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The format of all files is human readable plain text (excluding 3D models), which semantically describe the cave, and are compiled by the program into various output forms such as 2D PDF or SVG maps, or 3D models. Other files like map overlays, terrain models and pictures can be incorporated into the output.
Short Drop Cave – Gavel Pot System – links to Lost Johns' Cave by diving. Death's Head Hole – Long Drop Cave – links to Lost Johns' Cave. Rumbling Hole – links to Lost Johns' Cave. Pippikin Pot – links to Ease Gill Caverns, and to Witches Cave by diving. Ease Gill Caverns – links to Pippikin Pot, and to Bull Pot of Witches by diving.
The stones were inscribed with a sequential number followed by the letters "ABD" for Aberdeen. Aberdeen has two sets of march, or boundary, stones. The outer line surrounds the area of the Freedom Lands. The inner line of stones marks a smaller area: the boundary of the crofts immediately around the medieval Royal Burgh of Aberdeen. [4]
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The Sculptor's Cave is a sandstone cave on the south shore of the Moray Firth in Scotland, near the small settlement of Covesea, between Burghead and Lossiemouth in Moray. [1] It is named after the Pictish carvings incised on the walls of the cave near its entrances. [ 2 ]
Cove Bay, known locally as Cove, is a suburb on the south-east edge of Aberdeen, Scotland. Today Cove is home to around 8,000 people. It is a popular residential location owing to its village-like status. It is a quiet suburb at the Southern edge of Aberdeen City and in 2020 won the Silver Gilt award for Scotland in Bloom.
Visitors to the site can undertake various walks. The most popular walk is the 0.6 miles (1 km)-long journey to Ossian's Hall. Wheelchairs are accommodated via a pass-for-all route. [1] There is also a link to a thirty-mile network of footpaths beyond The Hermitage to various parts of Dunkeld. These paths date back to the 18th century. [1]
Star Carr now lies under farmland at the eastern end of the Vale of Pickering. During the Mesolithic the site was near the outflow at the western end of a palaeolake, known as Lake Flixton . [ 2 ] At the end of the last ice age a combination of glacial and post-glacial geomorphology caused the area to drain to the west (away from the shortest ...