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Loch Ness (/ ˌ l ɒ x ˈ n ɛ s /; Scottish Gaelic: Loch Nis [l̪ˠɔx ˈniʃ]) is a large freshwater loch in the Scottish Highlands extending for approximately 37 kilometres (23 miles) along the length of the Great Glen southwest of Inverness.
The Loch Ness Supergroup is one of the subdivisions of the Neoproterozoic sequence of sedimentary rocks (or their metamorphic equivalents) in the Scottish Highlands. [1] It is found everywhere in tectonic contact above the older Wester Ross Supergroup. It is thought to be unconformably overlain by the Cryogenian to Cambrian Dalradian Supergroup ...
The Loch Ness Monster (Scottish Gaelic: Uilebheist Loch Nis), [3] also known as Nessie, is a mythical creature in Scottish folklore that is said to inhabit Loch Ness in the Scottish Highlands. It is often described as large, long-necked, and with one or more humps protruding from the water.
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The most famous example is the Loch Ness Monster. Depictions of lake monsters are often similar to those of sea monsters. In the Motif-Index of Folk-Literature, entities classified as "lake monsters", such as the Scottish Loch Ness Monster, the American Chessie, and the Swedish Storsjöodjuret fall under B11.3.1.1. ("dragon lives in lake").
[2] [3] The volume of water in Loch Ness is nearly double that in all the lakes of England and Wales combined. [1] Murray and Pullar also note that the mean depth of Loch Ness is 57.4% of the maximum depth – higher than in any other large deep loch, with Loch Avich coming closest at 52.4%. [4]
Almost every sizeable Scottish body of water has a kelpie story associated with it, [11] [38] but the most widely reported is the kelpie of Loch Ness. Several stories of mythical spirits and monsters are attached to the loch's vicinity, dating back to 6th-century reports of Saint Columba defeating a monster on the banks of the River Ness. [45]
The Ballantrae Complex near Girvan was formed from this ocean floor and is similar in composition to rocks found at The Lizard in Cornwall. Nonetheless, northern and southern Britain were far apart at the beginning of this period, although the gap began to close as the continent of Avalonia broke away from Gondwana , collided with Baltica and ...