The Mid Cheshire Ridge is a range of low
sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks.
Most sandstone is composed of quartz or feldspar (both silicates) ...
hills which stretch north to south through
Cheshire
Cheshire ( ) is a ceremonial and historic county in North West England, bordered by Wales to the west, Merseyside and Greater Manchester to the north, Derbyshire to the east, and Staffordshire and Shropshire to the south. Cheshire's county t ...
in
North West England
North West England is one of nine official regions of England and consists of the ceremonial counties of England, administrative counties of Cheshire, Cumbria, Greater Manchester, Lancashire and Merseyside. The North West had a population of ...
. The ridge is discontinuous, with the hills forming two main blocks, north and south of the "Beeston Gap". The main mass of those to the south are known as the
Peckforton Hills
The Peckforton Hills are a sandstone ridge running broadly northeast–southwest in the west of the English county of Cheshire. They form a significant part of the longer Mid Cheshire Ridge which extends southwards from Frodsham towards Malpas. ...
; the larger group of hills to the north do not have a collective name.
Significant summits
The ridge attains its highest elevation at Raw Head in the
Peckforton Hills
The Peckforton Hills are a sandstone ridge running broadly northeast–southwest in the west of the English county of Cheshire. They form a significant part of the longer Mid Cheshire Ridge which extends southwards from Frodsham towards Malpas. ...
, some 227 m above sea level. Other significant summits and the parishes within which they lie, are from north to south:
*Beacon Hill (150 m), (
Frodsham)
*Woodhouse Hill (145 m), (
Frodsham)
*
Helsby Hill (140 m), (
Helsby)
*Alvanley Cliff (135 m), (
Alvanley
Alvanley is a small rural village and civil parish near Helsby, in the unitary authority of Cheshire West and Chester and the ceremonial county of Cheshire, England. The village is on the B5393 road and near junction 14 of the M56 motorway. ...
)
*Birch Hill (158 m), (
Manley)
*
Old Pale
Delamere Forest is a large wood in the village of Delamere in Cheshire, England. The woodland, which is managed by Forestry England, covers an area of making it the largest area of woodland in the county. It contains a mixture of deciduous and ...
(176 m), (
Delamere)
*Eddisbury Hill (158 m), (
Delamere)
*Primrosehill (158 m), (
Delamere)
*High Billinge (175 m), (
Utkinton
200px, Map of civil parish of Utkinton within the former borough of Vale Royal
Utkinton is a village and former civil parish, now in the parishes of Utkinton and Cotebrook and Tarporley, in the unitary authority of Cheshire West and Chester an ...
)
*Luddington Hill (145 m), (
Utkinton
200px, Map of civil parish of Utkinton within the former borough of Vale Royal
Utkinton is a village and former civil parish, now in the parishes of Utkinton and Cotebrook and Tarporley, in the unitary authority of Cheshire West and Chester an ...
)
**(''Beeston Gap'')
*
Beeston Castle Hill (155 m), (
Beeston)
*Stanner Nab (200 m), (
Peckforton
Peckforton is a scattered settlement (centred at ) and civil parish in the unitary authority of Cheshire East and the ceremonial county of Cheshire, England. The settlement is located to the north east of Malpas and to the west of Nantwich. ...
)
*
Peckforton Hill
The Peckforton Hills are a sandstone ridge running broadly northeast–southwest in the west of the English county of Cheshire. They form a significant part of the longer Mid Cheshire Ridge which extends southwards from Frodsham towards Malpas. ...
(203 m), (
Peckforton
Peckforton is a scattered settlement (centred at ) and civil parish in the unitary authority of Cheshire East and the ceremonial county of Cheshire, England. The settlement is located to the north east of Malpas and to the west of Nantwich. ...
)
*Burwardsley Hill (186 m), (
Burwardsley
Burwardsley is a village and civil parish the unitary authority of Cheshire West and Chester and the ceremonial county of Cheshire, England. The parish also includes the small villages of Burwardsley, Burwardsley Hill, Higher Burwardsley. The ...
)
*
Bulkeley Hill
The Peckforton Hills are a sandstone ridge running broadly northeast–southwest in the west of the English county of Cheshire. They form a significant part of the longer Mid Cheshire Ridge which extends southwards from Frodsham towards Malpas ...
(220 m), (
Bulkeley
Bulkeley () is a village and civil parish in the unitary authority of Cheshire East and the ceremonial county of Cheshire, England. The village is on the A534 road, west of Nantwich. In the 2011 census it had a population of 239.
History
Th ...
)
*
Bickerton Hill
Bickerton Hill refers to two low red sandstone hills that form the southern end of the Mid Cheshire Ridge in Cheshire, north-west England. The high point, Raw Head, lies on the northerly hill and has an elevation of 227 metres. Parts of the ...
(Raw Head) (227 m), (
Bickerton and
Harthill)
*
Bickerton Hill
Bickerton Hill refers to two low red sandstone hills that form the southern end of the Mid Cheshire Ridge in Cheshire, north-west England. The high point, Raw Head, lies on the northerly hill and has an elevation of 227 metres. Parts of the ...
(south) (193 m), (
Bickerton)
*
Maiden Castle (210 m), (
Bickerton &
Duckington
Duckington is a small village and civil parish in the unitary authority of Cheshire West and Chester and the ceremonial county of Cheshire, England. It is situated some 10½ miles (17 km) south-east of Chester, 10 miles (16 km) east o ...
)
Geology
The hills are composed of a range of
sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks.
Most sandstone is composed of quartz or feldspar (both silicates) ...
s of
Permian
The Permian ( ) is a geologic period and stratigraphic system which spans 47 million years from the end of the Carboniferous Period million years ago (Mya), to the beginning of the Triassic Period 251.9 Mya. It is the last period of the Paleoz ...
and
Triassic
The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period ...
age. North–south faulting is in part responsible for elevating harder-wearing strata above the general level of the
Cheshire Plain. Typically the higher summits are formed from the Helsby Sandstone.
The ridge acted as something of a barrier to the passage of
Irish Sea
The Irish Sea or , gv, Y Keayn Yernagh, sco, Erse Sie, gd, Muir Èireann , Ulster-Scots: ''Airish Sea'', cy, Môr Iwerddon . is an extensive body of water that separates the islands of Ireland and Great Britain. It is linked to the Ce ...
ice during the last
ice age
An ice age is a long period of reduction in the temperature of Earth's surface and atmosphere, resulting in the presence or expansion of continental and polar ice sheets and alpine glaciers. Earth's climate alternates between ice ages and gree ...
and its hills are etched with numerous glacial
meltwater channels, many of which formed subglacially. Particularly spectacular examples are those at Urchin's Kitchen in Primrosehill Woods and at Holbitch Slack near Cotebrook.
[British Geological Survey 1:50K map sheets 97, 109, 122]
Hill forts
A series of
Iron Age
The Iron Age is the final epoch of the three-age division of the prehistory and protohistory of humanity. It was preceded by the Stone Age (Paleolithic, Mesolithic, Neolithic) and the Bronze Age (Chalcolithic). The concept has been mostly appl ...
hill fort
A hillfort is a type of earthwork used as a fortified refuge or defended settlement, located to exploit a rise in elevation for defensive advantage. They are typically European and of the Bronze Age or Iron Age. Some were used in the post-Roma ...
s adorn the ridge from Woodhouse Hill and
Helsby Hill in the north through
Eddisbury and
Kelsborrow Castle
Kelsborrow Castle is an Iron Age hill fort in Cheshire, northern England. Hill forts were fortified hill-top settlements constructed across Britain during the Iron Age. It is one of only seven hill forts in the county of Cheshire and was probabl ...
to
Maiden Castle in the south.
Recreation
The ridge is traversed by the popular
Sandstone Trail
The Sandstone Trail is a long-distance walkers' path, following sandstone ridges running north–south from Frodsham in central Cheshire to Whitchurch just over the Shropshire border. The path was created in 1974 and extended in the 1990s. ...
, a middle-distance
recreational route originally established by the former
Cheshire County Council between Beacon Hill and Grindley Brook on the
Shropshire
Shropshire (; alternatively Salop; abbreviated in print only as Shrops; demonym Salopian ) is a landlocked historic county in the West Midlands region of England. It is bordered by Wales to the west and the English counties of Cheshire to th ...
border but now extended into
Frodsham to the north and
Whitchurch to the south. Sections of the
Delamere Way,
Longster Trail
The Longster Trail is a waymarked footpath in Cheshire, England. It runs for from the summit of Helsby Hill, Helsby, to the village of Piper's Ash, Chester, passing through Alvanley, Manley, Cheshire, Manley, Barrow, Cheshire, Barrow, and Guild ...
and
Eddisbury Way also explore parts of the ridge.
Numerous of the woods along the ridge have been used for
orienteering
Orienteering is a group of sports that require navigational skills using a map and compass to navigate from point to point in diverse and usually unfamiliar terrain whilst moving at speed. Participants are given a topographical map, usually a s ...
competitions over the years. Horseriding is also popular in the area, as it is traversed by a number of
bridleway
A bridle path, also bridleway, equestrian trail, horse riding path, ride, bridle road, or horse trail, is a trail or a thoroughfare that is used by people riding horses, riding on horses. Trails originally created for use by horses often now s ...
s, byways and green lanes.
See also
*
Geology of Alderley Edge
One of the classic locations for the study of Triassic sandstones in the UK is at Alderley Edge in Cheshire. Numerous scientists from the early 19th century up to the present day have studied the area and it is a popular field site for universit ...
References
{{GeoGroup
Valleys of Cheshire
Geology of Cheshire
Hills of Cheshire
Ridges of England