Loch Con | |
---|---|
Location | NN68776792 |
Coordinates | 56°47′04″N4°09′05″W / 56.784400°N 4.151484°W Coordinates: 56°47′04″N4°09′05″W / 56.784400°N 4.151484°W |
Type | freshwater loch |
Primary outflows | Allt Con |
Max. length | 1.3 km (0.81 mi) |
Max. width | 0.4 km (0.25 mi) |
Surface area | 25 ha (62 acres) [1] |
Average depth | 3.6 ft (1.1 m) [1] |
Max. depth | 8.8 ft (2.7 m) [1] |
Water volume | 9,505,016 cu ft (269,152.1 m3) [1] |
Shore length1 | 5 km (3.1 mi) [1] |
Surface elevation | 413 m (1,355 ft) [1] |
Islands | 0 |
1 Shore length is not a well-defined measure. |
Loch Con is a small, remote, shallow, irregular shaped freshwater loch that is located in Glen Errochty in the Perth and Kinross council area, at the edge of the Scottish Highlands. [1] [2] It is directly north of Loch Errochty. Directly north of the loch at the east end is Loch Cruinn. It is the source of the Allt Con, which flows a short distance southwards past Sròn Choin to Loch Errochty. [2] At the north-east end is Loch Cruinn, a very small dam, about 100 metres wide.
Perthshire, officially the County of Perth, is a historic county and registration county in central Scotland. Geographically it extends from Strathmore in the east, to the Pass of Drumochter in the north, Rannoch Moor and Ben Lui in the west, and Aberfoyle in the south; it borders the counties of Inverness-shire and Aberdeenshire to the north, Angus to the east, Fife, Kinross-shire, Clackmannanshire, Stirlingshire and Dunbartonshire to the south and Argyllshire to the west. It was a local government county from 1890 to 1930.
Sutherland is a historic county, registration county and lieutenancy area in the Highlands of Scotland. Its county town is Dornoch. Sutherland borders Caithness and Moray Firth to the east, Ross-shire and Cromartyshire to the south and the Atlantic to the north and west. Like its southern neighbour Ross-shire, Sutherland has some of the most dramatic scenery in the whole of Europe, especially on its western fringe where the mountains meet the sea. These include high sea cliffs, and very old mountains composed of Precambrian and Cambrian rocks.
The Stirling council area is one of the 32 council areas of Scotland, and has a population of about 94,330. It was created under the Local Government etc (Scotland) Act 1994 with the boundaries of the Stirling district of the former Central local government region, and it covers most of Stirlingshire and the south-western portion of Perthshire. Both counties were abolished for local government purposes under the Local Government (Scotland) Act 1973.
Loch Leven is a sea loch located on the west coast of Scotland. It is spelled Loch Lyon in Timothy Pont's map of the area and is pronounced Li' un. The local Gaelic pronunciation is Lee' oon
Loch Lubnaig is a small freshwater loch near Callander in the Stirling council area, Scottish Highlands. It lies in the former county of Perthshire. It is part of the Loch Lomond and The Trossachs National Park.
The Trossachs generally refers to an area of wooded glens, braes, and lochs lying to the east of Ben Lomond in the Stirling council area of Scotland. The name is taken from that of a small woodland glen that lies at the centre of the area, but is now generally applied to the wider region.
Loch Shiel is a freshwater loch situated 20 kilometres (12 mi) west of Fort William in the Highland council area of Scotland. At 28 kilometres long it is the 4th longest loch in Scotland, and is the longest to have retained a natural outflow without any regulation of its water level, being 120 m (393 ft) deep. Its nature changes considerably along its length, being deep and enclosed by mountains in the north east and shallow surrounded by bog and rough pasture in the south west, from which end the 4 km River Shiel drains to the sea in Loch Moidart near Castle Tioram.
The Southern Uplands are the southernmost and least populous of mainland Scotland's three major geographic areas. The term is used both to describe the geographical region and to collectively denote the various ranges of hills and mountains within this region. An overwhelmingly rural and agricultural region, the Southern Uplands are partly forested and contain many areas of open moorland - the hill names in the area are congruent with these characteristics.
Brenton Loch is an inlet-cum-small fjord in the Falkland Islands. It is one of a handful of sea lochs outside Scotland. It is sometimes known as "Brenton Sound". "Loch" is normally pronounced as "lock" in the English rather than Scottish manner, i.e. without a fricative "ch". The far south of the loch is known as "La Boca" or "The Boca".
Loch Errochty is a man made freshwater loch situated within the Perth and Kinross council area at the edge of the Scottish Highlands near the Highland Boundary Fault where the topography changes to lowland.
Beinn a' Chuallaich is a Scottish hill, four kilometres northeast of the village of Kinloch Rannoch in the Perth and Kinross council area. It is part of the high ground between Strath Tummel and Glen Errochty.
Loch Ness is a large freshwater loch in the Scottish Highlands extending for approximately 37 kilometres southwest of Inverness. It is named for the River Ness, which flows from the northern end. Loch Ness is best known for alleged sightings of the cryptozoological Loch Ness Monster, also known affectionately as "Nessie". It is one of a series of interconnected, murky bodies of water in Scotland; its water visibility is exceptionally low due to a high peat content in the surrounding soil. The southern end connects to Loch Oich by the River Oich and a section of the Caledonian Canal. The northern end connects to Loch Dochfour via the River Ness, which then ultimately leads to the North Sea via the Moray Firth.
Loch Veyatie is a large body of water in north-west Scotland. It stretches for 6 km north-westwards from the settlement of Elphin, and lies between Suilven and Cùl Mòr. It reaches depths of around 30 m (98 ft).
Minginish is a peninsula on the Isle of Skye in Scotland. It is situated on the west coast of the island and runs from Loch Scavaig in the south, along the western coast of Skye to Loch Bracadale in the north west, to Loch Harport in the north east, and Glen Sligachan in the south east. It includes most of the peaks of the Cuillin hills including Sgurr Alasdair, the highest point on the island at 992 metres (3,255 ft). The island of Soay lies offshore across the Soay Sound, with the Small Isles further south across the Cuillin Sound.
The River Garry is a major tributary of the River Tummel, itself a tributary of the River Tay, in the traditional county of Perthshire in the Scottish Highlands. It emerges from the northeastern end of Loch Garry (56.8193°N 4.2311°W), just to the southeast of the Pass of Drumochter, and flows southeastwards and eastwards down Glen Garry to the narrow Pass of Killiecrankie beyond which it joins the Tummel (56.7182°N 3.7790°W).
Loch Sween is a sea loch located near Lochgilphead, Argyll and Bute, Scotland. Castle Sween is located on the southern shore towards the seaward end of the loch. The village of Tayvallich, a favoured haven for water craft as it sits at the head of sheltered Loch a' Bhealaich, lies on the northern shore.
Struan is a small village in Perthshire in Scotland. It is 8 km west of Blair Atholl.
Dun Cruinn is a prehistoric site about 10 kilometres (6.2 mi) north-west of Portree, on the Isle of Skye, Scotland. It is on the Skerinish Peninsula, between Loch Snizort Beag and Loch Eyre.
The geology of the Isle of Mull in Scotland is dominated by the development during the early Palaeogene period of a ‘volcanic central complex’ associated with the opening of the Atlantic Ocean. The bedrock of the larger part of the island is formed by basalt lava flows ascribed to the Mull Lava Group erupted onto a succession of Mesozoic sedimentary rocks during the Palaeocene epoch. Precambrian and Palaeozoic rocks occur at the island's margins. A number of distinct deposits and features such as raised beaches were formed during the Quaternary period.