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Jarlshof is the best known prehistoric archaeological site in Shetland, Scotland. It lies near the southern tip of the Shetland Mainland and has been described as "one of the most remarkable archaeological sites ever excavated in the British Isles". It contains remains dating from 2500 BC up to the 17th century AD.

The Bronze Age settlers left evidence of several small oval houses with thick stone walls and various artefacts including a decorated bone object. The Iron Age ruins include several different types of structure including a broch and a defensive wall around the site. The Pictish period provides various works of art including a painted pebble and a symbol stone. The Viking-age ruins make up the largest such site visible anywhere in Britain and include a longhouse; excavations provided numerous tools and a detailed insight into life in Shetland at this time. The most visible structures on the site are the walls of the Scottish period fortified manor house, which inspired the name "Jarlshof" that first appears in an 1821 novel by Walter Scott.

The site is in the care of Historic Scotland and is open from April to September. In 2010 "The Crucible of Iron Age Shetland" including Mousa, Old Scatness and Jarlshof was added to those seeking to be on the "tentative list" of World Heritage Sites.

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The Old Man of Hoy is a 449-foot (137m) sea stack on the island of Hoy, part of the Orkney archipelago off the north coast of Scotland. Formed from Old Red Sandstone, it is one of the tallest stacks in Britain. The Old Man is popular with climbers, and was first climbed in 1966. Created by the erosion of a cliff through hydraulic action some time after 1750, the stack is no more than a few hundred years old, and may soon collapse into the sea.

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Smoo Cave is formed within Early Ordovician dolostones of the Durness Group (also known as the Durness Limestone). The cave has formed along the boundary between the light grey Sangomore Formation and the dark grey, mottled Sailmhor Formation (sometimes called Leopard Rock), both of which form part the Durness Group succession. These horizons close to the formation boundary are characterised by large and abundant chert nodules which can be found all along the inner stream chamber where they have been left behind after dissolution of the surrounding dolostone. The cave was formed along two geological lines of weakness by a combination of erosion from the sea and an inland underground stream which has formed the innermost chambers. Upstream of the Allt Smoo which runs into the cave, impermeable quartzites have been faulted against the Durness Limestone, causing the stream to sink down into the carbonate rock soon after it has crossed the contact between the two different rock types.

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The Quiraing is a landslip on the eastern face of Meall na Suiramach, the northernmost summit of the Trotternish Ridge on the Isle of Skye. The whole of the Trotternish Ridge escarpment was formed by a great series of landslips; the Quiraing is the only part of the slip still moving, the road at its base near Flodigarry requires repairs each year. Parts of the distinctive landscape have earned particular names. The Needle is a jagged 120-foot (37 m) high landmark pinnacle, a remnant of landslipping. Northwest of it is The Table, a flat grassy area slipped down from the summit plateau, with vistas of the Torridon Hills and the mountains of Wester Ross. Southwest is the Prison, a pyramidal rocky peak which can look like a medieval keep when viewed from the right angle - the ascent of this is an airy scramble.

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Skye or the Isle of Skye  is the largest and most northerly large island in the Inner Hebrides of Scotland. The island's peninsulas radiate from a mountainous centre dominated by the Cuillins, the rocky slopes of which provide some of the most dramatic mountain scenery in the country.Although it has been suggested that the Gaelic Sgitheanach describes a winged shape there is no definitive agreement as to the name's origins.

The island has been occupied since the Mesolithic period and its history includes a time of Norse rule and a long period of domination by Clan MacLeod and Clan Donald. The 18th-century Jacobite risings led to the breaking up of the clan system and subsequent Clearances that replaced entire communities with sheep farms, some of which also involved forced emigrations to distant lands. Resident numbers declined from over 20,000 in the early 19th century to just under 9,000 by the closing decade of the 20th century. Skye's population increased by 4 per cent between 1991 and 2001.[11] About a third of the residents were Gaelic speakers in 2001, and although their numbers are in decline this aspect of island culture remains important.

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Dunnottar Castle  is a ruined medieval fortress located upon a rocky headland on the north-east coast of Scotland, about 3 kilometres  south of Stonehaven. The surviving buildings are largely of the 15th and 16th centuries, but the site is believed to have been fortified in the Early Middle Ages.

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It’s made entirely from hexagon shape pillars and

lies on the uninhabited Scottish island of Staffa,

so yes, you’ll have to take a bit of a boat ride

over to this one.