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Sailing stones (also called sliding rocks, walking rocks, rolling stones, and moving rocks) are part of the geological phenomenon in which rocks move and inscribe long tracks along a smooth valley floor without animal intervention. The movement of the rocks occurs when large, thin sheets of ice floating on an ephemeral winter pond move and ...
The Giant's Causeway (Irish: Clochán an Aifir) [1] is an area of approximately 40,000 interlocking basalt columns, the result of an ancient volcanic fissure eruption. [3] [4] It is located in County Antrim on the north coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills.
Flagstone is a sedimentary rock that is split into layers along bedding planes. Flagstone is usually a form of a sandstone composed of feldspar and quartz and is arenaceous in grain size (0.16 mm – 2 mm in diameter). The material that binds flagstone is usually composed of silica, calcite, or iron oxide. The rock color usually comes from ...
The walkway is 1 metre (3 ft) in width and rises over 100 metres (330 ft) above the river below. Traversing a collapsed section in 2006. The original path was constructed of concrete and rested on steel rails supported by stanchions built at approximately 45 degrees into the rock face.
The Cape to Cape Track passes near the lookout over the rocks. [1] Facilities at the site include a car park, boat ramp, finger jetty and a walkway to access the closest rock formation. [1] A small, unpatrolled 200-metre-long (656 ft) beach is found to the lee-side of the rocks with low to subtidal sand and patchy rock reefs. [5]
Plants are a natural choice for walkway borders whether the swooping line of a tightly shorn boxwood leading to a dramatic sea view or the soft edge of hostas on the charming path to a poolside ...
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