Roche Rock and the Tresayes Trail - Cornwall Wildlife Trust
Roche Rock and the Tresayes Trail - Cornwall Wildlife Trust
Roche Rock and the Tresayes Trail - Cornwall Wildlife Trust
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Carolina Galindo HernándezProfessional Experience2004- Present Assistant Professor, School of Human Sciences, Universidad del Rosario.2002- 2004 Instructor, School of Human Sciences, Universidad del Rosario.2002- 2005 Lecturer, Department of Political Sciences, Universidad de los Andes.2002 Lecturer, Department of Political Sciences, Universidad Nacional de Colombia.1998- 2002 Instructor, Department of Political Science, Pontificia Universidad Javeriana.EducationPh.D. C<strong>and</strong>idate, Political Science, Berlin Graduate School of Social Sciences- Humboldt University.M.A., Philosophy, Pontificia Universidad Javeriana. Degree Awarded with Honors.B.A., Sociology, Universidad Nacional de Colombia.Teaching <strong>and</strong> Research InterestsDemocratization, Latin American Politics, State-Society Relations, Citizenship, PoliticalSociology, Political Philosophy.PublicationsBOOKS2009 Chaparro Amaya, Adolfo <strong>and</strong> Carolina Galindo Hernández. Génesis y transformaciones del Estadonación en Colombia. Una mirada topológica a los estudios sociales desde la Filosofía Política. Bogotá: CentroEditorial de la Universidad del Rosario.2008 Chaparro Amaya, Adolfo; Carolina Galindo Hernández <strong>and</strong> Anne- Marie Sallenave (Eds.)Estado, Democracia y Populismo en América Latina. Buenos Aires/Bogotá: ConsejoLatinoamericano de Ciencias Sociales - Centro Editorial de la Universidad del Rosario.1
400400wordsmillion yearsof <strong>Roche</strong> – in about& a few pictures!Around 400 million years ago this was all a shallow sea.Strange creatures lived in <strong>Roche</strong>! But of course <strong>Roche</strong>,<strong>and</strong> <strong>Cornwall</strong>, <strong>and</strong> <strong>the</strong> world looked very different.You would not have been able to recognise today’scontinents. Some have been made of bits <strong>and</strong> piecesof earlier continents, <strong>and</strong> anyway <strong>the</strong>y have driftedall over <strong>the</strong> place in <strong>the</strong> last 400 million years.S<strong>and</strong> <strong>and</strong> mud were eroded off <strong>the</strong>se old continents <strong>and</strong> dumpedon <strong>the</strong> sea-bed. Then we were in <strong>the</strong> middle of a slow-speed shuntbetween Africa <strong>and</strong> Europe which crumpled <strong>the</strong> new layers ofs<strong>and</strong> <strong>and</strong> mud. Slow speed? These old continents came toge<strong>the</strong>rat <strong>the</strong> stately pace of about 1 centimetre a year. That’s about<strong>the</strong> rate your fingernails grow. But imagine growing your fingernails for a million years – <strong>the</strong>y’d be ten kilometres long: no needfor extensions!The crumpled rocks made a mountain chain. Deep beneath <strong>the</strong>mountains some of <strong>the</strong> rock melted – <strong>and</strong> molten blobs popped up(like a ‘lava lamp’) <strong>and</strong> <strong>the</strong>n solidified as granite a few kilometresbelow <strong>the</strong> ground surface. All sort of o<strong>the</strong>r rocks – with strangenames - were formed: pegmatite, greisen, schorl, spotted slate, calcflinta,china clay – <strong>and</strong> ores of metals like tin, tungsten, iron, nickel<strong>and</strong> uranium. The mountains were worn down – strange reptileswalked <strong>the</strong> hot dry plains. Did dinosaurs ramblethrough <strong>Roche</strong>? They’d have been way aboveour heads! Several thous<strong>and</strong> metresof rock has been eroded since <strong>the</strong>dinosaurs roamed.Tin OreAbout 50 million years ago <strong>the</strong>climate was warm <strong>and</strong> wet, <strong>and</strong>probably a lot more feldspar rottedto form china clay (kaolin). In fact <strong>the</strong>whole of <strong>the</strong> granite,<strong>and</strong> <strong>the</strong> slate around it,was wea<strong>the</strong>red to quitea depth. Then in <strong>the</strong> Ice Age of <strong>the</strong> lastcouple of million years rapid erosionstripped off this material to leave tors –like Helman Tor <strong>and</strong> <strong>Roche</strong> <strong>Rock</strong>. Therewere no glaciers here but <strong>the</strong> conditionschanged from arctic – for ten of thous<strong>and</strong>sof years – to pleasantly warm,several times. Today we are living in a‘pleasantly warm’ time. In arctic times <strong>Roche</strong>would have been like Siberia today but probablywith <strong>the</strong> odd herd of mammoths.Unwea<strong>the</strong>redGraniteDid woolly mammoths once grazewhere cows <strong>and</strong> sheep do now?The last glacial period ended about twelve thous<strong>and</strong> years ago. Since <strong>the</strong>n we’vechanged <strong>the</strong> area a great deal. Cleared <strong>the</strong> l<strong>and</strong> <strong>and</strong> farmed. Built houses, churches,chapels, schools <strong>and</strong> factories. Dug up metal ores, <strong>and</strong> dug up china clay.It’s all written into <strong>the</strong> l<strong>and</strong>scape.5<strong>Roche</strong>5TTrezaise ChapelPSt Gomonda ChurchThis air photo was taken in 1995– what changes have taken placesince <strong>the</strong>n?- What changes may take placein <strong>the</strong> next hundred years?- Ano<strong>the</strong>r ten thous<strong>and</strong>?- Will it be warmer - or will <strong>the</strong>rebe an Ice Age?- Ano<strong>the</strong>r few million?Probably humans will have become extinctby <strong>the</strong>n! What sort of planet will we leave?<strong>Roche</strong> <strong>Rock</strong>Medieval Fields<strong>Tresayes</strong> Quarry1907Prosper TipCarbis Brickworks
<strong>Roche</strong> <strong>Rock</strong>& <strong>the</strong> <strong>Tresayes</strong> <strong>Trail</strong>You can start this trail ei<strong>the</strong>r from <strong>the</strong><strong>Roche</strong> <strong>Rock</strong> or from <strong>Tresayes</strong> Quarry.Part of <strong>the</strong> route is across fields <strong>and</strong> canbe muddy. There are also stiles to cross.Key - P Space to park a car T Toilets 5 Public HouseRoute + Route<strong>Roche</strong> <strong>Rock</strong> 1 has been written about for at<strong>Roche</strong>least four<strong>Rock</strong>centuries,1 has been<strong>and</strong> beenwrittendescribedabout forinatleastmanyfourways!centuries,“Craggy<strong>and</strong>ponderousbeen describedstones”,in“Amanyverie high,ways!steepe“Craggy<strong>and</strong>ponderouscraggie rocke”,stones”,<strong>and</strong> even“Averielikenedhigh,to asteepehuge<strong>and</strong>molarcraggie<strong>and</strong> anrocke”,upturned<strong>and</strong>bunchevenlikenedof bananas.to aIt’shugemademolarof two<strong>and</strong>veryan upturnedtough minerals,bunchofquartzbananas.<strong>and</strong> tourmaline,It’s made ofwhichtwo veryis whytoughitminerals,sticksquartzup. The<strong>and</strong>chapeltourmaline,was dedicatedwhich istowhySt Michaelit sticksinup.1409,Thebutchapelhas beenwasadedicatedruin sinceto<strong>the</strong>SteighteenthMichaelincentury.1409,Thebut hasrarebeenTunbridgea ruinfilmysincefern<strong>the</strong>grows ineighteenthshady placescentury.on <strong>the</strong>The<strong>Rock</strong>,rare<strong>and</strong>Tunbridgea wide rangefilmyoffernplantsgrows<strong>and</strong>inanimalsshadyliveplacesin <strong>the</strong>onheathl<strong>and</strong>around<strong>the</strong><strong>Rock</strong>, <strong>and</strong> a wide<strong>the</strong> rocks.rangeof plants <strong>and</strong> animalslive in <strong>the</strong> heathl<strong>and</strong>around <strong>the</strong> rocks.Tunbridgefilmy fern8TCemetery9P119071020052Follow one of <strong>the</strong> many pathsaround <strong>the</strong> <strong>Rock</strong> <strong>and</strong> <strong>the</strong>n <strong>the</strong>signposted footpath.76PThe name Hendra 2 has been found back to1270: it signifies a permanent farm, withbuildings (ra<strong>the</strong>r than a temporary place for ashepherd to sleep in near his flocks). Hendrevighan is mentioned in a document of 1302 –Little Hendra. The ruin beside <strong>the</strong> track wasonce a cottage.3At <strong>the</strong> tarmac road turn left until it ends,<strong>the</strong>n follow <strong>the</strong> track to <strong>the</strong> right, gentlyuphill to <strong>the</strong> nature reserve.The scrubby area 3 in <strong>the</strong> shallow valley is nowcalled Stennacks which means tinworks, but in<strong>the</strong> 19th century it was called Stennack Ladron– Thieves’ Tinworks. The s<strong>and</strong>s <strong>and</strong> gravels in<strong>the</strong> valley bottom were turned over for tinstone,leaving <strong>the</strong> characteristic l<strong>and</strong>scape of ridges<strong>and</strong> troughs, bumps <strong>and</strong> pools – as you cansee in <strong>the</strong> air photo.<strong>Tresayes</strong> Quarry 4 had twoquite different products at different times. Thequarry is mostly known for its very long feldsparcrystals. The rock was quarried <strong>the</strong>n <strong>the</strong> feldsparh<strong>and</strong>-picked by women – balmaidens –Long-tailed tit4 5using hammers. At one stage <strong>the</strong> quarried rockwas loaded into wagons, sent down a tramway<strong>and</strong> <strong>the</strong>n tipped down to women working inopen sheds below. The feldspar was worked on<strong>and</strong> off in <strong>the</strong> 19th century with short re-openingsin both world wars. The material was used inglazes, glass <strong>and</strong> porcelain. In <strong>the</strong> 20th century avery hard rock (like <strong>Roche</strong> <strong>Rock</strong>) was quarriedfor roadstone but this quarry is now under<strong>the</strong> tips 5 of Wheal Prosper clayworks, while evidence for <strong>the</strong>rock crushers, stock piles <strong>and</strong>waste tips is now hiddenunder <strong>the</strong> vegetation beside<strong>the</strong> track. The rock wascalled blue elvan by <strong>the</strong>Feldspar quarrymen, but this nameis also used in <strong>Cornwall</strong>for ‘greenstone’, which isusually a dolerite, a quitedifferent rock.The quarry is now a naturereserve with willow cloaked inlichens <strong>and</strong> ferns <strong>and</strong> mosses.On <strong>the</strong> dryer part you will findhea<strong>the</strong>rs <strong>and</strong> o<strong>the</strong>r wild flowers.Many birds find shelter <strong>and</strong> food in <strong>the</strong> willows.<strong>Cornwall</strong> <strong>Wildlife</strong> <strong>Trust</strong> pays one peppercornper year as rent to Goonvean – a bargain!The place-name <strong>Tresayes</strong> has been tracedback to 1260 – when it was spelt Treseis. Seiswas probably a person’s name, so Treseismeans ‘The farm belonging to Seis’. Today<strong>the</strong>re are several ways of spelling <strong>Tresayes</strong>.Seis would probably be quite at home in <strong>the</strong>flower-rich heathl<strong>and</strong> around <strong>the</strong> <strong>Rock</strong>: it hasnot changed much in a thous<strong>and</strong> years, buthis animals would have kept <strong>the</strong> gorse,bracken <strong>and</strong> brambles down!Retrace your steps back to <strong>the</strong> road, <strong>and</strong>continue towards <strong>the</strong> main road until justpast a farmyard - <strong>the</strong>n look back!The end wall of <strong>the</strong> barn 6 has an amazingcollection of <strong>the</strong> local stones – all <strong>the</strong> rocks in<strong>the</strong> neighbourhood are here: different granites,quartz-tourmaline rock (‘schorl’, or ‘blue elvan’to <strong>the</strong> quarrymen), killas (baked slates), ‘sparstone’(quartz), <strong>and</strong> more.Continue to <strong>the</strong> endof <strong>the</strong> road.Trezaise Chapel 7 wasbuilt in 1883 but incorporates anearlier building’s dedication stone. TheBible Christians broke away from <strong>the</strong> WesleyanMethodists, but later rejoined. Beside <strong>the</strong> mainentrance is some fancy carving in a limestone,brought in from around Bath. John Wesleyvisited <strong>Roche</strong> in 1768.Opposite <strong>the</strong> chapel is amodern Cornish hedgemade of Cornish Stone,brought in from a quarryat St Issey or Liskeard orsomewhere. Certainly <strong>the</strong>reis no stone like it found in <strong>the</strong>area. Using waste rock from <strong>the</strong>claypits would have been more in character.At <strong>the</strong> top of <strong>the</strong> hedge is some zig-zag work– Jack <strong>and</strong> Jills, or curzey-way – commonlyseen in North <strong>Cornwall</strong>.You can ei<strong>the</strong>r turn back down ProsperRoad <strong>and</strong> <strong>the</strong>n go down <strong>the</strong> track <strong>and</strong>across <strong>the</strong> fields to <strong>the</strong> <strong>Rock</strong>, or follow <strong>the</strong>main road back, past <strong>the</strong> new cemetery to<strong>the</strong> parish church <strong>and</strong> on to <strong>the</strong> <strong>Rock</strong>.The church 8 is dedicated toSt Gomonda. It was rebuilt twice in<strong>the</strong> nineteenth century but at least<strong>the</strong> Norman font of Pentewan stonesurvives. There are similar fonts inBodmin <strong>and</strong> St Austell parish churches. In<strong>the</strong> churchyard <strong>the</strong>re’s an unusual medievalcross <strong>and</strong> some fine carved slate tombstones.The walls of <strong>the</strong> church are made of blocksboth of granite <strong>and</strong> of darker schorl – <strong>the</strong>quartz-tourmaline rock which makes up <strong>the</strong><strong>Rock</strong>: can you tell which is which?Neolithic pottery was found under <strong>the</strong> newhousing estate 9, so <strong>Roche</strong> has beeninhabited for at least five thous<strong>and</strong> years.A short drive down <strong>the</strong> road towards Bugle, <strong>and</strong><strong>the</strong> mostly off-road Clay <strong>Trail</strong>s, is CarbisBrickworks. There’s no pavement so best notto walk down <strong>the</strong> road, but you could followa footpath downhill from Hendra.Carbis brickworks 10 is on private propertybut you can see <strong>the</strong> kilns <strong>and</strong> chimney stackfrom <strong>the</strong> road. It produced bricks for furnaces,calciners, smelting houses <strong>and</strong> foundries. Youcan also find white bricks stamped CARBIS usedin more humdrum situations. On both sidesare old clay dries, converted for modern uses.