Geography of the Isle of Man
|Ellan Vannin (Manx)|
Topographic map of the Isle of Man
|Adjacent bodies of water||Irish Sea|
|Area||572 km2 (221 sq mi)|
|Coastline||160 km (99 mi)|
|Highest elevation||621 m (2,037 ft)|
|Largest town||Douglas (pop. 23,000)|
|Pop. density||139.52 /km2 (361.36 /sq mi)|
The Isle of Man is an island in the Irish Sea, between Great Britain and Ireland in Western Europe, with a population of almost 85,000. It is a British Crown dependency. It has a small islet, the Calf of Man, to its south. It is located at .
- 1 Dimensions
- 2 Coast and Territorial Sea
- 3 Climate
- 4 Terrain
- 5 Land use
- 6 Natural hazards and environmental issues
- 6.1 Protected sites for nature conservation
- 7 Geology
- 8 Demographics
- 9 See also
- 10 Citations
- 11 References
total: 572 km2 (221 sq mi)
land: 571 km2 (220 sq mi)
water: 1 km2 (0.4 sq mi)
This makes it:
- slightly more than three times the size of Washington, DC
- slightly more than one third the size of Hertfordshire
- slightly smaller than Saint Lucia.
Coast and Territorial Sea
The Isle of Man has a coastline of 160 km (99 mi), and a territorial sea extending to a maximum of 12 nm from the coast, or the midpoint between other countries. The total territorial sea area is about 4000 km2 or 1500 sq miles, which is about 87% of the total jurisdiction of the Isle of Man. The Isle of Man only holds exclusive fishing rights in the first 3 nm. The territorial sea is managed by the Isle of Man Government Department of Infrastructure.
The Isle of Man enjoys a temperate climate, with cool summers and mild winters. Average rainfall is high compared to the majority of the British Isles, due to its location to the western side of Great Britain and sufficient distance from Ireland for moisture to be accumulated by the prevailing south-westerly winds. Average rainfall is highest at Snaefell, where it is around 1,900 mm (74.8 in) a year. At lower levels it can fall to around 800 mm (31.5 in) a year.
Temperatures remain fairly cool, with the recorded maximum being 28.9 °C (84.0 °F) at Ronaldsway.
The island's terrain is varied. There are two mountainous areas divided by a central valley which runs between Douglas and Peel. The highest point in the Isle of Man, Snaefell, is in the northern area and reaches 620 metres (2,034 ft) above sea level. The northern end of the island is a flat plain, consisting of glacial tills and marine sediments. To the south the island is more hilly, with distinct valleys. There is no land below sea level.
- Arable land: 43.86%
- Permanent crops: 0%
- Other: 56.14% (includes permanent pastures, forests, mountain and heathland) (2011)
Natural hazards and environmental issues
There are few severe natural hazards, the most common being high winds, rough seas and dense fog. In recent years there has been a marked increase in the frequency of high winds, heavy rains, summer droughts and flooding both from heavy rain and from high seas. Snow fall has decreased significantly over the past century while temperatures are increasing year round with rainfall decreasing.
Global warming and a sea level rise potentially pose a great threat to the Isle of Man. All of the Island's towns are at threat from rising sea levels while the Northern Plain, a large, flat and low-lying plain composed of soft marine sediments and glacial material, which makes up about a quarter of the Island's landmass, is in danger of being lost to the sea over the next two centuries. The same is true for the considerably smaller Southern Plain surrounding the settlements of Castletown and Ballasalla and including Ronaldsway Airport
Protected sites for nature conservation
In order of importance, international first, non-statutory last.
- The entire territory of the Isle of Man, including all land, sea, freshwater, airspace and seabed is a UNESCO Biosphere Reserve
- Ballaugh Curraghs (2006, 183.86 ha (454.33 acres)). Shares an identical boundary to the Ballaugh Curraghs ASSI.
- The Ayres (2000, 272 ha (670 acres))
There are 21 ASSIs on the Isle of Man as of 01/09/16. One additional ASSI has been rescinded (Ramsey Harbour).
- Ballachurry Meadows
- Ballacrye Meadow
- Ballateare Meadow
- Ballaugh Curraghs (2005, 183.86 ha (454.33 acres))
- Central Ayres (1996, 272 ha (670 acres))
- Cronk y Bing
- Cronk e King
- Dalby Coast
- Dhoon Glen (2007)
- Eary Vane
- Glen Maye
- Glen Rushen
- Greeba Mountain & Central Hills
- Jurby Airfield
- Langness, Derbyhaven & Sandwick
- Maughold Cliffs & Brooghs
- Port St Mary Ledges & Kallow Point
- Poyll Vaaish Coast
- Ramsey Harbour, designated and later rescinded in 2010
- Ramsey Moorage Shore
- Rosehill Quarry, Billown
- Santon Gorge & Port Soldrick
The Isle of Man had 45 non-statutory wildlife sites as of 30 January 2009, covering about 195 ha (0.75 sq miles) of land and an additional 10.5 km (6.5 mi) of inter-tidal coast. The Manx Wildlife Trust also manages 24 nature reserves, along with the Calf of Man, as of September 2016:
- Ballalough Reedbeds: 1.4 ha (3.5 acres)
- Ballamooar Meadow
- Ballanette: nature reserve, private
- Barnell Reservoir
- Breagle Glen: 0.75 acres (0.30 ha)
- Calf of Man: owned by Manx National Trust, managed by Manx Wildlife Trust
- Clay Head Brooghs
- Close Sartfield: 31 acres (13 ha), part of the Ballaugh Curraghs Ramsar Site
- Close Umpson
- Curragh Feeagh
- Curragh Kionedroghad: 1 ha (2.5 acres)
- Curraghs Wildlife Park: 26 acres (11 ha)
- Dalby Mountain Moorland: 28 ha (69 acres)
- Dalby Mountain Fields
- Dobbie's Meadow
- Fell's Field
- Gob ny Silvas: wildlife site, private
- Goshen: 28 acres (11 ha), part of Ballaugh Curraghs Ramsar Site
- Glen Dhoo: 24.5 acres (9.9 ha)
- Lough Cranstal
- Lough Gat-e-Whing
- Miss Gyler's Meadow
- Moaney & Crawyn's Meadows
- The Purt/Glen Dhoo
Marine no-take zones
The majority of the island is formed from highly faulted and folded sedimentary rocks of the Ordovician period. There is a belt of younger Silurian rocks along the west coast between Niarbyl and Peel, and a small area of Devonian sandstones around Peel. A band of Carboniferous period rocks underlies part of the northern plain, but is nowhere seen at the surface; however similar age rocks do outcrop in the south between Castletown, Silverdale and Port St Mary. Permo-Triassic age rocks are known to lie beneath the Point of Ayre but, as with the rest of the northern plain, these rocks are concealed by substantial thicknesses of superficial deposits.
The island has significant deposits of copper, lead and silver, zinc, iron, and plumbago (a mix of graphite and clay). There are also quarries of black marble, limestone flags, clay schist, and granite. These are all modern, and there was no noticeable exploitation of metals or minerals prior to the modern era.
The island has a census-estimated population of 84,497 according to the most recent 2011 census: up from 79,805 in 2006 and 76,315 in 2001.
The island's largest town and administrative centre is Douglas, whose population is 23,000 — nearly a third of the population of the island. Neighbouring Onchan, Ramsey in the north, Peel in the west and the three southern ports of Castletown, Port Erin and Port St Mary are the island's other main settlements. Almost all its population lives on or very near the coast.
- This article incorporates public domain material from the CIA World Factbook website https://www.cia.gov/library/publications/the-world-factbook/index.html.