A couple of weekends ago I had the opportunity to tour Glacier Bay National Park with Hoonah’s 5th and 6th grade class. The trip was the culmination of their “Plumes of Glacier Bay” curriculum where they had been studying the species of birds within the park. As an avid birder I was thrilled to bring these 16, rambunctious kids on an ecology trip into the park on the “Dayboat”. The boat travels into the park to pick up travelers and provides an 8.5 hour, 130+ mile cruise to tidewater glaciers with opportunities to view tons of wildlife.
Its not always (one might say rarely) sunny in Glacier Bay. The cold waters and moist air cause rain and fog to form quickly within the park. However, we started out our day under high clouds with small patches of blue sky. Just after launching, we encountered some choppy water in the passage out of Bartlett Cove. Our on-board park ranger, Jenny, explained that the bottom of the ocean had striations in the sediment from the receding glacier that pushed the water up, often making it choppier than the wind would merit. After 45 minutes of cruising at 20 knots, our first stop along the way was at South Marble Island. This small island offers refuge to nesting Black-legged Kittiwakes, Tufted Puffins, and other colonial sea birds looking to nest away from predators. It also has huge haul-outs of Stellars’s Sealions. The gigantic animals that I like to call “sea grizzlies” because of their immense size (up to 2,000 pounds), lay on the rocks in the sunshine like sausages. The dominant males sat with back arched and head erect. Their enormous size compared to the others around them made it easy to see why they were the boss.
Our boat cut through the water past South Marble Island, and we moved up the fjord. As we did, the mountains became more jagged and covered in snow. At the mouth of Glacier Bay most the mountains had been covered ice during the last glacial advance which rounded them off over time, but the terrain became more jagged as we moved past mountain tops untouched by the glaciers. An exception to the jagged mountains was the round, granite dome named “Gloomy Knob”. On that granite dome were well manicured lawns of grass with sporadic cottonwoods growing in the crevices. The lawns were kept short by overwintering Mountain Goats who grazed the pastures. Just after the spring thaw is the best time to watch the goats, and I think we counted 20 of them on Gloomy Knob. Many of them were feeding their kids, and we got some insight into the bonding of goats with their mothers – one made a spectacle by climbing onto its mothers back.
The goats were not the only four-legged mammals on Gloomy Knob. High up in the granite cliffs we spotted a family of four Coastal Brown Bears. They lounged on the rocks, sleeping, perhaps 1,000 feet above our heads. During our passing they roused and moved along the ridgeline. They even passed by a goat on the ledge below them. Although the grizzlies took a look at their potential meal, the Mountain Goat seemed to know it was safe from the predators above, as it never moved a muscle.
Tidewater Glaciers
Sixty-five miles from where we started in Bartlett Cove we finally reached the end of the park. Marjorie Glacier stood in front of us like icy walls. The glacier face is about 350 feet tall and extends nearly a mile from left to right. In many of the pictures, you can see pin-sized Harbor Seals with their pups on the ice flows to lend the glacier some size perspective. Two times the glacier let go of new ice bergs by “calving”. The roar was like thunder of an approaching storm. The glacier, which is currently 21 miles long, has retracted 65 miles. In 1750, it was responsible for pushing the Huna Tlingit from their homeland. Since the retreat has happened so quickly, there are many studies within the park boundaries to understand how recolonization of rock surfaces occurs. Also, the land around the glacier is springing back up from the weight of the ice in a process known as isostatic rebound. The land rises almost an inch a year which may cause river drainages to change and coast resources like clam beds to come out of the water.
The students gave the whole boat a treat by performing traditional Tlingit songs at the glacier. Their pounding drums mixed with the grandeur of the scenery for a truly memorable end to the day. The trip into Glacier Bay was an incredible introduction to this vast and wild park. I look forward to the day when I return for a more detailed look at its beauty.
Glaciers carry the earth in their walls and as they melt create new land. As I stepped into Mendenhall Glacier, the world trapped within was immediately evident. Far into the ice, large boulders and sheets of sediment could be seen within. The rocks were distorted by the curves of the ice face. At the base of the cave’s walls, ice flowed over rocks that were half in and half out of their century-old entrapment. The whole floor of the glacier was made from the boulders that melted from glacier. These boulders, it seems, are released at a rapid rate, as the glacier 
