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

At the head of Tarr Inlet, two tidewater glaciers dominate the view: Margerie Glacier, whose bright blue calving face actively sheds icebergs into the fjord, and Grand Pacific, now a receded shadow of its former self, heavily buried under its own debris. Harbor seals dot ice floes, and black-legged kittiwakes wheel overhead as meltwater turns the inlet a milky blue-green. The inlet itself was carved by one massive glacier that advanced all the way to Icy Strait hundreds of years ago. Named by John Muir for the main glacier, the inlet was renamed in 1911 to honor Cornell geographer Ralph Stockman Tarr, who studied its fjord in the early 20th century.
Tidewater Glacier
Commercial tour vessel access only
Margerie Glacier (active tidewater glacier with calving face), Grand Pacific Glacier (receded, heavily debris-covered), tidewater fjord, harbor seals on ice floes, seabird colonies
Bright blue glacier ice actively calving into the fjord, harbor seals hauled out on ice chunks, black-legged kittiwakes and herring gulls in flight, puffins in the water, milky blue-green meltwater, massive debris-laden glacier terminus
Furthest navigable point into Glacier Bay, showcasing active tidewater glacier dynamics. Dramatic contrast between Margerie (actively advancing and calving) and Grand Pacific (heavily retreated). Named by John Muir; inlet renamed in 1911 for geographer Ralph Stockman Tarr. Part of UNESCO World Heritage Site.
Late June through mid-August. Warmest weather, longest days, most reliable tour vessel operations, and frequent glacier calving in afternoon light.
Glacial calving is unpredictable; vessel maintains safe distance (typically 0.5–1.0 mile). Water temperature approximately 40°F; hypothermia risk if immersed. Respect 100-yard bear distance and 25-yard seal distance. Weather can change rapidly; fog, wind, and rain are frequent. Wave action from calving events can shake the vessel.
Furthest navigable point into Glacier Bay, showcasing active tidewater glacier dynamics. Dramatic contrast between Margerie (actively advancing and calving) and Grand Pacific (heavily retreated). Named by John Muir; inlet renamed in 1911 for geographer Ralph Stockman Tarr. Part of UNESCO World Heritage Site.
Tidewater glacier dynamics and rapid retreat as climate indicator, glacial striations and ice-rock interactions, harbor seal ecology on glacial ice, seabird colonies, Holocene isostatic rebound and fjord evolution
Fly or ferry to Gustavus, Alaska. From Gustavus, board a commercial tour boat at Bartlett Cove (9 miles south of town). Tours depart daily during peak season and take 8–10 hours round-trip to reach Tarr Inlet.
None (boat-based destination only)
None (boat access only)
Bow and railings of commercial tour vessel during approach to glacier face
Margerie Glacier calving events in afternoon light, harbor seals on ice floes, seabirds against glacier backdrop, glacial ice formations and bergy bits, wide-angle fjord vistas from vessel deck
Bow of vessel for glacier approach shots, port and starboard railings for seal and bird photography, stern for wide-angle fjord vistas
Harbor seals, black-legged kittiwakes, herring gulls, glaucous-winged gulls, tufted puffins, occasional sea otters and humpback whales
Frequent fog, afternoon winds, rapid weather changes, and high precipitation. Storms can delay or cancel tours. Bring rain gear and prepare for cold, damp conditions.
Margerie Glacier, Grand Pacific Glacier, Johns Hopkins Inlet, Lamplugh Glacier, Geikie Inlet, Bartlett Cove, Beardslee Islands
Gustavus, Alaska (basic lodging, restaurants, outfitters); Juneau (full services); tour operators headquartered in Juneau
Commercial tour vessels have standard maritime deck and cabin access. Persons with mobility limitations should contact tour operators in advance to discuss accessibility accommodations and available assistance.
Suitable for all ages if family members can board a vessel and tolerate extended boat time (8–10 hours). Motion sickness is common in rough waters; bring medication. Weather is cold; dress in layers. Children must be supervised on deck at all times due to open railings and proximity to water.
Bartlett Cove (ranger station, dock, primitive campground 9 miles from Gustavus); Gustavus (limited lodging, fuel, restaurants); full services in Juneau
To Park Entrance
By boat from Gustavus: approximately 30 miles (8–10 hours via commercial tour vessel)
" Visitors consistently cite glacier views and wildlife as highlights. Long tour duration (8–10 hours) and motion sickness risk are common drawbacks. Weather delays are frequent and unavoidable. Most visitors agree the experience justifies the logistical challenges and cost."
Yes. The inlet is accessible only by boat. Commercial tours from Gustavus are the standard; private kayak expeditions require permits and significant backcountry experience.
Margerie Glacier calves regularly, especially in warm afternoons, but calving is never guaranteed. Grand Pacific rarely produces visible calving events. You will see both glaciers; dramatic calving is common but not certain.
Yes. It is glacial flour—fine silt particles suspended in meltwater that scatter light, creating the characteristic milky blue color. Not paint, not algae, not dye.
Motion sickness is common, especially on the approach to the inlet. Take motion-sickness medication pre-emptively, stay on deck for fresh air, and avoid reading or screen time below deck. Some rough days will be rough.
Tour vessels maintain a safe distance (typically 0.5–1.0 mile) to avoid waves and ice debris generated by calving events. This distance is both mandatory for safety and protective of the ecosystem.
Harbor seals on ice are nearly certain. Seabirds (kittiwakes, gulls, puffins) are common. Bears are possible but rare. Whales are seasonal. Bring binoculars to see details.
Margerie is actively advancing and calving, fed by snow from high-elevation sources. Grand Pacific is heavily retreated and debris-covered, buried under moraine and outwash from the Ferris Glacier feeding into it. Both are products of the same fjord-carving glacier; they simply are at different stages of decline.
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