Portage was once a roadside glacier, but it recedes an average of one foot a day and is now no longer visible from the road. However, its big blue icebergs are often found along the shore of the lake, right in front of the parking area. You can see the lake in a half hour, but may want to spend time at the Begich Boggs Visitor Center (½-1 hour), take the boat cruise (1 hour), or have lunch at the local cafeteria.
Directions: Head south from Anchorage on the Seward Highway, to the end of the 5-mile Portage Spur Road. You can visit the face of Portage by tour boat from the dock at the lake. Bring a light jacket, as winds tend to pick up around the face of the glacier itself.
Distance: 48 miles south of Anchorage.
Drive Time: 1 hour.
Explore Time: 1-4 hours.
You can hike right up to Seward's Exit Glacier and feel the dense blue ice while listening to it crackle. Walk the lower trail to get a good photo in front of the glacier face. Or, choose the more challenging 7-mile round-trip Harding Icefield Trail. There is a short ranger-led walk daily at 11am and 3pm, from Memorial Day through Labor Day.
Spencer Glacier rises 3,500 feet in a stunning, natural ramp from a lake of royal-blue icebergs in the Chugach National Forest just 60 miles south of Anchorage. It’s a family-friendly recreation destination featuring camping, hiking, glacier exploration, nature walks, paddling and sightseeing. Maybe best of all: You have to take a train to get there!
Portage Valley may be one of the most popular visitor destinations in Alaska, but don't let that scare you away. The truth is that most people stop at the visitor’s center for a quick walkthrough, take a photo on the deck and then get back on the road, to Whittier or elsewhere. And while it’s true that the valley's blue ice and glacial scenery is outstanding from More...
Not too spectacular in size, these hanging glaciers dangle from mountains in the Chugach National Forest. Several pullouts allow for viewing. They feed the nearby stream systems that harbor many species of salmon and trout. Tangle Pond and Tangle Creek are favorite fishing spots for locals, and there are lots of places to camp in Portage Valley itself.
Directions: Head south from Anchorage on the Seward Highway, along the 5-mile Portage Spur Road. You'll spot these glaciers on the south side of the road, halfway from the Seward Highway to Portage Lake (thus the name Middle Glacier). Check them out on your way to Portage and Byron.
Distance: 48 miles south of Anchorage.
Drive Time: 1 hour.
Explore Time: 1/2 – 2 hours.
This glacier, named after Northwestern University in 1909, can be found at the head of Northwestern Fjord in Kenai Fjords National Park, just under 30 miles southwest of Seward. By the second half of the 20th century, Northwestern Glacier's recession revealed a number of islands in the Fjord that had previously been covered in ice. Take a cruise from Seward and envision the entirety of of Northwestern Fjord filled with ice, as you make your way to Northwestern Glacier.
The 700-square-mile Harding Icefield, one of four major ice caps in the United States, crowns Kenai Fjords National Park. The icefield may be a remnant of the Pleistocene ice masses once covering half of Alaska. The magnificent coastline of Kenai Fjords is steep valleys that were carved by glaciers in retreat. Active glaciers still calve and crash into the sea as visitors watch from More...
Look for three alpine glaciers back in Thumb Cove. Alpine glaciers keep their ice in the alpine region of a mountain and don't descend to a valley floor or the tidewater's edge. From the left the three are Prospect, Spoon and Porcupine glaciers.
Notice the lovely cabin on the edge of Thumb Cove. The land of the Resurrection Peninsula is divided between state park, national More...
Pedersen Glacier, located in Kenai Fjords National Park, receded throughout the 20th century exposing Pedersen Spit and Pedersen Lagoon. In the 1980s, the lagoon was designated as the Pedersen Lagoon Wildlife Sanctuary, a 1,700-acre sanctuary meant to preserve and protect the area's wildlife and land. Take a cruise from Seward to see Pedersen Glacier, and the beautiful habitat surrounding it just under 20 miles away.
One hundred and fifty years ago the valley now occupied by the ship facility and correctional center was filled with the ice of Godwin Glacier. If you look just below the 4 mountain peaks to the left side of the valley you can see the ice of Godwin glacier. In the year 1850 this glacier calved icebergs into Resurrection Bay waters. Now a days Godwin glacier is a valley glacier and More...
Looking beyond the peninsula you can see snowcapped mountains. Here you have a glimpse into the edge of the Harding Icefield. This icefield is the main feature of the Kenai Fjords National Park. 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. There are at least 38 rivers of ice or More...
Holgate Glacier, found in Holgate Arm in Aialik Bay, within Kenai Fjords National Park, is a tidewater and mountain glacier. While it is one of the smaller glaciers in Aialik Bay, Holgate Glacier is still a popular destination to see calving glaciers. And it is actually advancing! Holgate Arm is often filled with ice, but on a good day you can get to a close and safe distance from the glacier. Catch a cruise from Seward, or go kayaking!
Bear Glacier, found in Kenai Fjords National Park, is a tidewater glacier and a popular spot for kayakers, but you can easily see it on a cruise from Seward. With massive icebergs and blue waters, seeing the glacier up close is a thrilling experience. Many people camp on the outer beach near Bear Glacier, and enjoy the glacier views in the background. This is also a great area to check for whales, sea otters, puffins, and other wildlife.
Both of these photographs were taken from the same location in Nuka Passage, about 6 kilometers (3.7 miles) south of the position of the 1909 terminus of the glacier. The first photograph by D.F. Higgins, is an August 6, 1909 view of the then retreating northern part of the terminus. The absence of any icebergs indicates that by 1909, the glacier was no longer tidewater. When More...