Tag Archives: landscapes

The Tinners Way – An Old Track Through Time.

In the far west of Cornwall lies a trackway that has been trodden by many feet over many millennia.  Once a central part of a wider network of tracks it is now only used by ramblers, dog walkers, horse riders and those interested in the sites along its way.  What it was called in the past is unknown but today it has become known as the Tinners Way.

Paths and tracks traverse the landscape creating a maze of possible routes from A to B and are probably one of the least understood aspects of the past in Britain.  The greatest issue is in the understanding of the chronology of this particular site type.

“Unmetalled roads and trackways are extremely difficult to date.  They have no constructional material to aid interpretation and artefacts are rarely present.  This difficulty is compounded by the fact that their form has remained unchanged from prehistoric to modern times and that many were in continuous use for centuries, even millennia” (Prehistoric Roads, Trackways and Canals – Historic England 2011)

Historic England/English Heritage have defined a trackway as a ‘linear route which has been marked on the ground surface over time by the passage of traffic.  Trackways are usually relatively short routes for local use’.   In west Cornwall the Tinners Way has been identified as one such trackway, one which in all likelihood has a lengthy history going back into prehistory.  It follows the granite backbone of West Penwith passing by and sometimes through archaeological sites as well as the remains of later of tin mining.

So, from where does the Tinners Way begin and where does it end?  Well the answer to that would very much depend on from what direction you are coming as it travels between Cape Cornwall and St Ives.  For our purposes here we will begin at Cape Cornwall in the very far west, stopping at various points and ending up on the  Island in St Ives.

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Kenidjack Valley with Cape Cornwall in the background – photo by Tony Aitkin (geograph.co.uk)

It is probable that the Kenidjack Valley which runs alongside the Cape was the source of one of the earliest and most accessible deposits of alluvial tin ore.  Tin was an important resource to the Cornish economy from the Bronze Age into the 19th century. 

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The bracken covered sides of Kenidjack Valley hide the remains of alluvial mining.

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A view of one of the trio of stone circles known as the Tregeseal stone circles with Carn Kenidjack in the background.

 

From here the trackway heads inland and up onto the moors of Penwith past Carn Kenidjack and the Tregeseal Stone Circles not to mention the mysterious holed stones.   Continuing on to the fascinating sites of Chun Quoit and Chun Castle.

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Chun Quoit – drawing by William Copeland Borlase 1872

Back long before metals were exploited in Cornwall our Neolithic  ancestors built great stone tombs, archaeologically these are known as quoits or chambered cairns.  Although this is not the place to go into a lengthy discussion on the function of such sites it should be pointed out that many of these sites do seem to appear in significant places in the landscape and thus would seem to have a function beyond simple burial.  Along the Tinners Way there are several quoits which serve to mark the way – Zennor Quoit, Mulfra Quoit, and of course Chun Quoit with the possibility of more having been ravaged by time.

Just past Chun Quoit are the remains of what was once a great stone walled hillfort – Chun Castle.  The walls are still impressive even after the attempts at removal for use in other building projects (the pavement on Market Jew St in Penzance is made up of stone from the hillfort).  Originally occupied in the Iron Age it straddles the trackway, interestingly it was later occupied in the 5th and 6th centuries – a time of unease – and the evidence does seem to suggest it was used as a stronghold for the storage of tin ore.

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Plan drawing of Chun Castle by Charles Knight 1845.

 

 

 

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The imposing gateway of Chun Castle – photo by Rod Allday (geograph.co.u

 

All along the Tinners Way there is evidence of tin mining (hence the name) – old mine shafts can be a hazard for those wandering off the beaten track (please remember to keep your dogs under control when walking along here).  Much of the visible mining remains date from the 17th to the 19th centuries.

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The pumping engine house over the Greenbarrow shaft of Wheal Malkin often referred to as Ding Dong Mine – photo by Rod Allday (geograph.co.uk)

On leaving Chun Castle you pass the overgrown Iron Age courtyard house settlement of Bosullow Trehyllys – see an earlier article on the more well known courtyard house settlements of Chysauster and Carn Euny.  From here the trackway follows the well trod path past the Men-an-Tol and Men Scryfa.

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Men-an-Tol – the moorland behind is covered in disused mining shafts.  In the far distance is the abovementioned pumphouse of Ding Dong Mine.

The first was probably once a chambered tomb which has suffered at the hands of people over a very long time.  The latter an inscribed stone dating to the 5th/6th century and is a memorial stone to “Rialobrani Cunovali Fili’ – roughly translated as ‘the royal raven son of the glorious prince’.  It’s position along this important route undoubtedly deliberate.

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The Men Scryfa Stone – photo by Jim Champion (geograph.co.uk)

Not far from Men Scryfa is the Four Parish Stone.  This stone indicates the point in which the boundaries of the four ancient parishes of Zennor, Gulval, Madron and Morvah meet.  This is not the modern civil parish boundaries but the much older church boundaries.  A document from the 17th century mentions this place in the landscape, referring to it as ‘Meane Crouse’ or ‘stone cross’ suggesting the presence of a stone cross which marked this important crossroads.  Any traveller to Cornwall will note how stone crosses covered in moss and worn by weather are often found at road junctions.

From here the landscape is dominated by the impressive tor known as Carn Galva and whilst not the highest point in West Penwith (Watch Croft the adjacent tor takes that accolade) it is the most atmospheric of tors with its giant granite boulders standing silent sentinel over the millennia.  It is now generally believed that Carn Galva is one of the few Neolithic enclosures to be found in Cornwall – Carn Brea, Helman Tor and Trencrom are the more well known.

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One of the many remains of roundhouses to be found at Bodrifty – behind can be seen the high ground leading to Zennor Hill and Carn Glava. Photo by Alan Simkins (geograph.co.uk)

Further on the walker can take a minor side trip to see the Nine Maidens stone circle and the remains of a roundhouse settlement probably dating to the late Bronze Age/early Iron Age (Bodrifty).  Nearby the farmer at Bodrifty Farm has recreated a roundhouse and it is possible to visit but do ask first.  After Bodrifty the trackway goes past Mulfra Quoit.

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Mulfra Quoit – drawing by William Borlase 1769.

Alternatively and the most likely direction for the trackway to follow is across the moorland of Bosporthennis Common between the highpoint of The Beacon and Mulfra Hill to the parish boundary stone known as the Bishops Head and Foot.

“Used over generations, these trackways created permanent scars across hills and valleys, and formed a web of easily followed routes which were later utilised to mark the extent of private estates which had superseded previous communal use of tribal lands.  When the system of parishes was established about the 12th century additional use was made of these muddy tracks to form their boundaries in conjunction with streams and prominent rocks” (Antiquities of West Cornwall – The Tinners Way.  Ian Cooke 1991)

It is often speculated that the old parish boundaries are based on ancient trackways and at the Bishops Head and Foot there are important paths which traverse Penwith from Zennor to Castle-an- Dinas and Chysauster (both important Iron Age sites) and on to Mounts Bay.  The Tinners Way as already demonstrated follows several sections of parish boundaries along the high ground.  The trackway then continues through the parish of Towednack along the base of Rosewall Hill covered in old mining shafts and then onto the village of St Ives and The Island.

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The view from the Lady Downs in Towednack looking east.  In the distance it is possible to see Perran Sands and St Agnes Beacon.  Photo by Sheila Russell (geograph.co.uk)

Although today there stands a small chapel to St Nicholas on the Island it is thought that originally the headland was a much older promontory fort.  Its position which overlooks Porthmeor Beach and the wider expanse of St Ives bay including the entry to Hayle Harbour and with views all the way up the coast would suggest it was an important site.

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The Island at St Ives – Porthmeor Beach is in the foreground.  Photo by Chris Dixon (geograph.co.uk)

The Hayle Estuary was an important trading port on this coast until the Medieval period.  Dredging in the now silted harbour has in the past brought up finds from all periods including the Roman period and earlier.  Overlooking the harbour is the ancient enclosure of Trencrom Hill which as mentioned before can be dated to the Neolithic and later.

“It used to be thought that the earliest routes in Britain were prehistoric ‘ridgeways’, long distance trackways…This idea grew up in the early years of archaeological studies when the most obvious prehistoric monuments, such as Bronze Age burial mounds and Iron Age hillforts, were found concentrated in upland areas.” (Pre-industrial Roads, Trackways and Canals Historic England 2011).

Even though there is no concrete way of dating this particular route there are certainly a lot of indicators which point to it being an important part of the landscape in West Penwith with a long and fascinating history.

A useful wee book to read if you can get hold of one is “The Tinners Way”by Ian Cooke.  It is in essence a guidebook for walkers wishing to do the the Tinners Way, detailing the route and the  various features along the way.

 

 

The Karangahake Gorge and its Industrial Archaeology.

Summertime in New Zealand means roadtrips and exploring all that our lovely country has to offer.  Me and mine decided to spend some time in the goldmining town of Waihi and of course as always this meant a lesson in history, in particular the area around the Karangahake Gorge.

The Karangahake Gorge is situated between the Coromandel and Kaimai ranges and was formed by the flow of the Ohinemuri River.  It’s steep sides are covered in native bush, a haven for those wanting to experience the great outdoors.  There are plenty of walks and cycle trails to enjoy or you can simply sit by the river and enjoy a picnic.  However not so long ago the visitor would have been greeted by an entirely different scene.

On this visit we did the Windows Walk which takes you past and through several of the stamping batterys and the many associated building ruins then into the old tramway tunnels along the Waitawheta Gorge (an offshoot of the Karangahake Gorge).  Unlike other goldmining areas, alluvial gold is rare in the gorge and almost all of the gold and silver recovered from here was done by deep quartz mining.  This meant only the large well funded companies could afford to operate in the gorge.  The three main players were the Talisman Mining Company, The Woodstock Mining Company and the Crown Mining Company.  (The latter will ring some bells with those of you interested in Cornish mining history as they were a major player in the mining industry of Cornwall.  In fact many of the miners came from Cornwall which was at the time undergoing a decline in mining.  Their skills in hard rock mining was in great demand in colonial lands).  Today so much of the ruins are covered in dense bush, their edges softened by vegetation and with the sound of either the Ohinemuri or Waitawheta rivers filling your ears it is hard to imagine this as a place of heavy industry.

A continous rythmic thumping once filled the air here, as stamper batteries (gold recovery plants) of the Talisman, Woodstock and Crown Mining Companies pulverised quartz rock to free the gold within.” (taken from an information board at the beginning of the walk)

Much of the ore came from the steep sided Waitwheta Gorge and was then transported via aerial tramway across the gorge to the tramway and delivered to the stamping battery where it would undergo a series of crushings to extract the gold and silver which was then smelted into bullion bars.  The Talisman and Crown Mines were two of the largest of their type in New Zealand and together produced in the region of four million ounces of gold bullion.

The following are some of the photographs taken during our time exploring the industrial archaeology of the Karangahake Gorge.

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All that remains of the Talisman powerhouse on the banks of the Ohinemuri River.
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Several phases of building are present at the Talisman powerhouse – here you would have found the boilers and air compressors that powered the machinery for the battery and mines.

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Remains of the Woodstock Battery, note the water wheel for powering the stamping machine.
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Woodstock battery.
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These can be found lying all along the route, heavy cast iron crushers for pulverising the quartz.
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Woodstock battery.
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To increase yields potassium cyanide was used to remove even the smallest particles of gold and silver from the ore.

Once the ore had been crushed in the upper levels of the battery the fine powder that resulted was subjected to the cyanide process.  This involved mixing potassium cyanide with the finely crushed ore in tanks for several days then drawing off the solution and passing it through wooden boxes where the dissolved gold and silver precipitated as a black sludge on zinc shavings.  The sludge was then treated with sulphuric acid to remove the zinc.  The residue was then smelted into bullion bars (of gold and silver)” – From the above information board.

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Remains of the tanks where the powdered ore would be treated with cyanide.

 

One of the main features of the Windows Walk is the tramway, part of which goes through the side of the gorge (a torch is a must if you do this walk).  In its heyday, the ore was transported via tram but because of the steep sides of the gorge a trail had to be cut out of  and through the rockface.

A bit further on from the modern suspension bridge is the remains of the Crown  Mine.

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The entrance to the Crown Mine
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Drawing showing the extent of the Crown Mine in the Waitawheta Gorge.
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Side view of the mine workings through the gorge.
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The now peaceful view which was once dominated by the Crown Mine operations.

Today goldmining in the area is representated by the large open cast mine in nearby Waihi with the now defunct Cornish Pumphouse from the earlier 19th Century Martha Mine standing ever watchful over.

 

For more information –

Department of Conservation – Karangahake Gorge

Ohinemure Regional History Journal – Historic Karangahake Gorge

Waihi – Gold Discovery Centre

Waihi –  History and Heritage

Early Archaeology in Auckland – Ōtuataua Stonefields.

There are not many places within the city of Auckland where a person is able to get up close and personal with the early archaeology of the region, but the Ōtuataua Stonefields is one such place.  Although this small pocket is classed as a protected site, it is part of a much wider area called Ihuamāto which sadly is under threat by developers.  The stonefields did not exist in isolation and whilst the archaeology is not obvious  to the untrained eye, it is undoubtedly there.  It would be shameful if the council allowed work to proceed with out a full archaeological investigation.  In general attitudes in New Zealand towards archaeology is a case of “there’s not a lot of archaeology here” with the implication because we do not have the lengthy timeframes as elsewhere in the world it is not as important.  But this is erroneous and a result of a lack of knowledge –  there are over 70,000 archaeological sites listed in New Zealand…The stonefields and Ihuamāto are an important part of New Zealand’s very early history and to say otherwise would deny a people their past and demonstrate a dismal lack of understanding.

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Aerial view of the stonefields – the pale lines are stones piled along the natural ridges.

The story of this landscape begins much further back in time with three significant eruptions and subsequent lava flows that began some ninety thousand years ago and ended around fifteen thousand years ago. As with much of the isthmus of Tamaki Makaurau Auckland the volcanic activity served to create rich, well drained soils ideal for gardening.

Two hundred years ago there were some 8000 hectares of volcanic stonefields in the Auckland area, today the 100 hectare reserve of Ōtuataua is all which remains.  Dated to around 1300AD and situated near the international airport the reserve was established in 2001 to protect this important part of the archaeological record and is one of the last places where we can see large scale remains of how people once lived and worked in the volcanic areas of Auckland.

When the first Polynesians arrived in Aotearoa they bought with them the full range of tropical plants however the shorter growing season and colder temperatures meant that many of these tropical plants could not be grown.  Only plants such as the kumara (sweet potato), taro, yams and gourds had any success, particularly in the volcanic stonefields of Auckland.

There are two opposing theories as to how the settlement and gardens evolved at Ōtuataua –

  1. The initial focus was around the freshwater springs at the edge of the lava fields which then expanded to the volcanic cones later in the mid fourteenth to fifteenth centuries.
  2. Horticulture began on the volcanic cones and expanded outwards onto the lava fields; with the fortification of the cones occurring at a later date.

At Ōtuataua it is possible to see low mounds of the volcanic scoria stone scattered throughout an area referred to as the mound garden used mainly to grow kumara they extended the growing season by about a month.

“The mounds were built as special garden plots, which used the stone’s heat absorbing properties to help warm the earth and retain moisture.  Archaeologists have found that these types of mounds often contain specially modified soil, with added organic matter and ground shell.”

(from ‘The Ōtuataua Stonefields – Official Opening Commemorative Brochure’ Manukau City Council)

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The mound garden looking towards the later European dry stone wall.

It is safe to say that there is probably not a single stone which has not been moved by human hands. Walking towards the sea, you come across an area of low hills and gullies. The gully floors seem unnaturally free of stone, here the stone has been stacked on top of the hillocks to leave the gully floors free for cultivation.

On nearby Puketūtū Island, similar gardens were once present (very little if nothing remains of them today). In 1938 G. Fairfield recorded being told by a kaumātua from Māngere that “…each cultivation and sheltering wall was named after a particular ancestor or historical event…giving family groups their rights to occupy certain parts of the garden. In the corners of each of these walls there were upright stones that were never moved and considered tapu as they marked the limits of each family unit.” (from Shfiting Grounds: Deep Histories of Tamaki Makaurau Auckland L. Mackintosh pp29)

It would be fair to say that the same was occurring at Ōtuataua and beyond, thus creating a landscape that was deeply intertwined with the identity of those who lived and worked upon it.

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The cleared gullies of the gardens as seen from the pā – the Manakau harbour in the background.
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Other interesting archaeological features at Ōtuataua include the pā (hillfort or defended settlement) which utilised the volcanic cone.  Auckland has many volcanic cones, all of which were used and settled by the Māori throughout history.  Here at Ōtuataua it is no different. Unfortunately this particular cone has been extensively quarried for scoria before the site became a reserve resulting in the loss of a large part of the pā. However, it is still possible to make out the terraces on the southern side – these are the level areas cut into the lower slopes and were where Māori lived.

                                                              

Although the presence of a defensive structure such as the pā would suggest a time of unrest much of the Ōtuataua area consists of undefended settlements and gardens which tells a different story. One which is often left out of the histories. Past interpretations of pā have seen them as solely defensive structures used during periods of warfare and whilst this may be true on one level, it is likely that similar to the gardens, they represent more than the utilitarian. It has been recently suggested that pā could also have been part of the identity of the wider group/iwi, having a great deal to do with display and status (see another article on Kauri Point). When seen as a complete landscape the story of Ōtuataua becomes more than just gardens, houses and pā.

A second interesting feature is the site referred to as ‘The Big House’.  On an outcrop about half way between the mound garden and the gullies is a rectangular outline of stone.  This is believed to be the foundation of what was once a large house or structure, nearby are several shell middens.  Having never been excavated it is difficult to say what this structure was used for but the presence of the shell middens on the slopes below would indicate meals were eaten here.  Perhaps it was a communal place to share food whilst working in the gardens?

All over Ōtuataua shell middens can be found, not surprising given the proximity to the coast.  Fishing, shell fish gathering and horticulture were the mainstays of the local economy.

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A shell midden – the small white flecks are pieces of shell, note the deep rich colour of the soil, perfect for growing crops.
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This large mound on the edge of the pā is a very substantial midden…

In Polynesia crops such as kumara are left in the ground until they are needed however here in New Zealand with its cooler climate the early settlers found they could not do this as the kumara will rot. Instead it became necessary to harvest the kumara and store it. At Ōtuataua the visitor will occasionally come across a shallow depression in the ground, roughly rectangular in shape and usually found on slopes or ridges (for good drainage).  These are all that remains of the storage pits for kumara.  Originally these pits would have had timber walls and thatched roofs.  It is interesting to note that the storage pits here at Ōtuataua are outside of the defended pā, further evidence that the people felt secure and safe here on the edge of the Manukau Harbour – war was not as endemic to Tamaki Makaura as previously thought.

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A reconstruction drawing of how a kumara storage structure may have looked.

 

Above right is a depiction of a kumara storage pit with its timber frontage. On the left is a Rongo stone – these are representations of the god of agriculture and peace. They were considered tapu and left in the fields to encourage fertility of the land.

NB – During my visit to the stonefields, trying not to lose both the kids and the dog I was walking along the edge of a eroded shell midden when my eye was caught by an unusual stone.  Unusual because it was not scoria and was very smooth on one side.  The flip side was shaped to fit into the palm of your hand and although I am not much of an expert I am reasonably certain this was a rubbing stone for turning root vegetables such as taro or fern roots into pulp.  A necessary procedure if you wanted to eventually eat it.

 

See the following article for more information on Otuataua  – Photo-essay: Ihumatao and the Otautaua Historic Reserve

Reading – L. MacIntosh Shifting Grounds: Deep Histories of Tamaki Makaurau Auckland Bridget Williams Books 2021.

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Clues in the Landscape – Placenames, Maps and Fields.

“When you hear the Cornish folk mentioning the names of their villages, hills, and other landmarks, you will notice something un-English about them.  In the accent and cadence of some of the placenames there is an echo of the goblin world.  Is there not, in such names as Ogbeare, Killeganogue and Poulza, an oddity – a twist that is just on the edge of the bizarre.”

(Hopkins T. ‘Our Beautiful Homeland: Cornwall’ date unknown)

It is true that the first thing a visitor to Cornwall will notice is the placenames, they are very ‘un-English’ in particular the further west you go.  My interest in them began many years ago as a student writing a masters dissertation on the landscape continuity on the north coast of West Penwith.

The study of placenames can be highly complex, after all names do change for whatever reasons and in the case of Cornwall the names are often in Cornish which as a language has also undergone many changes.  The Cornish language is related to both the Welsh and Breton languages, all of which are regarded as being descended from the language spoken by the ‘Celts’.  The relationship with these Brittonic languages is often used as evidence for the age of a particular placename, albeit in a general sense.

“The name of a village or farm or field may describe the locality as it was when the name was given, or refer to a natural or man-made feature nearby, or include the name of a pioneer farmer or priest (the latter often termed a ‘saint’).  Names can seldom be translated with the certainty aimed a in normal translation between languages; generally they can only be interpreted, with a greater or less degree of probability, as unconscious and unintended messages from the past which are seldom free from ambiguity or obscurity.  The prime rule in placename interpretation is to attempt none until all available forms of the name have been considered, and then to place greater reliance on earlier rather than later forms.” (Pool P. A. S. 1990 ‘The Fieldnames of West Penwith).

The distribution of Cornish placenames is not uniform across the county, those places nearest the Tamar River – the natural boundary between  Cornwall and Devon – have a greater tendency to be more English than those in the far west.  In my dissertation I surveyed an area of the north coast of west Penwith (within the parishes of Morvah and Zennor) and of the forty placenames to be found on the Tithe map of 1841 only one had an English name – the hamlet of Wicca.

Below are a handful of the most common prefixes used in Cornish placenames and their meaning (from Weatherhill C. 1998 ‘Cornish Placenames and Language’)

Bos – as in Boscastle, Boscawen or Bosavern.  Also found as Bot-, Bo-, Boj-, Bus-, and Bod-.  Meaning dwelling or home it seems to be a very early form whose usage dwindles by 1500.  It is often followed by a persons name such as Bodilly on the Lizard which can be translated as ‘the dwelling of Deli’.

Car-/Gear-/Caer-/Cr- as in Caervallack, Carwythenack or Carvossa.  Meaning an enclosed settlement and occasionally a ‘fort’.  Often found associated with late prehistoric farmsteads within round enclosures as well as Iron Age hillforts.  Carvedras near Truro can be translated as ‘Modret’s fort’.

Carn – as is in Carn Brea, Carn Meal or Carn Clew.  One of the most common still in use today and is used in reference to prominent rock formations, on hilltops it can translated to ‘tor’ whilst at other locations it might mean ‘crag’ or ‘rockpile’.  Occasionally it may even refer to a Bronze Age Barrow.

 

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Carn Brea – the rocky tor visible on the hill top. (geograph.co.uk – 1185968)

 

Chy-/Che-/Ch-/Ty- as in Chun, Chyanvounder or Chynoweth.  Meaning either ‘cottage’ or ‘house’.   Thus Chyandour can be translated as ‘house by the water/stream’.  This prefix replaces the earlier ‘Bos’.

Hen – as in Hendra or Henscath. Meaning old as in former, ancient.  Hendra can in its simple form mean ‘old farm’ but is better interpreted as ‘farm which still stands on its original site.

 

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Entrance to Hendra Farm (geograph.co.uk – 210812)

 

Lan – as in Lamorran or Lanzeague.  Meaning ‘church enclosure’ it became redundant by 1500, historians usually take the presence of this prefix as an indicator for an early church site often surrounded by an enclosure which in some cases is a reused prehistoric site.

Tre-/Trev-/Tr- as in Tregenna or Tregeseal to name but two – this is by far and away the most common of all prefixes.  Meaning “farming settlement’ and later used to denote a larger settlement such as village.  They are often followed by a persons name such as Tregiffian or ‘Gifyan’s farm’ and in other cases it might be followed by a descriptive word such as Trencrom or ‘the farm on the curve’.

Venton-/Fenton- as in Venton Vedna or Ventonraze.  Meaning ‘a well’ in the sense of a natural spring, an artificially dug well is ‘Peeth’.  Often the prefix is followed by a name of a saint such as Venton Uny or ‘the well of St Euny’ others might be followed by a distinguishing feature such as Ventonwyn or ‘the white well’.

Of course understanding the meaning behind the names is not the only source of information.  Looking at the distribution of certain placenames within a given area may hint at the evolution of the human landscape.  In some areas it is possible to see the stratigraphy of the landscape.  An essential part of such a study involves the use of maps.

 

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John Speed’s Map of Cornwall 1614

 

 

No study of the landscape can be conducted without a good range of maps.  Early Ordnance Survey maps and Tithe maps are crucial in understanding any landscape before modern incursions such as motorways, housing subdivisions, caravan parks and business parks, make an appearance.  Even in the case of West Penwith the choice of the 1841 Tithe Map during my dissertation was to ensure that any more recent names attached to barn conversions and holiday lets did not lead to false results.  Maps can also show features which may no longer be obvious on the ground such as hedges which may have later been removed and mining remains among others.

 

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An early drawing for large scale OS map of Lands End.  Two points of interest are – the tin and copper mines are indicated by a dotted lines, also the circular marking on the left indicate the area around Sancreed and the hillfort of Caer Bran.  It was not until 1816 that the recording of archaeologica sites on OS maps became obligatory.

 

Of course very early maps can be quite frustrating as often the information included is not clear and/or very selective according to who made the map and why.   Just because a settlement does not appear on one map does not mean it did not exist at the time of surveying.  For example, the Domesday Book records only a handful of settlements in the whole of West Penwith.  It seems highly unlikely that the region was all but empty, but given this was an economic text and not a history one it is not too surprising either.  To this extent gaining insight from a wide range of maps is often the best course of action.

Another source of information which can often be overlooked in the study of past landscapes are fieldnames.  Although they are less well documented and it is not until the Tithe Apportionment of 1841 that fieldnames are properly recorded,  albeit by this stage most are in English. It is also important to note that by their very nature fieldnames are transient, their names can change as their usage does.  However there is on occasion names which stick and just occasionally these names can hint at a previously unknown archaeological site or field usage.  For example Park an Vellan could suggest the presence of a mill (vellan being a form of melyn or mill) and Park Menheere suggests the presence of standing stone.

In the case of later English fieldnames some may well have been directly translated from the Cornish and are thus older than expected.  So Spring Field may have originally been Park an Venton or Barrow Field was Gweal Creeg.

 

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A view of fields near the hamlet of Zennor demonstrating the higgly-piggly nature of the fields systems.  (geograph.co.uk – 633)

 

The study of placenames, maps and fieldnames is one of the least intrusive forms of research a person can do and yet can yield a myriad of information that in some cases was not known.  When combined with other sources such as documents and aerial photography it becomes a powerful part of archaeological research providing fresh insight into our ancient landscapes.

 

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An aerial photo giving a birds eye view over a portion of the West Penwith coastline (copyright Tom Corser 2009)

 

Once you have got your eye in so to speak, it will be forever impossible to go for a simple walk in the landscape.  I am doomed to be wandering the landscape always looking for patterns, asking what does that name mean and is it in it’s original form.

Sources:

Gelling M. (2000) Place-Names in the Landscape Phoenix Press

Hopkins R. T. (?) Our Beautiful Homeland: Cornwall Blackie and Son Ltd

Pool P. A. S (1990) The Fieldnames of West Penwith Published by the Author

Weatherhill C. (1998) Cornish Place Names and Language Sigma Leisure