak is another ice-covered volcano, 6,693 feet (2,040 m) tall. It has a strong fumarole field near the summit. Devils Desk is a heavily eroded stratovolcano, 6,411 feet (1,954 m) high. Kaguyak is a stratovolcano truncated by a caldera, like Katmai. The highest peak is 2,956 feet (901 m), with a 2.5-kilometre (1.6 mi) diameter crater lake. There are two large domes within the caldera and two on the flanks. Mount Douglas is a 7,021-foot (2,140 m) stratovolcano, extensively eroded by ice, with a small acidic crater lake at its summit. 7,454-foot (2,272 m) Mount Steller is located between Kukak and Denison, with an unknown number of vents in ice-covered terrain. Kejulik is a 4,977-foot (1,517 m) eroded volcanic remnant. None of these volcanoes have exhibited significant behavior in historic times.
Katmai is also well known for grizzly bears and the salmon which attract both bears and people. Katmai contains the world's largest protected brown/grizzly bear population, estimated to number about 2,200. Bears are especially likely to congregate at the Brooks Falls viewing platform when the salmon are spawning, and many well known photographs of grizzly bears have been taken there. The salmon arrive early at Brooks Falls compared to other streams, and between 43 and 70 individual bears have been documented at the falls in July and an equal amount of bears are seen in the lower river in September. The coastal areas such as Hallo Bay, Kukak Bay, Kuliak Bay, Kaflia Bay, Geographic Harbor and Chiniak Bay also host very high population densities of bears year-round, due to the availability of clams and edible coastal sedge as well as salmon and other fish. Other hotspots include Swikshak Lagoon, American Creek, and in the preserve, Moraine Creek and Funnel Creek.
The vast majority of Katmai visitors come to Brooks Camp, one of the only developed areas of the park, and few venture further than the bear viewing platforms and the adjacent Brooks Camp area. Rangers at the park are extremely careful not to allow bears to obtain human food or get into confrontations with humans. As a result, bears in Katmai Park are uniquely unafraid of and uninterested in humans, and will allow people to approach (and photograph) much more closely than bears elsewhere. New webcams pioneered by the NPS will bring the 100 bears of Brooks Camp directly to your computer or smartphone. July and September are by far the best months for viewing Grizzly Bears in the Brooks Camp area.
Lodging is available in the park at Brooks Camp and Grosvenor Lodge and at several other lodges scattered around the park on inholdings.
Weather at Katmai is variable, though reliably rainy or drizzly. Summer high temperatures average about 63 °F (17 °C) and winter lows are between −4 °F (−20 °C) and 40 °F (4 °C). Fall is somewhat drier than the rest of the year, and warm days can occur year round. Rainfall is heaviest near the coast, with up to 60 inches (150 cm), and lighter to the west. The park supports 29 mammal species, 137 bird species, 24 freshwater fish species and four anadromous fish species.
Apart from its famous grizzly bears, Katmai also has moose, gray wolves, beavers, porcupines, martens and other mammals. Marine mammals include hair seals, sea lions, sea otters. Cetaceans include beluga whales, orcas and gray whales. Caribou occasionally winter within the park. 
The most important fish in the park are sockeye salmon, who feed bears, bald eagles and others during their spawning runs in the park's rivers. Salmon enter the Naknek River drainage from Bristol Bay in June and July and spawn from August to October.
Prehistoric artifacts have been found dating to about 6,000 years before the present near the old Katmai village. A number of other sites have been found along the coast, with occupation into historic times. Inland, Brooks Camp is a significant archaeological site dating to about 4500 BP, listed on the National Register of Historic Places (NRHP) in 1977 and designated a National Historic Landmark in 1993. Another village has been documented near the junction of the Savonoski and Grosvenor Rivers, listed on the NRHP as the Old Savonoski Site.
Russians were the first Europeans to arrive in the area in significant numbers, trading in furs. They encountered the Aglegmuit Eskimos on the Bristol Bay side of the peninsula and the Koniag Eskino on the Shelikov Strait side. Katmai Village was the only location within the park where Europeans lived through the mid-19th century, though their numbers were always few. In the latter part of the 19th century a few villages were established inland at Severnosky and along the coast at Douglas and Kukak. American traders operating for the Alaska Commercial Company took the place of the Russians. As sea otters became scarce the trade dried up, and Katmai and Douglas were abandoned in the early 20th century. In the 1890s the region was a route for travelers going to Nome for Nome's short-lived gold rush. Writer Rex Beach was one of these, writing about life on Bristol Bay during the salmon run in The Silver Horde. Prospects for oil, gold and coal received brief attention, then died out by 1912.
By 1898 there were reports of frequent earthquakes in the vicinity of Katmai Pass. These intensified around June 1, 1912, inducing the few local residents to leave. Katmai and Novarupta erupted on June 6 with a noise heard in Fairbanks, 500 miles (800 km) away, and Juneau, 750 miles (1,210 km) distant. Heavy eruptions continued through June 7, then gradually declined from June 8 onwards. Ash fell 6 inches (15 cm) to 12 inches (30 cm) deep in Kodiak, and ash fell on the Alaskan mainland and eastwards as far as Puget Sound. Atmospheric haze was noted worldwide, and temperatures were depressed in the northern hemisphere during the second half of 1912. Initial reports pinpointed Mount Katmai as the center of eruption. Later reports cast doubt on Katmai's primary role, and it was not until 1954 that Novarupta was found to be the primary volcanic center. The region around the mountains, which had received heavy ashfall, was devastated.
The National Geographic Society backed five expeditions to Katmai, beginning in 1915 with a trip to Kodiak Island and a short stay on the mainland. The expedition, led by Robert Fiske Griggs, a botanist who was initially interested in the study of plant recolonization. Griggs' follow-up expedition in 1916 discovered and named the Valley of Ten Thousand Smokes and found Novarupta. The National Geographic Society, delighted with the discoveries, funded a larger expedition in 1917 to make a survey of the region. The subsequent articles published in National Geographic magazine brought the region to prominence in the public, and Griggs began to advocate for the protection of the area in the national park system, backed by the National Geographic Society. At this time legislation to establish Mount McKinley National Park (later renamed Denali National Park) was pending, and the idea of making Katmai a national park was discussed by National Park Service acting director Horace M. Albright and National Geographic Society president Gilbert Hovey Grosvenor. Albright advised that national park legislation was unlikely to pass, suggesting instead that the region be protected as a national monument by the President, using the Antiquities Act of 1906. After some negotiation, and after a 1918 expedition opined that the Valley of Ten Thousand Smokes was a permanent feature, a proclamation was prepared to protect 1,080,000 acres (440,000 ha) around Mount Katmai, the valley, and the Iliuk Arm on the coast. Although only a third the area of the present park and preserve, the monument was nevertheless half the size of Yellowstone National Park from the outset. President Woodrow Wilson signed the proclamation of Katmai National Monument on September 24, 1918.
The proclamation had little immediate effect, other than grumbling from territorial officials. A 1923 expedition found that the region had little exploitable mineral potential. Tourists in the early 1920s amounted to a few dozen. No Park Service staff were assigned to the site, which was in theory administered by Mount McKinley. By 1928 more visitors arrived. The most prominent among them was Father Bernard R. Hubbard, an explorer of Alaska who gained fame as "The Glacier Priest." Hubbard documented the Valley of Ten Thousand Smokes in movies that he showed at lectures until the 1950s. At the same time, the Park Service became aware that Katmai was among the best brown bear habitat in Alaska, and that the monument should be expanded to protect them and the prolific salmon spawning grounds. In 1931 President Herbert Hoover issued a proclamation expanding the monument under the Antiquities Act to 2,697,590 acres (1,091,680 ha), more than doubling it in size and creating the largest single Park Service unit. Crucially, the expanded monument included the falls at Brooks Camp, while avoiding lands along the coast thought to have potential oil deposits.
In 1937 a ranger was finally assigned to Katmai, seconded to the monument from Mount McKinley, spending most of June trying to get there and one day in the monument before returning to Mount McKinley. In 1939 the Bureau of Fisheries established an encampment at the Brooks Lake outlet, having previously blasted out part of the falls in 1921. At about the same time the Park Service became concerned about illegal trapping in the monument, asking the Alaska Fish and Game Commission to send wardens to patrol the area. Several trappers were apprehended, and Park Service personnel visited the monument, sending back positive reports on the scenery and wildlife. These reports, and efforts to make poaching more difficult, led to another boundary adjustment that included the islands in the Shelikof Strait and Cook Inlet within 5 miles (8.0 km) of the old boundary, signed by President Franklin D. Roosevelt on August 4, 1941, which increased the monument's area by several thousand acres.
Poaching increased after World War II. At the same time, Alaskan territorial interests sought to have the monument disestablished or reduced in size to allow mining and fishing, because the activity at the Valley of Ten Thousand Smokes had declined, and because the Park Service had made no effort to develop the monument for visitors. These proposals were turned aside, and in 1950 a seasonal ranger was assigned to Katmai. William Nancarrow built a small camp at Brooks River. By the mid-1950s the Park Service embarked on its Mission 66 program to expand visitor services. Katmai was to receive a headquarters at King Salmon, a visitor center at Valley Junction in the Valley of Ten Thousand Smokes, ranger stations, campgrounds, modest roads and dock facilities on the lakes. An airstrip was also proposed for Brooks Camp. The airstrip was not built, but a road from Brooks Camp to the valley was built. In the early 1960s a road was proposed that would run across the peninsula through the park, connecting to King Salmon. The Park Service was opposed. The 1964 Alaska earthquake stalled the proposal for several years, resurfacing in 1968 with local support. However, the Park Service opposed the plans and the road project was set aside. In the meantime headquarters facilities were developed at King Salmon. In 1967 the state of Alaska set aside the McNeil River State Game Sanctuary with 83,600 acres (33,800 ha) under protection to safeguard the bear fishing grounds on the river, adjacent to Katmai. McNeil River was declared a National Natural Landmark in 1968.
When George B. Hartzog, Jr. became director of the National Park Service in 1964 he commissioned a report on Alaskan public lands, entitled Operation Great Land. The study identified 39 site that might become preserves or recreation lands, and it recommended that Katmai be expanded somewhat to the west and substantially to the north. The boundary adjustments were amended to a westward expansion of 94,547 acres (38,262 ha) that President Lyndon B. Johnson signed in 1968, producing anger in Alaska. In 1971 Katmai finally gained a full-time, on-site park superintendent. Also in 1971, Congress passed the Alaska Native Claims Settlement Act (ANCSA), which established a framework to divide up Alaska's federal lands. ANCSA established a timetable for claims, withdrawals and designations, requiring the Park Service to come up with a plan for future park units. The Park Service proposed 33,000,000 acres (13,000,000 ha) of new park lands, among them a 1,218,490-acre (493,110 ha) expansion of Katmai. Through the mid-1990s a variety of proposals were circulated for expansion and wilderness designation. At the same time, concerns were raised about the wthdrawal of game lands from sport hunting, and the ability of local residents to continue to practice subsistence hunting. To address these concerns, legislation was proposed to create national preserve lands that would confer protection while allowing regulated sport hunting. Early versions of the Alaska National Interest Lands Conservation Act (ANILCA) proposed Katmai National Park and Preserve as a combination of park and preserve lands. This legislation was stalled in Congress by 1978. Because a deadline was approaching for state selection of public lands, President Jimmy Carter used his authority under the Antiquities Act to expand Katmai by 1,370,000 acres (550,000 ha) on December 1, 1978, mainly on the northern side of the monument.
National Park and Preserve
It took two more years for Congress to act on a final ANILCA bill. The final bill established Katmai National Park and Preserve with 1,037,000 acres (420,000 ha) of expanded park and 308,000 acres (125,000 ha) of preserve, with 3,475,000 acres (1,406,000 ha) of wilderness lands within the national park where all hunting is prohibited. Unlike most ANILCA parks, the legislation for Katmai did not grant subsistence hunting access to national park lands, only to the preserve. Sport and subsistence hunting is prohibited in Katmai National Park but allowed in the preserve.
Exxon Valdez oil spill
The grounding of the oil tanker Exxon Valdez in Prince William Sound on March 24, 1989 produced extensive contamination of the Katmai coastline. By early April oil had reached Kenai Fjords National Park. Oil reached Cape Douglas in Katmai on April 26 and points southwards in the following week. In early May a variety of dredges and skimmer vessels were working in the Shelikof Strait, but 90% of the Katmai coastline was oiled. The worst-hit areas were Cape Cjiniak and Chiniak Lagoon, Hallo Bay Beach and its lagoon, Cape Gull and Kaflia Bay, and Cape Douglas. Casualties in birds alone were estimated at 8,400 dead birds. Work resumed in 1990, with smaller efforts in 1991 to catch the last oil.
- National Register of Historic Places listings in Katmai National Park and Preserve
- Timothy Treadwell
- Katmai: Alaska's Wild Peninsula A film by John Grabowska.
- "Listing of acreage as of December 31, 2011". Land Resource Division, National Park Service. Retrieved 2012-03-07.
- "NPS Annual Recreation Visits Report". National Park Service. Retrieved 2012-03-07.
- "Map of Katmai National Park and Preserve". National Park Service. Retrieved 3 March 2013.
- "Coasts/Shorelines". Katmai National Park and Preserve. National Park Service. Retrieved 3 March 2013.
- "Katmai Preserve Bear Hunt". National Parks Traveler.
- "Katmai Hunting". National Park Service.
- "Geologic Activities". Katmai National Park and Preserve. National Park Service. Retrieved 4 March 2013.
- Norris, Ch. 1
- "Volcanoes & Lava Flows". Katmai National Park and Preserve. National Park Service. Retrieved 3 March 2013.
- "Mount Katmai description and information". Alaska Volcano Observatory. Retrieved 4 March 2013.
- "Katmai reported activity". Alaska Volcano Observatory. Retrieved 4 March 2013.
- "Novarupta description and information". Alaska Volcano Observatory. Retrieved 4 March 2013.
- "Novarupta reported activity". Alaska Volcano Observatory. Retrieved 4 March 2013.
- "Trident Volcano description and information". Alaska Volcano Observatory. Retrieved 4 March 2013.
- "Trident reported activity". Alaska Volcano Observatory. Retrieved 4 March 2013.
- "Mount Martin description and information". Alaska Volcano Observatory. Retrieved 4 March 2013.
- "Mount Martin reported activity". Alaska Volcano Observatory. Retrieved 4 March 2013.
- "Mount Mageik description and information". Alaska Volcano Observatory. Retrieved 5 March 2013.
- "Mageik reported activity". Alaska Volcano Observatory. Retrieved 5 March 2013.
- "Fourpeaked Mountain description and information". Alaska Volcano Observatory. Retrieved 5 March 2013.
- "Fourpeaked reported activity". Alaska Volcano Observatory. Retrieved 5 March 2013.
- "Mount Griggs description and information". Alaska Volcano Observatory. Retrieved 5 March 2013.
- "Snowy Mountain description and information". Alaska Volcano Observatory. Retrieved 5 March 2013.
- "Mount Denison description and information". Alaska Volcano Observatory.
- "Kukak Volcano description and information". Alaska Volcano Observatory. Retrieved 5 March 2013.
- "Devils Desk description and information". Alaska Volcano Observatory. Retrieved 5 March 2013.
- "Kaguyak Crater description and information". Alaska Volcano Observatory. Retrieved 5 March 2013.
- "Mount Douglas description and information". Alaska Volcano Observatory. Retrieved 5 March 2013.
- "Mount Steller description and information". Alaska Volcano Observatory. Retrieved 5 March 2013.
- "Kejulik description and information". Alaska Volcano Observatory. Retrieved 5 March 2013.
- "Plan Your Visit - Katmai National Park & Preserve". National Park Service. Retrieved 4 March 2013.
- "Brown Bears of Katmai". Katmai National Park and Preserve. National Park Service. Retrieved 4 March 2013.
- "Bear Watching in Katmai National Park and Preserve". National Park Service. Retrieved 4 March 2013.
- /printheadline.cfm?type=Announcements&id=12427 "Webcams Make Katmai Bears Accessible (NPS Digest)". National Park Service. Retrieved 24 July 2012.
- "Live Webstream Captures Fishing Bears | American Forests". American Forests. Retrieved 26 July 2012.
- "Lodging". Katmai National Park and Preserve. National Park Service. Retrieved 3 March 2013.
- "Weather". Katmai National Park and Preserve. National Park Service. Retrieved 5 March 2013.
- "Animals". Katmai National Park and Preserve. National Park Service. Retrieved 5 March 2013.
- "Fish". Katmai National Park and Preserve. National Park Service. Retrieved 5 March 2013.
- Norris, Ch. 2
- Norris, Ch. 3
- Norris, Ch. 4
- "Katmai National Park and Preserve". National Park Service. Retrieved 3 March 2013.
- Norris, Ch. 5
- "Superintendent Named for Katmai National Park". Aniakchak National Monument and Preserve. National Park Service. Retrieved 3 March 2013.
- Norris, Frank B. (1996) Isolated Paradise: An Administrative History of the Katmai and Aniakchak NPS Units, Alaska, National Park Service
|Wikimedia Commons has media related to Katmai National Park.|
|Wikivoyage has a travel guide for Katmai National Park.|
- Katmai National Park and Preserve National Park Service site
- Katmai National Park and Preserve at the National Park Service Alaska Regional Office