Search results
Results from the WOW.Com Content Network
The WGS 84 latitude lines are about 70 m south of the OSGB 36 lines in South Cornwall, the difference diminishing to zero in the Scottish Borders, and then increasing to about 50 m north on the north coast of Scotland. (If the lines are further east, then the longitude value of any given point is further west. Similarly, if the lines are ...
Module:Location map/data/United Kingdom is a location map definition used to overlay markers and labels on an equirectangular projection map of the United Kingdom. The markers are placed by latitude and longitude coordinates on the default map or a similar map image.
This is a list of the extreme points of England: the points that are farther north, south, east or west than any other location, as well as the highest and lowest points. England (including islands) [ edit ]
This is a list of the extreme points of the United Kingdom: the points that are farther north, south, east or west than any other location.Traditionally the extent of the island of Great Britain has stretched "from Land's End to John o' Groats" (that is, from the extreme southwest of mainland England to the far northeast of mainland Scotland).
Toggle Examples using location map templates subsection. 5.1 Location map, using default map (image) ... Module: Location map/data/UK England/doc. Add languages ...
UK's topography As this geological map of Great Britain demonstrates, the geology of the UK is varied and complex. The physical geography of the UK varies greatly. England consists of mostly lowland terrain, with upland or mountainous terrain only found north-west of the Tees–Exe line .
This page was last edited on 25 October 2019, at 20:39 (UTC).; Text is available under the Creative Commons Attribution-ShareAlike 4.0 License; additional terms may apply.
The centroid is a mathematically derived point that is in every sense the centre of a two dimensional area like a piece of land. If a straight line is drawn through a centroid in any direction there will be equal length of the line on either side of the centroid as measured from it to the boundary if the line is unbroken on either side.