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Falls Of Lora
The Falls of Lora is a tidal race which forms at the mouth of Loch Etive when a particularly high tide runs out from the loch. They form white water rapids for two to five days either side of the spring tides."Falls of Lora Information" The Falls of Lora. Retrieved 18 Sept 2011. Description The falls of Lora are generated when the water level in the (i.e. the open sea) drops below the level of the water in as the tide goes out. As the seawater in |
Falls Of Lora - Geograph
Falls may refer to: Places * Waterfalls or rapids * Falls, North Carolina, USA * Falls, West Virginia, USA Other uses * The ropes or wires, fed through Davit, davits, that are used to secure and lower a ship's Lifeboat (shipboard), lifeboats. * Falls (surname) * The sepals of the Iris (plant)#Flower, Iris flower * Falls in older adults See also * Meteorite falls * Belfast Falls (other) ** Falls Road, Belfast in Belfast, Northern Ireland ** Belfast Falls (Northern Ireland Parliament constituency) ** Belfast Falls (UK Parliament constituency) * Falls Festival * Blood Falls, an outflow of an iron oxide tainted plume of melting salty water occurring at the Taylor Glacier in the McMurdo Dry Valleys in Antarctica * Falls Airport (other) * Falls City (other) * Falls Creek (other) * Falls River (other) * Falls Township (other) * The Falls (other) * Fall (other) * The Fall (other) * Falling (disambiguat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tidal Race
Tidal race or tidal rapid is a natural occurrence whereby a fast-moving tide passes through a constriction, resulting in the formation of waves, eddies and hazardous currents. The constriction can be a passage where the sides narrow, for example the Gulf of Corryvreckan and the Saltstraumen maelstrom, or an underwater obstruction (a reef or rising seabed), such as is found at the Portland Race in the United Kingdom. In extreme cases, such as Skookumchuck Narrows in British Columbia, through which tides can travel at more than 17 knots, very large whirlpools develop, which can be extremely hazardous to navigation. Notable tidal races * Cape Reinga in New Zealand * Skookumchuck Narrows in British Columbia, Canada * The Bitches in Wales, United Kingdom * |
Loch Etive
Loch Etive (Scottish Gaelic, ''Loch Eite'') is a 30 km sea loch in Argyll and Bute, Scotland. It reaches the sea at Connel, 5 km north of Oban. It measures 31.6 km (19 miles) long and from 1.2 km ( mile) to wide. Its depth varies greatly, up to a maximum of . The name ''Etive'' is believed to mean "little fierce one" from the Gaelic goddess associated with the loch. It heads east for half its length alongside the main road and rail link to Oban, before heading northeast into mountainous terrain. A road along Glen Etive makes the head of the loch accessible from Glen Coe. The narrow mouth of the loch results in its most unusual feature, the Falls of Lora. Part of the north bank has been designated a Special Area of Conservation in particular due to old sessile oak woods. A small colony of around 20 common seals is resident in Loch Etive. Just seaward of the mouth of the loch is Dunstaffnage Castle. This was a stronghold of the kingdom of Dál Riata ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spring Tide
Tides are the rise and fall of sea levels caused by the combined effects of the gravitational forces exerted by the Moon (and to a much lesser extent, the Sun) and are also caused by the Earth and Moon orbiting one another. Tide tables can be used for any given locale to find the predicted times and amplitude (or " tidal range"). The predictions are influenced by many factors including the alignment of the Sun and Moon, the phase and amplitude of the tide (pattern of tides in the deep ocean), the amphidromic systems of the oceans, and the shape of the coastline and near-shore bathymetry (see '' Timing''). They are however only predictions, the actual time and height of the tide is affected by wind and atmospheric pressure. Many shorelines experience semi-diurnal tides—two nearly equal high and low tides each day. Other locations have a diurnal tide—one high and low tide each day. A "mixed tide"—two uneven magnitude tides a day—is a third regular category. Tide ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Firth Of Lorn
The Firth of Lorn or Lorne ( gd, An Linne Latharnach) is the inlet of the sea between the south-east coast of the Isle of Mull and the mainland of Scotland. It includes a number of islands, and is noted for the variety of wildlife habitats that are found. In 2005, a large part of the Firth became a Special Area of Conservation. Geography and geology The firth extends from the junction of the Sound of Mull and the Lynn of Lorn in the north-east, in a south-westerly direction towards Colonsay. The narrower north-eastern part is the Inner Firth, and the wider south-western part is the Outer Firth. The firth takes its name from the historic province of Lorne on the adjacent mainland. The Firth of Lorn is a continuation of the Great Glen - the Great Glen Fault runs along the north-westerm side of the firth. A conspicuous feature of the coasts of the firth is the presence of rock platforms and raised cliffs. These can be seen on the coast of Mull, on the Island of Kerrera and o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rapids
Rapids are sections of a river where the river bed has a relatively steep gradient, causing an increase in water velocity and turbulence. Rapids are hydrological features between a ''run'' (a smoothly flowing part of a stream) and a ''cascade''. Rapids are characterized by the river becoming shallower with some rocks exposed above the flow surface. As flowing water splashes over and around the rocks, air bubbles become mixed in with it and portions of the surface acquire a white color, forming what is called "whitewater". Rapids occur where the bed material is highly resistant to the erosive power of the stream in comparison with the bed downstream of the rapids. Very young streams flowing across solid rock may be rapids for much of their length. Rapids cause water aeration of the stream or river, resulting in better water quality. Rapids are categorized in classes, generally running from I to VI. A Class 5 rapid may be categorized as Class 5.1-5.9. While Class I rapids are eas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
High Tide
Tides are the rise and fall of sea levels caused by the combined effects of the gravitational forces exerted by the Moon (and to a much lesser extent, the Sun) and are also caused by the Earth and Moon orbiting one another. Tide tables can be used for any given locale to find the predicted times and amplitude (or "tidal range"). The predictions are influenced by many factors including the alignment of the Sun and Moon, the phase and amplitude of the tide (pattern of tides in the deep ocean), the amphidromic systems of the oceans, and the shape of the coastline and near-shore bathymetry (see '' Timing''). They are however only predictions, the actual time and height of the tide is affected by wind and atmospheric pressure. Many shorelines experience semi-diurnal tides—two nearly equal high and low tides each day. Other locations have a diurnal tide—one high and low tide each day. A "mixed tide"—two uneven magnitude tides a day—is a third regular category. Tides va ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oban
Oban ( ; ' in Scottish Gaelic meaning ''The Little Bay'') is a resort town within the Argyll and Bute council area of Scotland. Despite its small size, it is the largest town between Helensburgh and Fort William. During the tourist season, the town can have a temporary population of up to over 24,000 people. Oban occupies a setting in the Firth of Lorn. The bay forms a near perfect horseshoe, protected by the island of Kerrera; and beyond Kerrera, the Isle of Mull. To the north, is the long low island of Lismore and the mountains of Morvern and Ardgour. Pre-history and archaeology Humans have used the site where Oban now stands since at least Mesolithic times, as evidenced by archaeological remains of cave dwellers found in the town. Just outside the town, stands Dunollie Castle, on a site that overlooks the main entrance to the bay and has been fortified since the Bronze Age. Just to the north of Oban, at Dunstaffnage, excavations in 2010, by Argyll Archaeology, in advanc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bonawe
Bonawe (; ) is a village in Ardchattan Parish Argyll and Bute, Scotland opposite Taynuilt on the north shore of Loch Etive, most famous for the shipping firm J & A Gardener's Bonawe Quarry - now owned by Breedon Aggregates Scotland Ltd (). Bonawe is primarily a linear settlement along on the B845 road and the coast. The iron furnace is at Bonawe in Glenorchy & Inishail Parish across Loch Etive nr Taynuilt in Muckairn Parish. Bonawe Quarry In the early 1900s there were 1,000 people living in Bonawe. The hub of this community was the Bonawe Quarry which still operates to this day. In those days there were stonemasons, drillers and miners extracting the stone and of course their families and support industries such as local shops, butchers, bowling greens, a cinema, bakeries and laundry. But now technology has advanced which means very few people are needed from the quarry and people can come from far to work, and as a result there are no shops left in Bonawe. Ardchattan Primary ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Connel Bridge
Connel Bridge is a cantilever bridge that spans Loch Etive at Connel in Scotland. The bridge takes the A828 road across the narrowest part of the loch, at the Falls of Lora. It is a category B listed structure. History The bridge was built by Arrol's Bridge and Roof Company to carry the Ballachulish branch line of the Callander and Oban Railway, which opened on 20 August 1903. Nearly of steel were used in its construction and it cost almost £43,000 to build. When complete it had a longer span than any other railway bridge in Britain except the Forth Bridge, built by a different firm. The Connel Bridge was constructed by a firm called Arrol, of the Germiston Iron Works, Glasgow It was engineered by John Wolfe Barry and others. Originally, the bridge carried just the railway (a single track). In 1909, however, an additional train service started running between Connel Ferry station and on which road vehicles could be transported over the bridge. A single car was ca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kayak
A kayak is a small, narrow watercraft which is typically propelled by means of a double-bladed paddle. The word kayak originates from the Greenlandic word ''qajaq'' (). The traditional kayak has a covered deck and one or more cockpits, each seating one paddler. The cockpit is sometimes covered by a spray deck that prevents the entry of water from waves or spray, differentiating the craft from a canoe. The spray deck makes it possible for suitably skilled kayakers to roll the kayak: that is, to capsize and right it without it filling with water or ejecting the paddler. ] Some modern boats vary considerably from a traditional design but still claim the title "kayak", for instance in eliminating the cockpit by seating the paddler on top of the boat ("sit-on-top" kayaks); having inflated air chambers surrounding the boat; replacing the single hull with twin hulls; and replacing paddles with other human-powered propulsion methods, such as foot-powered rotational propellers and "fli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
