Gros Morne National Park

Gros Morne National Park is a large protected landscape on the west coast of Newfoundland, Canada, recognised as a UNESCO World Heritage site for its geological features and natural diversity. The park covers a rugged area of mountains, fjords, coastal lowlands and glacial valleys.

Key attractions include the dramatic fjord of Western Brook Pond, the steep bulk of Gros Morne Mountain and the distinctive Tablelands where exposed mantle rock provides visible evidence of ancient plate boundary processes. Hiking, boat tours and coastal drives are primary visitor activities that showcase the park’s geological and scenic features. Wildlife viewing includes moose and a range of coastal and forest species.

The park’s geological formations illustrate continental drift and the collision and uplift of ancient oceanic crust, and research and interpretation focus on these features. Conservation and visitor infrastructure balance public access with protection of sensitive habitats and geological sites.

Gros Morne is located on the island of Newfoundland’s west coast near the town of Rocky Harbour; the park occupies a coastal and mountainous landscape facing the Gulf of St. Lawrence.

• Seasonal access: Boat excursions on Western Brook Pond and guided hikes up Gros Morne Mountain are seasonal and often subject to weather conditions; check local operators for availability.
• Geological significance: The park is recognised for its geology that displays uplifted oceanic crust and evidence relevant to plate tectonics, drawing both scientific and recreational interest.

What to See #

• Western Brook Pond: A dramatic inland freshwater fjord formed by glacial action, accessible by hiking and boat tours and noted for its still waters and steep cliffs.
• Gros Morne Mountain: The highest peak in the park and a steep granite mountain that is a popular but challenging hike offering wide-ranging views over the park.
• Tablelands: An area of exposed mantle rock known as the Tablelands, notable for its sparse vegetation and significance to geological interpretation of plate tectonics.