A geography of england
Jurassic Coast. Gloucestershire is blessed with deep and impossibly verdant valleys and combes, where houses of warm yellow stone nestle, giving way to broad and sometimes sunlit uplands with breath-taking views; not far to the south is the more open landscape of Somerset with its massy tors and the tamed wetland of the Levels; to the east, Wiltshire has its hoarily ancient landscape of chalk and downs, littered with ancient barrows — a place that still feels like the beginning of everything. Historically, the most important ports on the south coast include Dover, Folkestone, Portsmouth, Southampton, and Poole. This mountain range measures approximately kilometres or miles in length. Despite the political, economic, and cultural legacy that has secured the perpetuation of its name, England no longer officially exists as a governmental or political unit—unlike Scotland, Wales, and Northern Ireland , which all have varying degrees of self-government in domestic affairs. Winter temperatures seldom plummet below zero degrees Celsius, while summer highs can reach about 30 degrees Celsius. It is rarely marked by extremes of heat or cold. Precipitation, heaviest during October, averages about mm 30 in annually in most of England, although the west coast tends to be wetter than the east. England occupies all of the island east of Wales and south of Scotland, another country and division of the United Kingdom. Unsourced material may be challenged and removed. The capital, largest city, and chief port of England is London, with a population of 7,, England makes extensive use of its inland waterways, such as its rivers.
The Highland Zone This zone is characterised by rocky, rugged hills and eroded mountain faces, interrupted by valleys and extensive plains.
The mean annual temperature ranges between This church also has a constitutional position within the United Kingdom.
Precipitation is also common throughout much of the year. The coastline here is similar to the North Sea coast in that it is mainly flat and sandy, with the only notable cliffs along this stretch of coast being at St Bees Head in Cumbria. Because these higher lying areas get less sunlight during the day and more rainfall than the lower lying areas, they are generally colder and unsuitable for farming.
The average January and July temperatures for London, which has its own, warmer, microclimate, are 4. However, they are physically connected to each other by the Channel Tunnel near Folkestone. Further to the south are the counties of the Channel Coast, Hampshire and Dorset, rich in good harbours and from very early on places where both contacts overseas as through two safe expanses of water at Poole and the Solent and necessary defence Roman forts, mediaeval castles, Victorian batteries have left their mark.
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