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The Great Britain Guide

Public art & sculpture · London

The Barrier

Free admission

The Barrier — a public art in england-london, United Kingdom.

Ex-LSWR 4-4-0 at Nine Elms Locomotive Depot - geograph.org.uk - 2976376

Ben Brooksbank — CC BY-SA 2.0 via Wikimedia Commons licence

Plan your visit

Typical visit
1 h–2 h
  • Free entry
  • Dog-friendly

About

The Barrier is a public art located in england-london, United Kingdom. Sourced from OpenStreetMap (ODbL licence); see local listings for visitor information, opening hours and admission details.

Photo gallery

From the Wikipedia article

The Barrier is a lava dam retaining the Garibaldi Lake system in southwestern British Columbia, Canada. It is about 80 kilometres (50 miles) north of Vancouver in Garibaldi Provincial Park of New Westminster Land District. The Barrier lies in the Cheakamus River watershed of the southern Coast Mountains where snow-capped mountains, diverse vegetation and rich geological history exist. Garibaldi Lake is the largest lake impounded by The Barrier; it has a length of 5.23 km (3.25 mi) and a width of 2.4 km (1.5 mi). The much smaller Lesser Garibaldi and Barrier lakes are also impounded by The Barrier. However, they lie within depressions on the surface of the lava dam rather than behind it. All three lakes are drained by Rubble Creek, a tributary of the Cheakamus River flowing northwest from the foot of The Barrier. The Barrier formed about 13,000 years ago when lava flowed into Rubble Creek valley. It then ponded and cooled against the retreating Cordilleran Ice Sheet, resulting in the lava flow being unusually thick. The source of the lava flow was Clinker Peak on the western shoulder of Mount Price, a stratovolcano reaching an elevation of 2,049 metres (6,722 feet). In 1855–1856, The Barrier was the source of a large rock avalanche that travelled down Rubble Creek valley to the Cheakamus River. This collapse of the lava dam created its current headwall; it rises about 500 m (1,600 ft) above the floor of Rubble Creek valley. The headwall has been highly unstable since the 1855–1856 landslide, having been the site of several rockfalls. Debris from these rockfalls has formed a talus deposit at the base of the headwall. Concerns about The Barrier's instability prompted the provincial government to declare the area immediately below it unsafe for human habitation in 1980–1981. This led to the evacuation of the small resort village of Garibaldi nearby and the relocation of residents to new recreational subdivisions away from the hazard zone. As of 2025, The Barrier merits consideration in future volcanic hazard assessments. This is particularly due to the presence of Garibaldi Lake, which would be released catastrophically if the lava dam were to ever give out.

Excerpt from Wikipedia under CC BY-SA 4.0. See the source article linked in Sources below.

Background

History

The Barrier is part of the Mount Price volcanic complex, which also includes the 2049 m high stratovolcano of Mount Price and the 1983 m high stratovolcano of Clinker Peak on the western shoulder of Mount Price. This complex was formed by the eruption of lavas and pyroclastic flows during three periods of volcanic activity in the last 1.2 million years; the lavas and pyroclastic flows are andesitic and dacitic in composition. The Mount Price complex is the oldest eruptive centre in the Garibaldi Lake volcanic field, which also includes Cinder Cone, The Black Tusk and The Table. Volcanism throughout the Garibaldi Lake volcanic field has produced a broader range of volcanic rocks; among them…

Architecture

area showing the location of The Barrier]] The Barrier formed about 13,000 years ago when the Cordilleran Ice Sheet had retreated from higher elevations but still existed in lower valleys. During this time, an andesite lava flow was erupted from Clinker Peak and then entered Rubble Creek valley for 1.5 mi where it ponded against the ice. The Barrier, which has a width of 0.5 mi and a thickness of at least 250 m at its headwall, consists of unusually thick andesite lava as a result of this impoundment. Pseudo-pillow joints and irregular, radiating and horizontal columnar joints are present in The Barrier; they are indicative of lava cooling against ice. The andesite comprising The Barrier is…

Visiting

Daisy Lake Road, 30 km north of Squamish, provides access to The Barrier from Highway 99. At the end of this 2.5 km long road is the Rubble Creek parking lot, from which the 7.5 km long Garibaldi Lake Trail begins. This graded hiking trail switchbacks more than 20 times as it climbs 770 m up the northern side of Rubble Creek valley. About 6 km down the trail is a junction with the Taylor Meadows route; the right fork leads to Garibaldi Lake. A short distance beyond this junction is another route that branches off the Garibaldi Lake Trail; this branch leads to The Barrier viewpoint. The Barrier cannot be accessed using snowmobiles, motorcycles, trail bikes, aircraft or all-terrain vehicles…

Sourced from Wikipedia under CC BY-SA 4.0.

Coordinates
51.4748, -0.1365
District
Wandsworth
Parish
Wandsworth, unparished area
Postcode
SW8 4HX
Parliamentary constituency
Battersea

Sources

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Frequently asked questions

Where is The Barrier?
The Barrier is in London, United Kingdom (postcode SW8 4HX), in the parish of Wandsworth, unparished area.
Is The Barrier free to visit?
Yes, The Barrier is free to enter.
How do I get to The Barrier?
Drivers can navigate to postcode SW8 4HX. It sits within the Battersea parliamentary constituency.