The Kenai Fjords, like much of Alaska’s landscape, were formed by two incredibly powerful but seemingly opposite forces: tectonic activity and glaciers. Fox Island is the kind of place that makes you feel good inside. Kenai Fjords National Park was established in 1980 by the Alaska National Interest Lands Conservation Act (ANILCA). In the process of their formation, hot silica-rich fluids penetrated the young rocks and then crystallized to form milky white quartz veins. We use cookies to personalise content and ads, to provide social media features and to analyse our traffic. Tectonic activity did the building We think of Alaska as a chillingly cold place, but that cold belies its volcanically active past, present, and future. The Kenai Fjords, like much of Alaska’s landscape, were formed by two incredibly powerful but seemingly opposite forces: tectonic activity and glaciers. Some stretch northwest into rugged hills of the Kenai Peninsula. Recent park management documents or current laws and policies can be found in the park management section. The fjords on the Kenai Peninsula in Alaska, which give the Kenai Fjords National Park its name, were created by the movement of the glacier known as Exit Glacier. However, much of the area deglaciated since 1950 is partly flooded most years; this has slowed succession compared to other chronosequences on glacial till. A short history. Valley glaciers are nestled in valleys and don’t reach the sea. A Slice of Early Seward: How Archeology Provides a glimpse into Daily Life in this Frontier Town (2013) by Dan Trepal. Kenai Fjords National Park goes a step further, too, making available Art for Parks Backpacks filled with art supplies to explore your creative side whilst in the aprk. It is a relatively small and accessible park by Alaskan national park standards, about 88% as big as Yosemite National Park. How Large is a Fjord? A true fjord is formed when a glacier cuts a U-shaped valley by ice segregation and abrasion of the surrounding bedrock. The Bear valley glacier, seen on Kenai Fjords Tours, is the largest glacier in Kenai Fjords National Park. Here you have a glimpse into the edge of the Hard­ing Ice­field. Visitors can walk around the bottom of Exit Glacier and learn about climate change in the nature center. Nov 21, 2017 - Explore MICHAEL SHERMAN's board "Kenai Fjords" on Pinterest. It is the only Alaska national park that did not originally allow subsistence use by Native Americans, but native vi… The fractures in the rock filled swiftly with jets of superheated water from deep in the Earth. 65 million years ago, the Kenai Mountains originated from the sands and muds deposited on the sea floor. In certain places, it was also broken. Kenai Fjords National Park is a land dominated by glaciers, massive rivers of ice that flow out from the Harding Icefield. The park’s dramatic landscape includes spectacular mountains with great glaciers flowing down between them to the sea, as well as mile-deep fjords that provide a habitat for thousands of nesting seabirds and smaller marine mammals such as sea otters, harbor seals, and sea lions. After the glaciers melt back a bit, seawater flows into the valley, submerging it and forming a steep-walled cove. JUNE 4 – SEPTEMBER 6, 2021. Hear the story of how the glaciers were formed and how the land recovers as they recede. The Sandstone found in Kenai Fjords National Park is typically; white, gray, yellowish, or dark red. Kenai Fjords National Park is a must see in Alaska. A vegetation chronosequence has developed on an outwash plain formed as Exit Glacier (Kenai Fjords National Park, Alaska, U.S.A.) retreated, beginning in the late 1700s. Source: Kenai Fjords National Park/Facebook … Glaciers, earthquakes, and ocean storms have shaped Alaska's Kenai Fjords for centuries, resulting in constantly changing terrain. ️ . This book would make a really nice coffee table book. The dramatic coastal fjords and valleys of the park reveal a long … 270. A plug dome volcano is made of solid lava. Beyond the Exit Glacier area, Kenai Fjords is really only accessible via water. Whether you are planning a trip to south-central Alaska or exploring from home, learn more about the history of the park by exploring these articles, books, recordings, and more about the history of this special area. Kenai Fjords National Park is located just outside the town of Seward in South-central Alaska, 126 miles south of Anchorage. Several different types of glaciers can be seen from our cruises, including tidewater, piedmont, hanging, and cirque glaciers. Thought for Kenai Fjords National Park: Provide shelter to others in the storm, just like fjords provide calm water refuge in rough seas. All of these rocks … How was Kenai Fjords formed? A Stern and Rock-Bound Coast (1998) by Linda Cook and Frank Norris. Thanks to the archeological investigations of the Seward Privy Project, researchers learned fascinating details about life in early Seward, Alaska. 5 Adventures That'll Make Your Stomach Drop, Information about the device's operating system, Information about other identifiers assigned to the device, The IP address from which the device accesses a client's website or mobile application, Information about the user's activity on that device, including web pages and mobile apps visited or used, Information about the geographic location of the device when it accesses a website or mobile application. Some rock was once coral reef close to the equator: It was carried along as the Pacific plate rotated counterclockwise, traveling north. Resurrection Bay: A boat trip out on the bay gives you a great view of the coast, and you can do a little fishing at the same time. Glaciers move slowly over time and leave significant changes to the landscape they pass over in a process known as glaciation. This ice­field is the main fea­ture of the Kenai Fjords Nation­al Park. One of the most astounding trademarks in the golden country of the South, KENAI FJORDS NATIONAL PARK is the perfect place to research fish for marine life, salmon and halibut, and to catch icebergs underwater … Don't miss this place! Things to do at Kenai Fjords National Park Visitor Center. Today, nearly 51 percent of the park is covered by ice. It was heated and pressed into a new form. Exit Glacier is an active glacier, meaning it is still in motion, though it is retreating into the icefield it is connected to. It is the fifth most-visited park in Alaska, but the 11th of 13 Alaska parks in area, and is the closest national park to Anchorage. Seward is accessible year round via the Seward Highway, a National Scenic Byway with stunning views of Turnagain Arm, Kenai Lake, glaciers, wetlands and rugged mountains. The bedrock of Kenai Fjords National Park was carried north by the action of the tectonic plates. The fjords of the Kenai Peninsula were formed by the advance and retreat of the glaciers. Fjords form when glaciers carve those deep, u-shaped valleys into the rocky earth near coastlines. As park glaciers retreat, more bedrock is exposed. The park covers an area of 669,984 acres (1,046.85 sq mi; 2,711.33 km) on the Kenai Peninsula in southcentral Alaska, near the town of Seward. There are even some parts of the rock, like fossils, that come from other parts of the world! Most people visit Kenai Fjords National Park to explore the Exit Glacier. The historic resource study of Kenai Fjords National Park. Such valleys are fjords when flooded by the ocean. Kenai Fjords has very unique rock structure. The ice-dammed lake above Bear Glacier, in Alaska's Kenai Fjords National Park was full on November 4. The book talks about the history of the national park, how people ended up in the Fjords, about how the glaciers got formed, wildlife and plant species found in the park. Just 12 miles by boat from Seward, Fox Island and Kenai Fjords Wilderness Lodge are a world away from all you know. Coastal landforms are created or formed as a result of wave processes. Kenai Fjords National Park was established in 1980 with the specific goals of maintaining the scenic beauty and environmental integrity of the Harding Icefield and its glaciers and fjords. Glaciers Of Kenai Fjords: Instructional Resources. Visit our exclusive Fox Island lodge and enjoy a delicious wild Alaska salmon buffet and a National Park Ranger program. Established in 1980, by the Alaska National Interest Lands Conservation Act, this book explores the administrative history of Kenai Fjords National Park. A fjord forms where a glacier cuts a gorge below sea level, and then retreats, allowing the sea to flood the channel. Sightseeing at Kenai Fjords National Park, History: How the Kenai Fjords Were Formed. The valley fills with water from a nearby ocean or sea, leaving steep rock formations above water on either side. Thus fjords … ADULT PRICE: $239.00. If you are only there for the day, you will want to visit the National Park visitor center. Cruise … Enjoy skipping rocks and a guided nature walk with a National Park Ranger. Find out if there are any ranger-led activities. The cost was $159.00 per person (our kids are no longer considered children). However, scientists believe that Lassen Peak formed relatively quickly in just a few years. See the film. On Facebook, the Kenai Fjords National Park service shared three photos of an “ice-dammed lake” above Bear Glacier taken on three different … Exit Glacier Project Jukebox is a digital branch of the University of Alaska Fairbanks Oral History Program. 8.5 Hour Northwestern Fjord Cruise. Since we weren’t up for a multi-day kayaking tour, we signed up for Major Marine Tour’s 7 1/2 hour tour of the fjords, glaciers, and wildlife of the park and it was stellar! All of this land was once buried beneath the ice and still bears its influence, in both the physical forms, and the everyday glacial terminology used at the park. . The reason it was made into a national park is to preserve the fjord, the surrounding rainforest, the diverse wildlife, Harding Icefield, and the … The boats usually depart form Seward or Whittier , small towns in southern Alaska settled approximately one-hour drive from each other. There are even some parts of the rock, like fossils, that come from other parts of the world! Often, they terminate in large, freshwater lagoons. The first section organizes the Instructional Resources by resource type. Often, they terminate in large, freshwater lagoons. Some rock was once coral reef close to the equator: It was carried along as the Pacific plate rotated counterclockwise, traveling north. Most of the rocks throughout Kenai Fjords are categorized in a group called the Chugach terrane which is mostly made up of two major types or smaller groups of rocks.The first mini group is made up of marine volcanic rocks combined with shale and chert. Big companies such as Major Marine Tours, Kenai Fjords Tours and Alaska Fjords Charters offer half-day to full-day tours. Kenai Fjords National Park has many fjords from glaciers that sprout off the Harding Icefield and flow down into the Gulf of Alaska. The park's headquarters is in Seward. A fjord is formed by the movement of a glacier that cuts rock formations, forming steep ridges or cliffs on each side of a valley. More than half of Kenai Fjords is obscured by it, and glaciers are one of Alaska’s coolest natural attractions. The scenery is gorgeous and seeing it is a sure thing (barring insane levels of fog.) This shallow threshold in the mouth of the fjord, is the reason that fjords often are quieter than the open sea. Glaciers continue to flow out of the mountains. Since the park was established, evidence of global climate change has been brought to the forefront of science. It is truly one of the most beautiful places I have ever been. The historic resource study of Kenai Fjords National Park. Take a fabulous boat tour and enjoy a day whale watching in Alaska! Sort By: Fjords are formed by the movement of glaciers. Tectonic activity did the building We think of Alaska as a chillingly cold place, but that cold belies its volcanically active past, present, and future. The work of the glacier then left an overdeepened U-shaped valley that ends abruptly at a valley or trough end. The ice age lingers here in the Harding Icefield which works as a thermostat for surrounding terrestrial and marine ecosystems. Kenai Fjords National Park The park landscape is a dramatic juxtaposition of land and water, shaped by the advance and retreat of glaciers. 10. They are formed on the many mountainsides and push slowly down, through the valleys. Renowned for jagged cliffs and pristine pebble beaches, they are a must-see for Alaska visitors. Kenai Fjords National Park is an American national park.The park covers a zone of 669,984 acres (2,711.3 km) on the Kenai Peninsula in south-central Alaska, close to the town of Seward. Established as a national monument in 1978, the Kenai Fjords National Park officially became a national park in 1980. After reading descriptions and reviews, I decided on Major Marine Tours’ 6 hours long Kenai Fjords Cruise. The park is capped by the largest icefield entirely contained within the United States, Harding Icefield, a 300 square mile expanse covering a mountain range under ice several thousand feet thick. Title, Alaska National Interest Lands Conservation Act. Formed dur­ing the ice age some 20, 000 years ago, the Hard­ing Ice­field is 30 miles wide by 50 miles long and in places pre­sumed to be 3000 – 5000 feet thick. By 2010, the status of the river was changed to a Category 2, or "water that attains its designated uses." According to the standard model, glaciers formed in pre-glacial valleys with a gently sloping valley floor. Glaciers move slowly over time and leave significant changes to the landscape they pass over in a process known as glaciation. Kenai Fjords has very unique rock structure. Geography. Kenai Fjords National Park is a United States National Park established in 1980 by the Alaska National Interest Lands Conservation Act. Date of experience: September 2020. Valley glaciers are nestled in valleys and don’t reach the sea. arete. These features are incredibly scenic and are a part of the reason that this region was protected and established as Kenai Fjords National Park. A vegetation chronosequence has developed on an outwash plain formed as Exit Glacier (Kenai Fjords National Park, Alaska, U.S.A.) retreated, beginning in the late 1700s. This project highlights conversations with long-term residents of Seward, Alaska about their lives, and the traditional activities in the area around Exit Glacier from 1950-1980. The coast of Kenai Fjords National Park continued for many miles to the southwest, but our time to explore was growing short. 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