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The British Wool Society grazed sheep on the island in the 1790s and the land was farmed for many years until the last farmer, Peter Hogg, died in 1904. [11] Throughout most of its history, Cramond Island was used for farming, especially sheep-farming, [2] and perhaps served as a fishing outpost as well.
The island was also used for a construction office and the castle buildings were re-roofed to accommodate workers. Some of the stone from the former castle was used to build the caissons of the bridge. [2] [53] Cramond Island in the Almond estuary is a tidal island that is 7.7 hectares (19 acres) in extent and is currently part of the Dalmeny ...
Off the coast lie the small islands of Inchmickery and Cramond Island. The land gradually rises to the south, with the Pentland Hills in the south-west, Moorfoot Hills in the centre-south and the Lammermuir Hills in the far south-east. Blackhope Scar on the border with Peeblesshire is the highest point in the county at 651 m (2,136 ft).
Milton Island or Green Inch was an island in the Clyde's estuarine waters close to the old ford across the river at Dumbuck near Dumbarton. Newshot Island or Newshot Isle was an island of circa 50 acres or 20 hectares lying in the River Clyde close to Park Quay, Renfrewshire, Scotland. It is now partly joined to the river bank.
Coastal fortifications in Scotland played a vital role during the World Wars, protecting shipping as they mustered to convoy.New fortifications were built and old defences were also rebuilt or strengthened around the Scottish coast in case of invasion.
Cramond Roman Fort is a Roman-Era archaeological site at Cramond, Edinburgh, Scotland. [1] The settlement may be the "Rumabo" listed in the 7th-century Ravenna Cosmography . The fort was established around 140 AD and occupied until around 170 AD, with a further period of occupation from around 208 to 214 AD. [ 2 ]
Interest in the island's history began to surface again in 2022 when it was announced the Carleton Island Villa, one of the most well-known landmarks on the St. Lawrence River, although in ...
Geologically, the Firth of Forth is a fjord, formed by the Forth Glacier in the last glacial period. [6] The drainage basin for the Firth of Forth covers a wide geographic area including places as far from the shore as Ben Lomond, Cumbernauld, Harthill, Penicuik and the edges of Gleneagles Golf Course.