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Money Tump is a bowl barrow situated in Gloucestershire, England, representing a form of burial monument characteristic of the Neolithic and Bronze Age periods. The site is registered on the National Heritage List for England under entry number 1016874. As a bowl barrow, the monument consists of a circular or oval earthwork mound of modest elevation, a common funerary structure type in prehistoric Britain. The barrow's local name reflects the folk nomenclature often applied to such ancient monuments in the English landscape, though the specific circumstances of its construction and use remain typical of the broader corpus of comparable burial sites from the same archaeological period and region.
Bowl barrow known as Money Tump is a scheduled monument protected by Historic England under reference 1016874. View the official record →
Money Tump is a bowl barrow situated in Gloucestershire, England, representing a form of burial monument characteristic of the Neolithic and Bronze Age periods. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1016874.
Bowl barrow known as Money Tump 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 1016874.
Several scheduled monuments lie within 10 km, including Norn`s Tump long barrow, 400m south-east of Hill Farm (6.5 km), Romano-British farmstead 200m south west of Longman's Barn Farm (7 km), Bowl barrow 150m north-east of Brandhouse Farm (7.4 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Bowl barrow known as Money Tump'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.
Bowl barrow known as Money Tump stands on Great Oolite Group, bedrock that formed in the Bathonian. The rock here is sandstone, limestone and argillaceous rocks.