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Loch Ryan
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Loch Ryan
Loch Ryan (Scottish Gaelic: Loch Rìoghaine, pronounced [l̪ˠɔx ˈrˠiː.ɛɲə]) is a Scottish sea loch that acts as an important natural harbour for shipping, providing calm waters for ferries operating between Scotland and Northern Ireland. The town of Stranraer is the largest settlement on its shores, with ferries to and from Northern Ireland operating from Cairnryan further north on the loch.
Loch Ryan is orientated on a north–south axis, its mouth looking northward into the North Atlantic and Firth of Clyde, and the town of Stranraer sitting on its southern shores. The loch is bounded by the Rhins of Galloway peninsula on its western side and the Scottish landmass in the east (comprising Galloway and South Ayrshire), the northern points of the loch are Milleur Point and Finnarts Point. The loch itself is about 8 miles (13 km) long from north to south, and about 3 miles (4.8 km) wide at its widest point. Nearby roads include the A77 in the east and the A718 in the west. The Loch Ryan basin as it is seen today formed as a result of geological and glacial activity. The first period of activity occurred during the Paleozoic era, with two periods of change. Firstly, during the Devonian period (360 to 416 million years ago) the land in the area underwent a series of shearing events which considerably altered its shape, forming a basin. Then, during the Permian period (250 to 300 million years ago) this basin filled up with sediments which were compacted to form soft sandstones. At this point in time the area would have been positioned around the equator and would form part of the Pangaea supercontinent. The second period of activity was as a result of the numerous glacial episodes during the Quaternary period, from 2 million years ago up until the last glaciers retreated 10,000 years ago.
As all of northern Europe experienced numerous Ice ages, glacier formation created ice flows and Ice sheets. The erosive force of the ice moved across the land, removing the soft sandstone and leaving behind the harder rocks. When the ice sheet melted with the rising temperatures 10,000 years ago the basin was uncovered and was flooded by the sea, forming the loch that is seen today.
Since the end of the last ice-age the sea has continued to change the loch by erosion and deposition. The loch has a sandbank on its western shores called 'the Scar'. This bank, just south of the village of Kirkcolm, is an important breeding ground for terns.
Historically the loch has seen human activity on its shores since ancient times. Sheltered from the rough seas of the North Channel and the North Atlantic the loch has been an important safe harbour for vessels. William Smith, Britain's foremost classicist of the 19th century, identifies Ptolemy's toponym Abrauannus (Ancient Greek: Ἀβραουάννος), with Loch Ryan, particularly with its outlet to the sea. Ptolemy described Abrauannus or Abravannus as a river of Britannia Barbara, that discharged itself a little northward of the Promontorium Novantum, or Mull of Galloway into Luce Bay. According to Smith, Abravannus is probably the stream which flows through Loch Ryan into the sea – Ab-Ryan, or the offspring of Ryan, being easily convertible into the Roman form of the word Ab-Ryan-us – Abravannus.
In early 1307 at the beginning of Robert the Bruce's campaign in the wars of independence he sent two forces to attempt to gain control of south west Scotland. One force, led by his two brothers, consisting of eighteen galleys, landed in the loch. In the Battle of Loch Ryan, they were immediately overwhelmed by local forces, led by Dungal MacDouall, who was a supporter of the Comyns.
The loch would have been used historically for traditional maritime activities including fishing. The Statistical account of Scotland 1791–99, records:
The later Account of 1834-45 expands on this issue, as it states:
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Loch Ryan AI simulator
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Loch Ryan
Loch Ryan (Scottish Gaelic: Loch Rìoghaine, pronounced [l̪ˠɔx ˈrˠiː.ɛɲə]) is a Scottish sea loch that acts as an important natural harbour for shipping, providing calm waters for ferries operating between Scotland and Northern Ireland. The town of Stranraer is the largest settlement on its shores, with ferries to and from Northern Ireland operating from Cairnryan further north on the loch.
Loch Ryan is orientated on a north–south axis, its mouth looking northward into the North Atlantic and Firth of Clyde, and the town of Stranraer sitting on its southern shores. The loch is bounded by the Rhins of Galloway peninsula on its western side and the Scottish landmass in the east (comprising Galloway and South Ayrshire), the northern points of the loch are Milleur Point and Finnarts Point. The loch itself is about 8 miles (13 km) long from north to south, and about 3 miles (4.8 km) wide at its widest point. Nearby roads include the A77 in the east and the A718 in the west. The Loch Ryan basin as it is seen today formed as a result of geological and glacial activity. The first period of activity occurred during the Paleozoic era, with two periods of change. Firstly, during the Devonian period (360 to 416 million years ago) the land in the area underwent a series of shearing events which considerably altered its shape, forming a basin. Then, during the Permian period (250 to 300 million years ago) this basin filled up with sediments which were compacted to form soft sandstones. At this point in time the area would have been positioned around the equator and would form part of the Pangaea supercontinent. The second period of activity was as a result of the numerous glacial episodes during the Quaternary period, from 2 million years ago up until the last glaciers retreated 10,000 years ago.
As all of northern Europe experienced numerous Ice ages, glacier formation created ice flows and Ice sheets. The erosive force of the ice moved across the land, removing the soft sandstone and leaving behind the harder rocks. When the ice sheet melted with the rising temperatures 10,000 years ago the basin was uncovered and was flooded by the sea, forming the loch that is seen today.
Since the end of the last ice-age the sea has continued to change the loch by erosion and deposition. The loch has a sandbank on its western shores called 'the Scar'. This bank, just south of the village of Kirkcolm, is an important breeding ground for terns.
Historically the loch has seen human activity on its shores since ancient times. Sheltered from the rough seas of the North Channel and the North Atlantic the loch has been an important safe harbour for vessels. William Smith, Britain's foremost classicist of the 19th century, identifies Ptolemy's toponym Abrauannus (Ancient Greek: Ἀβραουάννος), with Loch Ryan, particularly with its outlet to the sea. Ptolemy described Abrauannus or Abravannus as a river of Britannia Barbara, that discharged itself a little northward of the Promontorium Novantum, or Mull of Galloway into Luce Bay. According to Smith, Abravannus is probably the stream which flows through Loch Ryan into the sea – Ab-Ryan, or the offspring of Ryan, being easily convertible into the Roman form of the word Ab-Ryan-us – Abravannus.
In early 1307 at the beginning of Robert the Bruce's campaign in the wars of independence he sent two forces to attempt to gain control of south west Scotland. One force, led by his two brothers, consisting of eighteen galleys, landed in the loch. In the Battle of Loch Ryan, they were immediately overwhelmed by local forces, led by Dungal MacDouall, who was a supporter of the Comyns.
The loch would have been used historically for traditional maritime activities including fishing. The Statistical account of Scotland 1791–99, records:
The later Account of 1834-45 expands on this issue, as it states:
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