t
The Group's aim is to identify, survey, protect and promote geological and geomorphological sites in the former County of Avon - the modern unitary authorities of Bath and North East Somerset, Bristol, North Somerset and South Gloucestershire. RIGS are selected for their educational, research, historical and aesthetic value.

Showing posts with label Local groups. Show all posts
Showing posts with label Local groups. Show all posts

Tuesday, 14 May 2013

RIGS of the month [May] - Troopers Hill, Bristol


RIGS of the Month - May
Troopers Hill, Bristol
Fig. 1: Location of Troopers Hill, St George, Bristol. Postcode BS5 8BL.

SITE SPECIFIC INFORMATION 
Location: BS5 8BL
Accessibility: The entrance at Malvern Road provides the easiest access for those with limited mobility. Some of the slopes on this path may mean that some wheelchair users need assistance. The remainder of the paths on the hill are unsurfaced.
Topography: Hilly, grassed footpaths
Restrictions: Troopers Hill is owned and managed by Bristol City Council, there is free unrestricted access.


This article has been adapted from Andrew's post on the Friends of Troopers Hill website - the original version can be accessed here and includes a detailed stratigraphic log. Eilene Stonebridge also contributed a great deal of material to the site (see section on geology) and wrote an accompanying leaflet which can be downloaded for free - link at the bottom of this post.

Introduction
Troopers Hill’s geology is unusual in Bristol. Much of the city lies on Carboniferous Limestone, but Troopers Hill is dominated by sandstone of the Pennant Measures which are sedimentary rocks formed in tropical swamps some 300 million years ago. In places, the sandstone can be seen on the surface, both as natural outcrops and old quarry faces.

The combination of sandstone and local industry has resulted in acid soils, which are rare in Bristol. This has encouraged a wealth of plants to flourish, that are found nowhere else in the City.

Much of the shape of the hill is the result of quarrying for the sandstone which was used as building stone throughout Bristol. The largest quarry was the gully in the centre of the hill which was worked until the end of the nineteenth centuary. The humps and bumps above Troopers Hill Rd are where the unsuitable stone was tipped.

As well as sandstones the Pennant Measures include mudstones, shales, clay and coal seams. In the past coal has been dug where it outcroped on the hill and both fireclay and coal have been taken from deep mines under the hill.
 
History
Troopers Hill is made up of a thick pile of layers of rock which must have been
well known to the generations of miners and quarrymen who extracted coal, fireclay and sandstone from them for centuries. However, much of that knowledge has been lost and no one now is quite sure what lies under the hill.

There are at least 9 coal seams there and some of these were exposed at the surface. Local geologist Tom Fry recalled one seam 5-6ft. thick revealed on the west side of the hill in 1968, but all the other seams are probably much thinner. He also remembered that a very thin seam was worked by unemployed
men in 1913 on the hill near the bottom of Troopers Hill Road, where sadly a friend of his died after the shaft collapsed.
 

The rocks are sandstone, mudstone, coal and clay, and they all dip to the south at between 25 and 45 degrees. They belong to the Upper Carboniferous Coal Measures, and are near the base of the Pennant Sandstone. The rock types, structures and fossils suggest that they were formed when the area was covered by a forested swamp. At this time (about 300 million years ago) the area is thought to have been near the equator with a tropical climate. The rocks were next squeezed by huge forces, which crumpled them into a large arched fold that runs east-west through Kingswood. The Trooper's Hill rocks lie on the south side of this structure. 

Pennant Sandstone
The sandstone at Troopers Hill is called Pennant, since the early geologists took the name traditionally used by miners and quarrymen. The Pennant forms a thick mass of sandstone in the middle of the local Coal Measures around Bristol, as well as in the Forest of Dean and South Wales. The name is thought to have been derived from the Welsh words penn and nant, meaning head of the valley.The rock is well exposed in the Gully Quarry, just south of Trooper's Hill chimney.

The sandstones exposed on the north side of the Gully display cross bedding, indicating that the original sand grains were carried by running water in rivers. 

On the south of the Gully the rocks are coarser grained with coal pebbles and fossil imprints of tree trunks, suggesting that at times the water was flowing fast enough to erode sediment and move large pieces of wood.


 
Fossilised wood in Pennant Sandstone. Photo credit: Steve England
Pennant was quarried at many sites in the local coalfields and provided stone for thousands of buildings, including the chimney at the top of Trooper's Hill. It sometimes splits into thin slabs which were much used for paving, kerbs, steps, gravestones, and, in earlier times, for roofing.

Mudstone
The mudstones were known as duns by the miners. They are less well exposed but can be seen in the paths to the south of Troopers Hill, and they indicate a period when the waters in the swamps must have been still. They had no commercial value. 

Coal 
The miners called the coal seams “veins” and gave them names which were used at each pit in the area where they were found, from Newton St Loe, near Bath, to St Phillips Marsh, in Bristol. Some seams thinned to nothing and others split, which made the naming uncertain in places. Each seam is thought to be the compressed remains of deposits of peat, built up from the remains of the trees of the forest. 

Crewe's Hole Pit was sited at the south end of Troopers Hill, and is marked by the remains of he chimney of the mine engine house. Air Balloon Pit was next to Air Balloon Road, about half a mile north of the Hill. The mining geologist John Anstie was employed to gather information on all the local coal mines for the Royal Commission on Coal. He collected some details of what had been found in these pits, although both were disused when he visited the area in about 1870 and he was concerned that the information might not be completely reliable. He also observed that “the outcrops of the Devil's seam, Buff and Parrot seams, follow parallel lines about 500 yards to the north of those of the Millgrit and Rag seams ... (and at) ..Trooper's Hill .. the shallow works on all of them are clearly traceable.” He noted that the Air Balloon Pit only worked for three or four years as the seams were too variable to be worked economically. 

The engine house in Troopers Hill Rd, c. 1914. Reproduced by kind permission of the Bristol Reference Library.

Tom Fry was brought up near Troopers Hill and knew the area very well. He recalled one seam 5-6ft. thick revealed on the west side of the hill in 1968 before the council used the area as a rubbish tip. Tom recalled that in around 1910, his father used to warn him of the dangers of the hill, telling him that it was all undermined. His father worked in the Fireclay Mine. Tom also recalled the collapse of an old sloping shaft in the floor of the main quarry, the sides of which had been walled with mortared stone, and that he could trace the sites of at least six shallow mines on the Hill.

Fireclay
Fireclay is usually found beneath a coal seam and is basically the clay soil where the trees grew which provided the peat deposits. Fireclay is rich in clay minerals which means that when fired into bricks or tiles, they can withstand high heat. Tom Fry noted that the Troopers Hill fireclay was used to produce high quality terra cotta tiles that were used in many local buildings. 

Three fireclay beds are known to have been worked beneath Trooper's Hill. 
 

Andrew Mathieson

Further reading
Downloadable leaflets on the geology, wildlife and history of Troopers Hill are available at http://www.troopers-hill.org.uk/leaflets/index.htm


December 2016 Update.

Eileen Stonebridge and Andrew Mathieson, of The Avon RIGS Group, have been working for some time with The Friends of Troopers Hill on the interpretation boards in general and the Geological interpretation board in particular. This new board can be seen near the Upper Chimney.

The four boards can be seen on this page of the Troopers Hill web site:-




References
Anstie, 1873, The Coalfields of Gloucestershire and Somersetshire, London
Bristol Fireclay Company Co Ltd, 1911, Section of the Mines at Troopers Hill
British Geological Survey 6 inch map Sheet ST 67 SW
Buckland and Conybeare, 1824, Transactions of the Geological Society of London (available online through Google Books)
Cornwell, 2003, The Bristol Coalfield, Landmark Publishing
Fry, Accounts of my Earliest Years (up to 1922) www.troopers-hill.org.uk/memories
Kellaway and Welch, 1993, Geology of the Bristol District, HMSO
Prestwich, 1871, Report of the Royal Commission on Coal (in) Gloucestershire and Somersetshire, HMSO (available online through Google Books)

The original walk was funded by our Stepping Forward Sustainability Grant, through the BIG Lottery Community Spaces Programme www.troopers-hill.org.uk/steppingforward


Tuesday, 5 February 2013

Geo-gardening at Trendlewood Quarry, Nailsea


Geo-gardening - Sunday 3rd February 2013

On Sunday 3rd February 2013 a Joint Gardening Force (JGF) from Friends of Trendlewood Park (FoTP) and Avon RIGS Group descended on Trendlewood Quarry in Nailsea and proceeded to spend a few hours clearing ivy and other encroaching vegetation from the lower parts of the quarry face in three areas.

Before worked started. Photo credits: Richard Kefford. More photos at
These three areas were selected to demonstrate the differing bedding types – from varves to massive -  in this Pennant Sandstone of the Downend Formation and the differing types of deposition – point bars and channel deposits.


Geo-gardeners at work

This is the first part of the implementation of the quarry management plan that was agreed at a site meeting between N Somerset Council, Friends of Trendlewood Park and Avon RIGS Group. The second part which will be carried out by the N Somerset Green Team will consist of clearing the upper levels of the face and removing a few selected trees that are in danger of falling and have extended their roots into the joints and fissures rock close to the face and so are damaging the exposure.


Meeting one of the site natives



See here for details of the geology of this site and its location.

A cleared area on one face
Richard Kefford




Friday, 7 September 2012

Nailsea Environmental & Archaeological Team – NEAT

Nailsea Environmental & Archaeological Team





NEAT - Aims and Objectives

Nailsea Environmental & Archaeological Team – NEAT, was set up in September 2004 to undertake archaeological research in the Nailsea area, including Tickenham, Wraxall, Backwell, Chelvey and Brockley.
     Our aim is to carry out fieldwork to find new archaeological sites, record existing sites and to augment the North Somerset Historical Environment Record, in conjunction with the County Archaeologist. 

     The methods used include land survey, geophysical survey, map regression and reference to local archives and involve work with other similar groups in North Somerset. 

     In addition, NEAT has carried out a survey of dry stone walls in Nailsea, recorded the age of buildings and recorded the hedges in the area. There is research ongoing into other aspects of our local environment. 

     During 2011 NEAT established a geology group with the initial aim of establishing ‘geotrails’ around the area to show and explain the local geology. It is intended to complete the geotrails project and publish a guidebook in 2012.

     There is a live link to the NEAT web site in the right hand column on this blog home page.

David Sowdon

Thursday, 26 July 2012

Geology in the West Country blog

Have you visited the Geology in the West Country blog?

This blog's main purpose is to publicise talks, field trips and events organised by West Country geological organisations. It also includes links to blogs and webpages of similar groups from around the UK. Discussion is encouraged and anything of general geological interest is included. Latest stories include Rock Circus in Box takes shape and Chemical ghost of 120million years-old bird.




There is a live link to the Geology in the West Country on the Outcrop homepage so that you can keep up to date with what is happening in our region.


Friday, 6 July 2012

Avon Wildlife Trust

In the first of a new series, we catch up with local groups who are involved in geoconservation in the Avon region. First up, Avon Wildlife Trust.


From belemnites & brachiopods to bats & bullfinches...

Avon Wildlife Trust is committed to working for people and wildlife in the local area, and we manage 35 nature reserves, some of which are also sites with outstanding geological features. One reserve which has been at the centre of our recent 'Bats for Bath' project is Brown's Folly.

Brown's Folly, Bathford. Photo credit: Avon WT
Browns Folly Nature Reserve is a Special Area of Conservation (SAC) and Site of Special Scientific Interest (SSSI) that has rare calcareous grassland habitats, unique geology, ancient woodland and a cave system with fantastic bat populations, with 12 of Britain’s 18 Bat species having been recorded here.  The caves are the remnants from mining the local oolitic limestone which was extracted for building material, and which is known locally as 'Bath Stone'. Oolitic limestone gets its name from the spherical particles or 'ooids' it contains. This word comes  from the Greek word for 'egg' because ooids are thought to resemble fish eggs. You can see fossils  in the exposed stone - thick shelled bivalves such as Trigonia, found today in the Pacific, along with brachiopods, ammonites and belemnites which once swam in the sea which covered this area 170 million years ago.

Oolitic limestone hand specimen (left) and thin section (right). Photo credit: http://www.earthscienceeducation.com

The stone was used for building in Roman times, but intensive mining of the limestone beds in the valley was carried  out from the 17th to the early 20th century. The characteristic stone was used for the construction of most of Bath's famous buildings, as well as Buckingham Palace and many stately homes across the country. The different mines, which were driven in to the rock in the  area, stretched for many miles and contained stables, cart-roads and tramways. Stone was extracted by the 'room and pillar' method, by which chambers were mined, leaving pillars of stone to support the roof.  By the time the mines closed down in 1930 there were over 300 acres of interconnecting underground workings and tunnels, which were used for storing ammunition and government  records during the Second World War.

Bats are very fussy about their roosting sites - they need somewhere with stable temperature and ventilation levels, and the old mine tunnels under the woodland seem to suit them very well. The huge size of the mines means that areas deep down are less affected by outside variations in climate - a perfect spot to hibernate for the winter months. The Trust has installed bat grilles on the entrances of the mines in the woodland to make sure that the bats remain at peace within their hilly homes. Bats are protected by law, and the grilles also prevent access to the mines - protection for people as well as preserving peace for the bats. In spring and summer when the bats awake and come out to feed at dusk, the grassland glades of the reserve are rich with insects right on their doorstep.

Greater horseshoe bat - just one of the twelve species recorded in the caves at Brown's Folly. Photo credit: Avon WT
Brown's Folly in Bathford is one of our most popular reserves that receives around 5000 visitors each year with most people enjoying the fantastic views from the grassland plateau across to Bath and the surrounding area, and talking long walks through the ancient woodland full of rocky fissures, giant veteran trees, mosses and ferns, and open glades that all help support the bats roosting in the caves.

You can read more about Brown's Folly and other Trust nature reserves here.

Pat Ellingham
(Avon WT Director of Communications and Development)


Look out for more information on the geology of Brown's Folly - it is soon set  to feature on the blog as a RIGS of the Month.