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Broomrigg G is a standing stone located in Broomrigg Plantation, approximately 730 metres south-east of Street House in Cumberland, England. The monument dates to the prehistoric period, representing a surviving example of the standing stones erected during the Bronze Age in northern England. The stone forms part of a wider landscape of prehistoric monuments in the region, reflecting the ritual and territorial significance of these monuments to ancient communities. It is recorded as a scheduled ancient monument under the national heritage listing system.
Broomrigg G: standing stone in Broomrigg Plantation, 730m south east of Street House is a scheduled monument protected by Historic England under reference 1015275. View the official record →
Broomrigg G is a standing stone located in Broomrigg Plantation, approximately 730 metres south-east of Street House in Cumberland, England. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1015275.
Broomrigg G: standing stone in Broomrigg Plantation, 730m south east of Street House is a Scheduled Ancient Monument, legally protected by Historic England (NHLE) — the body responsible for designating and safeguarding heritage sites in England. The official designation reference is 1015275.
Several scheduled monuments lie within 10 km, including Broomrigg F: two hut circles in Broomrigg Plantation, 900m south east of Street House (0.5 km), Kirkoswald Castle moated site (5.9 km), Medieval moated site W of St Oswald's Church (6.1 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Broomrigg G: standing stone in Broomrigg Plantation, 730m south east of Street House's history, each drawn from the record and mapped to the exact spot:
Every location is different. Not every section appears for every place, only what the historical record actually holds turns up in a report.
Broomrigg G: standing stone in Broomrigg Plantation, 730m south east of Street House stands on Triassic Rocks (Undifferentiated), bedrock that formed in the Triassic. The rock here is sandstone and conglomerate, interbedded.