Loch Ness Monster
Author Rai Radiotelevisione Italiana
Loch Ness Monster – The Loch Ness Monster is a cryptid – a creature whose existence has been suggested but is not recognized by scientific consensus. Nessie, is reputedly a large unknown animal that is said to inhabit Loch Ness in the Scottish Highlands. It is similar to other supposed lake monsters in Scotland and elsewhere, though its description varies from one account to the next. Popular interest and belief in the animal’s existence has varied since it was first brought to the world’s attention in 1933. Evidence of its existence is anecdotal, with minimal and much-disputed photographic material and sonar readings.
The most common speculation among believers is that the creature represents a line of long-surviving plesiosaurs. The scientific community regards the Loch Ness Monster as a modern-day myth and explains sightings as including misidentifications of more mundane objects, outright hoaxes, and wishful thinking. Despite this, she remains one of the most famous examples of cryptozoology. The legendary monster has been affectionately referred to by the nickname Nessie since the 1950s.
Carvings of this unidentified animal, made by the ancient inhabitants of the Scottish Highlands some 1,500 years ago, are the earliest evidence that Loch Ness harbors a strange aquatic creature. Most Nessie witnesses describe something with two humps, a tail, and a snakelike head. A V-shaped was often mentioned, as well as a gaping red mouth and horns or antennae on the top of the creature’s head. Nessie’s movements have been studied, and the films and photos analyzed to determine what Nessie might be, if she exists.
Loch Ness is located in the North of Scotland and is one of a series of interlinked lochs which run along the Great Glen. The Great Glen is a distinctive incision which runs across the country and represents a large geological fault zone. The interlinking was completed in the 19th century following the completion of the Caledonian Canal.
The Great Glen is more than 700 ft (213 m) deep and ice free. It is fed by the Oich and other streams and drained by the Ness to the Moray Firth. It forms part of the Caledonian Canal. By volume, Loch Ness is the largest freshwater lake in Great Britain.
History
Pre-History
The sedimentary rocks which cradle Loch Ness are some of the oldest in the world. The sandstones were originally laid down in warm seas which then comprised Scotland. You would not have recognized the land masses at that time and, surprisingly, Scotland was probably located in the latitude where Australasia exists today.
As part of continental drift the continents very slowly drifted northwards as Scotland became squeezed into the dry center of the super-continent Pangaea. By this time, 250 million years ago, the Great Glen side slip fault, which is home to Lochs Ness, Oich, Lochy and Linnhe, had already been created.
As Scotland crossed the equator it was the time of the dinosaurs and then as the continents began to break up and cluster around the north pole, the great ice ages began. Scottish mountains, which would have been Himalayan in size were gradually worn down to the stumps which you see today.
Scotland was still in the grip of the ice twelve thousand years ago, but the main advances were over, and the land was beginning to rebound from being depressed into the mantle. The surface of Loch Ness would have been at a similar elevation to sea level, but detailed and thorough examination of the sediments at the northwest end of the loch show no evidence for any incursion of the sea since the last ice age.
Anything living in Loch Ness today must have arrived from the freezing North Sea up the River Ness after the final retreat of ice, ten to twelve thousand years ago. This automatically eliminates certain Loch Ness monster candidates, primarily the reptiles, amphibians and invertebrates.
Today, without the weight of ice, the land has risen, and the surface of the loch would naturally stand at about 42 feet (12.8m) above sea level, but during the building of the Caledonian Canal, completed 1822, Telford built a weir at Loch Doc four SATPIC 1 raising the level of the loch by 9 feet (3m) and saving the necessity for a lot more excavation to make that area navigable. The mean height of the surface of the loch above sea level is now taken as 51 feet (15.5m) although in recent years the wetter winters may have increased the mean somewhat.
When the ice retreated the area would have been an extremely barren landscape. It may be hard to imagine the lack of trees, or even grass, rainfall washing deposits off the hills into the loch. Gradually wind-blown seeds would have introduced vegetation, the first trees being the silver birch which is still here in huge numbers. As part of the Loch Ness Project’s Rosetta Project an examination of the sediments has shown that silver birch pollen existed here just after the retreat of ice. Once you have a few grasses and trees the birds and animals would have begun to enter the new habitat. They would bring berries and heavier seeds thus continuing the movement of the Caledonian Forest northwards.
Throughout this period the heavier wind-blown seeds like sycamore and ash would have been carried northwards until the Highlands mixed forest was established.
While the loch would gradually become populated with cold-water fish, the land saw a far greater variety of life including wolves, bears, beavers and elk – all extinct here now, although the last wolf in the area was only shot in the nineteenth century. That wolf was known as Altsaigh SATPIC 22 and the name is still used for the burn (stream) which enters the loch from the northern side halfway along its length. It was here that Altsaigh was killed.
Mankind entered the Great Glen following the animals. The Picts left their mark throughout the glen. Gradually they were superseded by the Scots who had come across from Scotia (Ireland) around the sixth century, although the “amalgamation” appears to have been relatively peaceful. Certainly, there is no implication that the Scots conquered the Picts as they were outnumbered by around 20 to 1. Even today the Picts/Celts represent a major part of the Scottish population.
At the beginning of the last millennium the Scots elected their kings, and this was the time of Kenneth, Duncan and Macbeth. Interestingly it was a Scottish King, James VI who also became king of England when Elizabeth Tudor died and he unified the countries, conveniently handing Scotland to England on a plate when he moved his court south when becoming James I of England.
Today many of us are looking for Scotland to become an independent nation within the European community and, in 1997, a measure of devolution occurred with the creation of the Scottish Parliament.
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Loch Ness Monster
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