Lamplugh Glacier

Lamplugh Glacier

Natural Attr
Last Updated: July 2026

Type

Tidewater Glacier

Accessibility

Boat access only; no hiking required from vessel viewpoint; viewing from boat deck

Best Season

Late May–early September; peak activity and services July

Busiest Season

July peak season; expect most tour boats, cruise ship excursions, and visitor congestion on boats.

Features

Calving tidewater glacier descending from Brady Icefield; active subglacial stream discharge creating milky fjord plume; subglacial cave mouths in ice face; 120-million-ton rock debris from 2015 landslide visible on glacier surface; outwash mudflats (formed 2010–present); grounded western terminus.

Overview

About This Attraction

Lamplugh's ice face rises from an embayment of milky turquoise water, studded with subglacial cave mouths where freshwater floods into the sea with enough force to reshape fjord sediments. The glacier descends from Brady Icefield, its surface buried in 120 million tons of rock from a 2015 landslide—a burden that internally redirected meltwater flow and visibly altered ice dynamics. Retreating at 50–100 feet annually, Lamplugh's outwash mudflats now host moose, bears, and marmots traversing the pioneering tundra.

Quick Facts

Type

Tidewater Glacier

Access

Boat access only; no hiking required from vessel viewpoint; viewing from boat deck

Main Features

Calving tidewater glacier descending from Brady Icefield; active subglacial stream discharge creating milky fjord plume; subglacial cave mouths in ice face; 120-million-ton rock debris from 2015 landslide visible on glacier surface; outwash mudflats (formed 2010–present); grounded western terminus.

What You'll See

Massive ice face with active calving events producing house-sized ice blocks; milky discharge plume from subglacial stream extending miles into fjord; subglacial cave mouths and ice cliff detail; Fairweather Range peaks (clear weather); recently exposed outwash terrain with pioneer vegetation; browsing moose, bears, or marmots on forelands; humpback whales in adjacent waters (summer).

What Makes It Special

Rapid retreat rate (50–100 feet per year) visible across visits; 2015 massive landslide fundamentally altered glacier hydrology and ice flow mechanics; active subglacial sediment discharge visibly building fjord mudflats in real time; one of most accessible tidewater glaciers in Alaska for observation of dynamic glacial processes.

Best Time to Visit

Late May–early September for boat access and guided tours; peak activity July with midnight sun. Morning visits (4–6 AM) offer clearest light and ice detail; afternoon fog common. Early May and September provide fewer crowds and dramatic low-sun angles.

Safety Considerations

CALVING ICE: Falling blocks (often exceeding house-size) and surge waves—maintain minimum 0.5 mile distance; listen for audible fractures as warning. BEARS: 100-yard minimum separation; use binoculars for scanning. COLD WATER: Hypothermia risk if immersed; wear layered, waterproof clothing. TIDAL: Western third of terminus grounded at low tide; tidal range affects visible ice face and mudflat exposure.

Visitor Tips

  • Listen for low-frequency rumbling—calving events produce audible fractures seconds before ice falls; maintain 0.5+ mile boat distance
  • Watch the subglacial discharge plume (milky blue/tan water) for visible sediment transport and glacier hydrology dynamics
  • Stay 100 yards minimum from bears; scan outwash mudflats with binoculars for moose, bears, and marmots
  • Early morning offers clearest light for ice cliff detail photography; afternoon develops fog and cloud cover
  • Tides expose the grounded western terminus—check tide tables before departure for optimal viewing
ℹ️ Data Sources
🏞️ National Park Service 📝 YourNPGuide Editorial

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