Great Land of Alaska

Burns Glacier (on the left side of the valley) is easily visible from the highway and is a popular tourist destination. It's located a short drive away from Anchorage at the eastern end of Portage Valley. Portage Glacier is barely visible in this picture in the bottom center.

Bryn Mawn Glacier is one of the many glaciers seen from the Phillip's 26-Glacier Cruise based in Whittier. This glacier has begun to receed, showing bare eroded rock at its base.

The small valleys and mountain sides of Portage Valley are abundant with glaciers. Byron Glacier is one of the many smaller glaciers between the mountains in this valley.

Deadman Glacier is a small Kenai Mountains glacier in the Placer River valley. The Kenai Mountains are not exceptionally high, but do have a large number of glaciers and ice fields due to the massive quantities of snow that fall on them during the winter.

Harding Icefield is a large "lake" of ice high in the Kenai Mountains. Several small glaciers flow from this ice field, and it is one of the many sources of the Kenai and Kasilof Rivers.

Harvard Glacier is the climax to the Phillip's 26-Glacier cruise. Located at the end of College Fjord, it is a large wide tidewater glacier. Passengers on the cruise are often treated to the impressive sight of a large piece of ice calving from the glacier and falling into the water.

With all of the rock and gravel covering Learnard Glacier's terminal, it's hard to tell that this is a glacier.

Matanuska Glacier is a large glacier that's about a 2-hour drive east of Anchorage. It isn't as popular as Portage Glacier due to its distance, but it is a very impressive glacier. It is visible from many areas of the Glenn Highway and a small road leads to it, giving adventurers a chance to take a short walk on it.

Matanuska Glacier is by no means amongst the largest glaciers of Alaska, but it's large enough, and being located right next to the Glenn Highway, it's a popular hiking destination for adventurers from both within and without Alaska. The last picture in this series shows that this somewhat average-sized glacer is still pretty large, as indicated by the comparitive size of the hikers circled in red.

Another small Portage Valley glacier, this one clinging to the side of Maynard Mountain. There are so many small glaciers in this area that many are either unnamed or else have obscure hard-to-find names.

Portage Glacier, perhaps one of Southcentral Alaska's most visited glaciers. This glacier has retreated quite a bit over the past several decades--it used to be easily visible from the highway but now only the very tip of its terminal is visible. A large lake, Portage Lake, has formed at this glacier's terminal. Daily cruises on this lake give visitors a chance to see the glacier up close.

A few more Portage Valley glaciers, possibly unnamed.

Skilak Glacier is one of the many glaciers flowing from the Kenai Mountain's Harding Icefield. The river flowing from the lake in the first picture is Skilak River, which empties into Skilak Lake.

Smith Glacier is yet another one of the many glaciers seen on the Phillip's 26-Glacier cruise in College Fjord.

Spencer Glacier is an impressive Kenai Mountains glacier. It is not reachable by highway, visitors must either take the train or hike to it. A tour company offers float trips through the lake at the glacer's terminal and down the small river flowing from the lake.

Surprise Glacier is a tidewater glacier in the Kenai Peninsula's Harriman Fjord. It is another stop on the Phillip's 26-Glacier cruise.

High in the Chugach Mountains near Thompson Pass is Worthington Glacier, a large impressive alpine glacier easily seen from the Richardson Highway.

A tiny, presumably unnamed glacier of the Kenai Mountains.