Nassau Fjord or Nassau Fiord is a four mile long inlet in Alaska branching off from Prince William Sound. Nassau Fjord is glacially carved and also home to the famous tidewater Chenega Glacier which shares a two mile long calving face with the Fjord. The Princeton and Tigertail Glaciers both come terminate within one mile of the fjord's waters as well. [1]
Due to the large amount of glacial activity in the fjord, it is a popular destination for many kayakers and boaters and features many icebergs. Most trips to the fjord leave from nearby Chenega or Whittier.
In physical geography, a fjord or fiord is a long, narrow sea inlet with steep sides or cliffs, created by a glacier. Fjords exist on the coasts of Antarctica, the Arctic, and surrounding landmasses of the northern and southern hemispheres. Norway's coastline is estimated to be 29,000 km (18,000 mi) long with its nearly 1,200 fjords, but only 2,500 km (1,600 mi) long excluding the fjords.
Chenega is a census-designated place (CDP) on Evans Island in the Chugach Census Area in the U.S. state of Alaska. Located in Prince William Sound, the CDP consists of the Chugach Alutiiq village of Chenega Bay, which was established only after the Good Friday earthquake destroyed the original community on Chenega Island to the north. As of the 2020 census, the population of the CDP was 59, largely Alaska Natives; as of 2021, the population of Chenega is estimated at 49. Chenega Bay is in the Chugach School District and has one school, Chenega Bay Community School, serving approximately 16 students from preschool through high school.
Cordova is a city in Chugach Census Area, Alaska, United States. It lies near the mouth of the Copper River, at the head of Orca Inlet on the east side of Prince William Sound. The population was 2,609 at the 2020 census, up from 2,239 in 2010.
Prince William Sound is a sound off the Gulf of Alaska on the south coast of the U.S. state of Alaska. It is located on the east side of the Kenai Peninsula. Its largest port is Valdez, at the southern terminus of the Trans-Alaska Pipeline System. Other settlements on the sound, which contains numerous small islands, include Cordova and Whittier plus the Alaska native villages of Chenega and Tatitlek.
The 1964 Alaskan earthquake, also known as the Great Alaskan earthquake and Good Friday earthquake, occurred at 5:36 PM AKST on Good Friday, March 27, 1964. Across south-central Alaska, ground fissures, collapsing structures, and tsunamis resulting from the earthquake caused about 131 deaths.
The Kenai Peninsula is a large peninsula jutting from the coast of Southcentral Alaska. The name Kenai is derived from the word "Kenaitze" or "Kenaitze Indian Tribe", the name of the Native Athabascan Alaskan tribe, the Kahtnuht’ana Dena’ina, who historically inhabited the area. They called the Kenai Peninsula Yaghanen.
Hubbard Glacier is a glacier located in Wrangell–St. Elias National Park and Preserve in eastern Alaska and Kluane National Park and Reserve in Yukon, Canada, and named after Gardiner Hubbard.
Kenai Fjords National Park is an American national park that comprises the Harding Icefield, its outflowing glaciers, and coastal fjords and islands. The park covers an area of 669,984 acres on the Kenai Peninsula in south-central Alaska, west of the town of Seward.
Evans Island is an island in the Prince William Sound of southern Alaska. It lies just east of Bainbridge Island across the Prince of Wales Passage. Elrington Island lies to its south, Latouche Island to its southeast, and Knight Island to its northeast. Although Evans Island had been inhabited up to the time of the Russian exploration of Alaska, the island had no modern-day inhabitants until 1984, when a group of residents and former residents of the original Alutiq village of Chenega, on Chenega Island, decided to build the village of Chenega Bay on Crab Bay on Evans Island. Old Chenega had been destroyed and one-third of its residents had been killed by the tsunami from the 1964 Alaska earthquake. The new community of Chenega is coextensive with Evans Island, which has a land area of 74.605 km2 and a population of 86 persons as of the 2000 census.
Orca Inlet is an arm of Prince William Sound in southern Alaska. The town of Cordova was founded on its coast in 1906. All marine traffic reaches the town through Orca Inlet.
College Fjord is a fjord located in the northern sector of Prince William Sound in the U.S. state of Alaska. The fjord contains five tidewater glaciers, five large valley glaciers, and dozens of smaller glaciers, most named after renowned East Coast colleges. College Fjord was discovered in 1899 during the Harriman Expedition, at which time the glaciers were named. The expedition included a Harvard and an Amherst professor, and they named many of the glaciers after elite colleges. According to Bruce Molina, author of Alaska's Glaciers, "They took great delight in ignoring Princeton."
Portage Glacier is a glacier on the Kenai Peninsula of the U.S. state of Alaska and is included within the Chugach National Forest. It is located south of Portage Lake and 6 km (4 mi) west of Whittier.
Chenega Glacier is a tidewater glacier located in Prince William Sound and on the Kenai Peninsula in the U.S. state of Alaska.
Chenega Island is an island in Prince William Sound in the U.S. state of Alaska. It is the traditional home to the community of Chenega, though much of its population eventually migrated to Chenega Bay on nearby Evans Island after the 1964 Good Friday earthquake and accompanying tsunami. Chenega Island and its surrounding habitat were also heavily impacted by the 1989 Exxon Valdez oil spill. The island has a land area of 57.084 km2 and, after the mass emigration, was unpopulated as of the 2000 census.
The Sargent Icefield is a large icefield located on the eastern portion of the Kenai Peninsula bordering Prince William Sound in Alaska. The ice field has numerous outflow glaciers including the Chenega, Princeton, and Ellsworth Glaciers.
The Knik Glacier is an ice field located 50 miles (80 km) east of Anchorage, Alaska on the northern end of the Chugach Mountains. The ice field averages over 25 miles (40 km) long and over 5 miles (8.0 km) across, making it one of the largest glaciers in southcentral Alaska. Knik Glacier feeds the 25-mile (40 km) long Knik River which empties into the Knik Arm section of Cook Inlet.
Knight Island is an island in western Prince William Sound of the Gulf of Alaska in the U.S. state of Alaska.
The Princeton Glacier is a glacier in the Sargent Icefield, Kenai Peninsula in Alaska.
The Harvard Glacier is a large tidewater glacier in the Alaska's Prince William Sound. The glacier has a 1.5-mile (2 km) wide face where it calves into the College Fjord. It is 300 ft thick and covers 120,000 acres of Chugach National Forest. The Harvard Glacier is the second largest glacier in the Prince William Sound, after the Columbia Glacier. It is a popular destination of cruise ships in the Prince William Sound.
The Prince Christian Sound is a waterway in Southern Greenland. It separates the mainland from Sammisoq and other islands of the Cape Farewell Archipelago near the southernmost tip of Greenland. The name was given in honour of the prince, later king Christian VIII of Denmark.
60°15′46″N148°21′25″W / 60.26278°N 148.35694°W