Natural AttractionStickeen – Dogs of the NPS
Dog crosses glacier crevasse with John Muir, 1880. A historical account of ice, fear, and unexpected bravery.

From the water, Russell Island reads as a green, forested rise set against a large U-shaped valley in the mountains beyond — hard to square with what John Muir saw here in 1879, when the island was a bare rocky hummock emerging from the face of the retreating glacier. Its entire forest has grown up in the years since, a plant-succession clock running in real time. The island is still responding to the ice, too: pressed into the mantle under thousands of feet of Little Ice Age ice, the land here is now rising about 32 mm (1.26 inches) per year through isostatic rebound — the fastest in the world. Scan the broad, open alluvial fan on the eastern shore as you pass; wildlife regularly patrols it.
Island
Boat-based viewing
Recently deglaciated bedrock island, now covered in vegetation; a broad, open alluvial fan on the eastern shore; measurable isostatic rebound of about 32 mm (1.26 inches) per year.
A forested island set before a large U-shaped valley in the mountains beyond, and the open alluvial fan of the eastern shore, where wildlife regularly patrols.
Under thousands of feet of ice during the Little Ice Age, the landscape here is now rising about 32 mm (1.26 inches) annually — the fastest isostatic uplift in the world.
The main visitor season runs late May through early September, with July the peak month; park services are extremely limited outside that window.
Wildlife rules apply from the water: keep at least 100 yards from bears and wolves and 25 yards from other wildlife. There are no visitor facilities listed for the island — plan around your vessel, not the shore.
Under thousands of feet of ice during the Little Ice Age, the landscape here is now rising about 32 mm (1.26 inches) annually — the fastest isostatic uplift in the world.
The fastest measured isostatic rebound in the world — about 32 mm (1.26 inches) of uplift per year — plus a natural laboratory for plant succession: the island has hosted scientific research for over 100 years.
Viewed from the water. Vessels travel the narrow channel between Russell Island and the mainland; there is no road access listed for this site.
From the water in the narrow channel between the island and the mainland, with the eastern shore's alluvial fan in view.
The island framed against the large U-shaped valley behind it; the contrast between the young forest and the surrounding glacial terrain.
The channel between the island and the mainland, which frames Russell Island in front of the U-shaped valley beyond.
Wildlife regularly patrols the island's shores, especially the broad, open alluvial fan on the eastern side.
Viewed from vessels on the water; no developed visitor facilities are listed for the island itself.
Viewing is from the water, so it works for any age — binoculars help kids pick out wildlife on the eastern shore's open fan.
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Because in 1879 it wasn't one. When John Muir came through, this was bare rock emerging from the face of the retreating glacier. You're looking at roughly 150 years of plant succession from zero, on land that is still rising 1.26 inches a year.
No guarantees, but wildlife regularly patrols the island's shores — the broad, open alluvial fan on the eastern side is the stretch to scan as you pass through the channel.
It's real and measured: upper Glacier Bay is rising about 32 mm (1.26 inches) per year — the fastest isostatic uplift in the world. The crust was pressed into the mantle under thousands of feet of Little Ice Age ice and is still springing back.
Glacier Bay National Park charges no entrance fee and has no entrance gates — the island is viewed from the water as you travel the bay.
Park rules: at least 100 yards from bears and wolves, and at least 25 yards from other wildlife. Judge the distance from your vessel before you close in for a look.
No — the island was named in 1937 for explorer Israel Cook Russell, who worked in the Yakutat region in the early 1890s. It was John Muir who saw it emerging from the ice in 1879 and 1880.
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