Geography of Jersey
|This article needs additional citations for verification. (February 2013)|
|Native name: Jèrri|
Map of islands of Bailiwick of Jersey
Jersey (off the coast of France)
|Area||119.49 km2 (46.14 sq mi)|
|Length||14 km (8.7 mi)|
|Width||8 km (5 mi)|
|Coastline||70 km (43 mi)|
|Highest elevation||143 m (469 ft)|
|Highest point||Les Platons|
|Capital city||Saint Helier|
|Largest settlement||Saint Helier|
|Population||99,500 (as of 2013)|
|Density||819 /km2 (2,121 /sq mi)|
|Ethnic groups||English and Norman-French descent. Portuguese and Polish minorities|
This article describes the geography of Jersey, an island territory in the English Channel. The island of Jersey has an area of 119 square kilometres, with 70 kilometres of coastline. Jersey claims a territorial sea of 3 nmi (5.6 km; 3.5 mi) and an exclusive fishing zone of 12 nmi (22.2 km; 13.8 mi).
Jersey is the largest and southernmost of the Channel Islands. It is located north of Brittany and west of the Cotentin Peninsula in Normandy. About 30% of the population of the island is concentrated in Saint Helier, which is a parish and the capital town of the island.
The highest point in the island is Les Platons on the north coast, at 136 metres (446 ft). Parts of the parish of St Clement in the south were previously below sea-level but the construction of a seawall and infilling of low land has probably left only a few pockets of land below mean sea level. The terrain is generally low-lying on the south coast, with some rocky headlands, rising gradually to rugged cliffs along the north coast. On the west coast there are sand dunes. Small valleys run north to south across the island. Very large tidal variation exposes large expanses of sand and rock to the southeast at low tide.
The climate in the island is temperate, with mild winters and cool summers. Although the minimum daily temperature can fall below freezing in the winter, the monthly average temperature does not. The Atlantic Ocean has a moderating effect on temperature in Jersey, as water has a much greater specific heat capacity than air and tends to heat and cool slowly throughout the year. This has a warming influence on coastal areas in winter and a cooling influence in summer.
The highest temperature recorded was 36.0 °C (96.8 °F) on 9 August 2003, and the lowest temperature recorded was −10.3 °C (13.5 °F) on 5 January 1894. By comparison, higher temperatures are found in mainland United Kingdom, which achieved 38.5 °C (101.3 °F) in Faversham, Kent on 10 August 2003. The impact of the Atlantic Ocean and costal winds ensure that Jersey is cooler than the UK during the summer months.
Snow falls rarely in Jersey, some years will pass with no snow fall at all.
|Climate data for Jersey|
|Average high °C (°F)||8.3
|Average low °C (°F)||4.3
|Average rainfall mm (inches)||93.1
|Avg. rainy days (≥ 1.0 mm)||14.8||11.7||11.7||10.1||8.9||7.5||7.1||7.3||9.2||13.6||15.2||15.2||132.2|
|Mean monthly sunshine hours||66.1||91.6||134.0||196.5||236.7||245.4||252.7||235.3||184.6||118.8||79.9||63.2||1,904.8|
|Source: Met Office|
The main natural resource on this island is arable land. 66% of the island's land is used as such, and the remaining 34% is used for other purposes.
Current environmental issues for Jersey include waste disposal, air pollution and traffic.