Tuesday, 8 June 2010


Bodmin Moor (Cornish: Goen Bren) is a granite moorland in northeastern Cornwall, England, United Kingdom. It is 208 square kilometres (80 sq mi) in size, and originally dates from the Carboniferous period of geological history.

Bodmin Moor is one of five granite batholiths in Cornwall.
The name 'Bodmin Moor' is relatively recent, being an Ordnance Survey invention of 1813. It was formerly known as Fowey Moor after the River Fowey which rises within it.
Dramatic granite tors rise from the rolling moorland: the best known are Brown Willy, the highest point in Cornwall at 417 m (1,368 ft), and Rough Tor at 400 m (1,300 ft). To the south-east Kilmar Tor and Caradon Hill are the most prominent hills. Considerable areas of the moor are poorly drained and form marshes (in hot summers these can dry out). The rest of the moor is mostly rough pasture or overgrown with heather and other low vegetation.

The Moor contains about 500 holdings with around 10,000 beef cows, 55,000 breeding ewes and 1,000 horses and ponies. Most of the moor is a Site of Special Scientific Interest (SSSI) and has been officially designated an Area of Outstanding Natural Beauty, as part of Cornwall Rivers and inland waters

Bodmin Moor is the source of several of Cornwall's rivers: they are mentioned here anti-clockwise from the south.
The River Fowey rises at a height of 290 m (950 ft) and flows through Lostwithiel and into the Fowey estuary.
The River Tiddy rises near Pensilva and flows southeast to its confluence with the River Lynher  flows generally south-east until it joins the Hamoaze near Plymouth). The River Inny rises near Davidstow and flows southeast to its confluence with the River Tamar.
The River Camel rises on Hendraburnick Down and flows for approximately 40 km (25 mi) before joining the sea at Padstow. The River Camel and its tributary the De Lank River are an important habitat for the otter and both have been proposed as Special Areas of Conservation. The De Lank River rises near Roughtor and flows along an irregular course before joining the Camel south of Wenford.

The River Warleggan rises near Temple and flows south to join the Fowey.
On the southern slopes of the moor lies Dozmary Pool. It is Cornwall's only natural inland lake and is glacial in origin. In the 20th century three reservoirs have been constructed on the moor; these are Colliford Lake, Siblyback Lake and Crowdy reservoirs which supply water for a large part of the county's population. Various species of waterfowl are resident around these waters.

10,000 years ago, in the Mesolithic period, hunter-gatherers wandered the moor when it was wooded and had a temperate climate. There are several documented cases of flint scatters being discovered by archaeologists, indicating that these hunter gatherers practised flint knapping in the region.

During the Neolithic era, from about 4,500 to 2,300 BC, people began clearing trees and farming the land. It was also in this era that the production of various megalithic monuments began, predominantly long cairns (three of which have currently been identified, at Louden, Catshole and Bearah) and stone circles (sixteen of which have been identified). It was also likely that the naturally forming tors were also viewed in a similar manner to the manmade ceremonial sites.

In the following Bronze Age, the creation of monuments increased dramatically, with the production of over 300 further cairns, and more stone circles and stone rows. More than 200 Bronze Age settlements with enclosures and field patterns have been recorded. and many prehistoric stone barrows and circles lie scattered across the moor.

King Arthur's Hall thought to be a late Neolithic or early Bronze Age ceremonial site can be found to the east of St Breward on the moor.
Where practicable areas of the moor were used for pasture by herdsmen from the parishes surrounding the moor. Granite boulders were also taken from the moor and used for stone posts and to a certain extent for building (such material is known as moorstone). Granite quarrying only became reasonably productive when gunpowder became available.

The moor gave its name (Foweymore) to one of the medieval districts called stannaries which administered tin mining: the boundaries of these were never defined precisely. Until the establishment of a turnpike road through the moor (the present A30) in the 1770s the size of the moorland area made travel within Cornwall very difficult.
Roughtor was the site of a medieval chapel of St Michael and is now designated as a memorial to the 43rd Wessex Division of the British Army. In 1844 on Bodmin Moor the body of 18 year old Charlotte Dymond was discovered. Local labourer Matthew Weeks was accused of the murder and at noon on 12 August 1844 he was led from Bodmin Gaol and hanged. The murder site now has a monument erected from public money and the grave is at Davidstow churchyard.

Historical Text taken from Wikipedia.


  1. Very interesting article Monts. The B&W photograph is very atsmopheric.

  2. A very moody photo, Monty and interesting facts too.

    Only just managed to view your previous post. Strangely enough, that is the second Angle Shades I have seen on a blog in the last 15 minutes having never heard of it before! I loved the picture of the Song Thrush among the daisies, so pretty.

  3. What a fascinating read!! I enjoyed the history and geography lesson very much. Monty, thanks for swinging by my blog today. It was nice to see you there, and a gentle reminder to check in with you to see what's up! ~karen

  4. Great post Monty. Love the image.

  5. Nice image and interesting text never worked out where it was previously so may look for it when i'm next down in ten days or so.

  6. Lovely shot Monts, Black and white photos of the moors are so etherial. Well done!!

  7. I remember the Bodmin Moor and you have captured it perfectly in black and white.
    Sorry to late in with a comment, my son is visiting for several days so I running behind.
    Have a wonderful week.
    ☼ Sunny