Gamelshiel Castle - 4 Things to Know Before Visiting

Whiteadder Reservoir is a reservoir in East Lothian, Scotland, UK, in the Lammermuir Hills, 11 miles north west of Duns in the Scottish Borders, and five miles south east of Garvald. It was created to provide additional water facilities for East Lothian. Work on the Dam forming the reservoir commenced in 1964. Design was carried out by consulting civil engineers GH Hill & Sons of Manchester and London, on behalf of the then local water authority - East Lothian Water Board.

Sancta Maria Abbey, Nunraw is a working Trappist monastery. It was the first Cistercian house to be founded in Scotland since the Scottish Reformation. Founded in 1946 by monks from Mount St. Joseph Abbey, Roscrea, Ireland, and consecrated as an Abbey in 1948, it nestles at the foot of the Lammermuir Hills on the southern edge of East Lothian. The estate of the abbey is technically called White Castle after an early hill-fort on the land.

A decidious and scenic woodland in East Lothian that features a large lake with quiet walks along several trails. The 212-acre site is managed by the Woodland Trust who have saved the native broadleaf trees from invasive Rhododendrons that were planted by the Victorians.

Pressmennan Lake is a lake in East Lothian in Scotland. It is an artificial reservoir constructed in 1819 by a Mr Nesbit who dammed the streams flowing into the gully, it was said to be well stocked with carp, perch and trout. It lies in a gully in the Lammermuir Hills, above the village of Stenton in East Lothian. It is roughly 2 kilometres in length but less than 100 metres broad.

Yester Castle is surely one of Scotland’s most memorable and hair-raising castles. Concealed in the woods of the Yester Estate in East Lothian, it dates to the mid-13th century. The only remaining complete structure is the subterranean Goblin Ha' or Hobgoblin Ha' . It is a Scheduled Ancient Monument, recorded as such by the Royal Commission on the Ancient and Historical Monuments of Scotland.

The Lammermuirs are a range of hills in southern Scotland, forming a natural boundary between East Lothian and the Borders. Numerous dykes of different lithologies largely of Devonian age but some of Carboniferous age and with a generally NE-SW alignment occur throughout the area. The Priestlaw Intrusion is a mass of late Silurian/early Devonian granite which occurs in the area of Whiteadder Reservoir.