Blog Archive

Earthworks at Redmire

Redmire, a charming village nestled in the heart of North Yorkshire, England, boasts a rich tapestry of history that is as picturesque as its serene landscapes.

Earthworks at Bellerby, Leyburn

Bellerby, a charming village nestled in the heart of North Yorkshire, England, boasts a rich tapestry of history that dates back to the Domesday Book of 1086, where it was recorded as “Belgebi” – a name derived from Old Norse, meaning “Berg’s farmstead or clearing.”

St Michael & All Angels, Downholme

The history of St Michael & All Angels in Downholme is woven through the centuries.

How Hill Hillfort

How Hill, near Downholme in North Yorkshire, is the site of a large univallate hillfort.

Earthworks at Walburn Hall Farm, Richmond

The Earthworks at Walburn Hall Farm in Richmond are a testament to the area’s rich historical tapestry, dating back to medieval times.

Earthworks at Stainton

The earthworks surrounding Stainton in North Yorkshire are part of a rich archaeological tapestry that speaks to the region’s ancient past. These structures are believed to be remnants of extensive field systems, possibly dating back to the post-Roman period.

Ellerton Abbey

Ellerton Abbey, nestled in the picturesque landscape of North Yorkshire, holds a rich tapestry of history that intertwines with the broader narratives of England’s past.

Marrick Priory

Marrick Priory, a historic gem nestled in the Yorkshire Dales, has a rich history that dates back to the 12th century.

Penhill Preceptory – Chapel of the Knights Templar

The history of Penhill Preceptory is closely tied to the dramatic rise and fall of the Knights Templar. The order was initially founded to protect Christian pilgrims travelling to the Holy Land, but over time, they amassed great wealth and influence, which eventually led to their downfall.

Grinton Lodge Earthworks

The earthworks that sit on the hillside between Grinton Lodge and the B6270 are part of a fascinating archaeological landscape in North Yorkshire. These features are distinct from the nearby Grinton-Fremington Dyke System, which dates back to the post-Roman period and is believed to have formed part of the boundary of an early British kingdom.

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