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The Isle of Mull [6] or simply Mull [3] [7] (Scottish Gaelic: Muile ⓘ) [8] is the second-largest island of the Inner Hebrides (after Skye) and lies off the west coast of Scotland in the council area of Argyll and Bute. Covering 875.35 square kilometres (337.97 sq mi), Mull is the fourth-largest island in Scotland.
Kilfinichen and Kilvickeon is a civil parish on the Isle of Mull in the county of Argyll, Scotland, part of the Argyll and Bute council area. It is one of three parishes on the island and extends over the south-western part and includes the islands of Iona, Erraid and Inch Kenneth. It is bordered by the parish of Torosay in the north and east ...
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Inch Kenneth (Scottish Gaelic: Innis Choinnich) is a small grassy island off the west coast of the Isle of Mull, in Scotland. It is at the entrance of Loch na Keal , to the south of Ulva . It is part of the Loch na Keal National Scenic Area , one of 40 in Scotland. [ 4 ]
Tobermory (/ ˌ t oʊ b ər ˈ m ɔːr i /; Scottish Gaelic: Tobar Mhoire) [2] is the capital of, and until 1973 the only burgh on, the Isle of Mull in the Scottish Inner Hebrides.It is located on the east coast of Mishnish, the most northerly part of the island, near the northern entrance of the Sound of Mull.
Sa Vĩ Cap in Trà Cổ island is the North-Easternmost promontory of Vietnam Co To Islands 20°59′00″N 107°46′00″E / 20.98333°N 107.76667°E / 20.98333; 107 Hạ Long Bay 's islets 20°54′N 107°12′E / 20.900°N 107.200°E / 20.900; 107
The Ross of Mull (Scottish Gaelic: An Ros Mhuileach) is the largest peninsula of the Isle of Mull, about 28 kilometres (17 mi) long, and makes up the south-western part of the island. It is bounded to the north by Loch Scridain and to the south by the Firth of Lorne .
The geology of the Isle of Mull in Scotland is dominated by the development during the early Palaeogene period of a ‘volcanic central complex’ associated with the opening of the Atlantic Ocean. The bedrock of the larger part of the island is formed by basalt lava flows ascribed to the Mull Lava Group erupted onto a succession of Mesozoic ...