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Waterfalls are sometimes interchangeably referred to as "cascades" and "cataracts", though some sources specify a cataract as being a larger and more powerful waterfall [1] [4] [5] and a cascade as being smaller. [6] A plunge pool is a type of stream pool formed at the bottom of a waterfall. [7] A waterfall may also be referred to as a "foss ...
The falls form when seawater rushes through two short and narrow gorges which are about 300 metres (1,000 ft) apart from each other. They are located in the coastal McLarty Ranges situated within Talbot Bay (Ganbadba) within the Buccaneer Archipelago. The seaward gap is about 20 metres (70 ft) wide and the landward one is about 10 metres (30 ft).
Waterfall Bay (Tasmania, Australia) [11] King George River, (Western Australia) New Zealand: the following waterfalls empty into fjords of the Tasman Sea: into Doubtful Sound - Chamberlain Falls, Helena Falls, Lady Alice Falls. into Milford Sound - Bowen Falls, Stirling Falls. Samoa: Mu Pagoa Waterfall in the Palauli District on Savaii:
A plunge pool (or plunge basin or waterfall lake) is a deep depression in a stream bed at the base of a waterfall or shut-in. It is created by the erosional forces of cascading water on the rocks at the formation's base where the water impacts. [1] The term may refer to the water occupying the depression, or the depression itself. [2]
This is an accepted version of this page This is the latest accepted revision, reviewed on 7 February 2025. Waterfalls between United States and Canada This article is about the waterfalls on the Canada–United States border. For other uses, see Niagara Falls (disambiguation). Niagara Falls Niagara Falls seen from the Canadian side of the river, including three individual falls (from left to ...
Such waterfalls are described by geologists as "a living phenomenon" because they are continuously rebuilt by the sediments in spring water. [3] Dunn's River Falls is one of the very few travertine waterfalls in the world that empties directly into the sea. [3]
A sinkhole was discovered at on Wednesday evening near the base of Ocean City's Isle of Wight Bay Bridge, Route 90. Here's what caused it, plus more.
Often, waterfalls form at or near the outlet of the upper valley. [7] Hanging valleys also occur in fjord systems underwater. The branches of Sognefjord are much shallower than the main fjord. The mouth of Fjærlandsfjord is about 400 meters (1,300 ft) deep while the main fjord nearby is 1,200 meters (3,900 ft) deep.