The
Caldicot and Wentloog Levels are two areas of low-lying estuarine
alluvial wetland and
intertidal mudflats adjoining the north bank of the
Severn estuary, either side of the
River Usk estuary near
Newport in south east
Wales. They are also known collectively as the
Monmouthshire Levels or
Gwent Levels.
The
Caldicot Level lies to the southeast of Newport between the
River Usk and
River Wye and consists of . It is home to
Newport Wetlands Reserve. The
Wentloog Level lies to the southwest between the River Usk and
Rhymney River and consists of .
The levels are formed from tidal deposits and
alluvium, which have been recurrently inundated and reclaimed from the Severn Estuary by humans since
Roman times. They have patterns of settlement, enclosure and drainage systems belonging to successive periods of use, and are extremely rich
archaeologically, with finds from the
Mesolithic,
Bronze Age and
Iron Age periods.
They are an important wetland resource. Parts have been designated as
Sites of Special Scientific Interest. They are registered as a Historic Landscape of Outstanding Historic Interest in Wales.
History and archaeology
There have been variations in both land and sea levels in the Severn estuary since the start of human habitation in the area. The Levels have been reclaimed from the sea at different times during the historic period, preserving evidence of patterns of settlement, enclosure and drainage...
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