Magna Carta concession to forest access > .
Magna Carta accedes to dis-afforestation > .
What was the Charter of the Forest? | Magna Carta Series > .
Carta Foresta 1217 - TrId >> .
Ray Mears: Forest of Dean Wild Britain S01E01 Deciduous Forest
https://www.youtube.com/watch?v=bhnBhObR5QU
The Forest of Dean lies in west Gloucestershire in the angle formed by the rivers Severn and Wye as they approach their confluence. A large tract of woodland and waste land there was reserved for royal hunting before 1066 and survived into the modern period as one of the principal Crown forests in England, the largest after the New Forest. The name Forest of Dean was recorded from c. 1080 and was probably taken from the valley on the north-east of the area, where a manor called Dean was the Forest's administrative centre in the late 11th century.
In modern times the name Forest of Dean was sometimes used loosely for the part of Gloucestershire between the Severn and Wye, but all that land belonged to the Forest (used in the specific sense of the area subject to the forest law) only for a period in the early Middle Ages. In the 13th century the Forest's bounds were the two rivers and it extended northwards as far as Ross-on-Wye (Herefs.), Newent, and Gloucester; it then included 33 Gloucestershire and Herefordshire parishes, besides a central, uncultivated area which the Crown retained in demesne. Revised bounds, perambulated in 1300 and accepted by the Crown in 1327, reduced the extent of the Forest to the royal demesne and 14 parishes or parts of parishes, most of them, like the demesne itself, in St. Briavels hundred. The royal demesne remained extraparochial until the 1840s when, villages and hamlets having grown up within it, it was formed into the civil townships (later parishes) of East Dean and West Dean and into ecclesiastical districts.
......
The formerly extraparochial land of the Forest of Dean lies mainly at over 200 m. (656 ft.), reaching its highest point, 290 m. (951 ft.), at Ruardean hill in the north. Sometimes described as a plateau but actually comprising steep ridges and the valleys of streams draining to the Severn and Wye, its boundaries with the surrounding cultivated and ancient parochial lands are in most places defined by a scarp where the underlying carboniferous limestone of the region outcrops. On the west, however, the limestone outcrops at a shallower angle and there is a less obvious distinction in height between the Forest and the cultivated land of the large ancient parish of Newland. The long valley of Cannop brook, earlier called the Newerne stream, crosses the west part of the Forest from north to south, and a stream called in its northern part Cinderford brook and in its southern Soudley brook forms a long winding valley through the east part. Blackpool brook, so called by 1282, carves another deep valley through the south-eastern edge of the high land to meet Soudley brook at Blakeney below the Forest's scarp, and at the Forest's northern edge Greathough brook, formerly Lyd brook, descends a valley to the Wye. The streams were dammed in places for ironworks, notably in the Cannop valley where two large ponds were made in the 1820s to provide power for works at Parkend. Other large ponds on a tributary stream of Soudley brook at Sutton bottom, near Soudley, were built as fishponds in the mid 19th century for a privately-owned estate in that part of the Forest called Abbots wood. In the late 20th century the Forestry Commission maintained the Forest's ponds as nature reserves and as a public amenity; new ones were made at Woorgreen, near the centre of the Forest, as part of landscape restoration following opencast coal mining in the 1970s, and at Mallards Pike, near the head of Blackpool brook, in 1980.
Geology has given the Forest its rich industrial history. The land is formed of basin-shaped strata of the Carboniferous series. Underlying and outcropping at the rim are limestones which, especially the stratum called Crease Limestone, contain deposits of iron ore. Above are beds of sandstone, shale, and coal. The lowest bed of sandstone is known by the local name of Drybrook Sandstone, and the highest is the Pennant Sandstone. There are over 20 separate coal seams, varying in thickness from a few inches to 5 ft., the highest yielding being the Coleford High Delf which rises close to the surface near the rim of the Forest. Surface workings, shallow pits, or levels driven into the hillsides were the means of winning the iron ore and coal until the late 18th century when deeper mines were sunk. There were also numerous quarries, notably those in the Pennant Sandstone at Bixhead and elsewhere on the west side of the Cannop valley; that stone, which varies in colour but is mainly dark grey, was the principal building material used in the Forest's 19th-century industrial hamlets.
The Forest was most significant as a producer of oak timber, which was the principal reason for its survival in the modern period. Until the early 17th century, however, there was as much beech as oak among its large timber trees, and chestnut trees once grew in profusion on the north-east side of the Forest near Flaxley and gave the name by 1282 to a wood called the Chestnuts. The underwood was composed of a variety of small species such as hazel, birch, sallow, holly, and alder. The ancient forest contained many open areas. In 1282 various 'lands', or forest glades, maintained by the Crown presumably as grazing for the deer, included several with names later familiar in the Forest's history, Kensley, Moseley, Cannop, Crump meadow, and Whitemead (later a part of Newland parish). Numerous smaller clearings called 'trenches' had also been made as corridors alongside roads for securing travellers against ambush or for the grazing and passage of the deer. Larger areas of waste, or 'meends', such as Clearwell Meend and Mitcheldean Meend, lay on the borders adjoining the manorial lands, whose inhabitants used them for commoning their animals.
Although the royal demesne land was without permanent habitation until the early modern period, it was crossed by many ancient tracks, used by ironworkers, miners, and charcoal burners; large numbers, many termed 'mersty' (meaning a boundary path), were recorded in 1282 in a perambulation of the Forest bailiwicks, its administrative divisions. One of the more important ancient routes, known as the Dean road, had a pitched stone surface and borders of kerbstones. It ran between Lydney and Mitcheldean across the eastern part of the demesne by way of Oldcroft, a crossing of Blackpool brook, recorded as Blackpool ford in 1282, and a crossing of Soudley brook at Upper Soudley. The survival of much pitching and kerbing after the road went out of use in the turnpike era, and the possibility that it had linked two important Roman sites at Lydney and Ariconium, in Weston under Penyard (Herefs.), has led to the suggestion that it was a Roman road, though much of the stonework probably dates from the medieval and early modern periods; an estimate was made for renewing long stretches of the road, including the provision of new border stones, as late as the 1760s.
Two main routes crossed the extraparochial Forest from north-east to south-west and on them were sited the principal points of reference in a terrain with few landmarks. A route from the Severn crossing at Newnham to Monmouth recorded in 1255, when 'trenches' were ordered to be made beside it, was presumably that through Littledean, the central Forest, and Coleford. It entered over a high ridge west of Littledean, where a hermitage of St. White had been founded by 1225, and crossed Soudley (or Cinderford) brook at the place called Cinder ford in 1258, long before its name was taken by the principal settlement of the extraparochial Forest that formed on the hillside to the north-east of the crossing. Further west, near the centre of the Forest, the road passed the clearing called Kensley, where a courthouse stood by 1338 close to the site of the later Speech House, and crossed Newerne (or Cannop) brook at Cannop. The road emerged into the cultivated land of Coleford tithing at a place later called Broadwell Lane End, where a tree called Woolman oak in 1608 (fn. 34) was probably the 'W(o)lfmyen' oak which in 1282 was a landmark at the boundary of four of the Forest's bailiwicks. The other main route, recorded in 1282 as the high road to Monmouth, was that crossing the high north-western part of the extraparochial land from Mitcheldean, by way of Nailbridge, Brierley, Mirystock, where it crossed a tributary of Cannop brook above Lydbrook, to Coleford. The two remained the principal routes through the Forest but the northern one, described in the 1760s as the great road through the Forest from Gloucester to South Wales, was much altered in its course by later improvements.
The rivers Severn and Wye played a vital role in the development of Dean's industry but few of the various tracks and hollow ways that led from the central Forest to riverside landing-places and ferries were usable other than by packhorses before the 19th century. One of the few routes negotiable by wagons and timber rigs was the central main road out to Littledean with its branch down to Newnham; that was the usual route for carrying timber out of the Forest in 1737 when the Crown was asked to assist Newnham parish to repair part of it. Later in the 18th century a road leading from the south part of the woodlands by way of Parkend and Viney Hill to Gatcombe and Purton on the Severn became the principal route for timber destined for the naval dockyards.
The Crown's hunting rights, which provided the original motive for the Forest's preservation, were much used in the 13th century. The frequent orders made at the period for taking deer for gifts by the Crown and to meet the needs of the royal household suggest that fallow deer were the majority species in Dean, with red deer and roe present in smaller numbers. In 1278 the Forest was sufficiently well stocked for royal huntsmen to take 100 fallow bucks. At that period all three species of deer were classed as beasts of the forest, reserved for the exclusive use of the Crown, but roe were not classified as such after 1340.
http://www.british-history.ac.uk/vch/glos/vol5/pp285-294
Forest of Dean: Forest administration
http://www.british-history.ac.uk/vch/glos/vol5/pp354-377
Forest of Dean: search
http://www.british-history.ac.uk/search?query=forest%20of%20dean
Magna Carta accedes to dis-afforestation > .
What was the Charter of the Forest? | Magna Carta Series > .
Carta Foresta 1217 - TrId >> .
Ray Mears: Forest of Dean Wild Britain S01E01 Deciduous Forest
https://www.youtube.com/watch?v=bhnBhObR5QU
The Forest of Dean lies in west Gloucestershire in the angle formed by the rivers Severn and Wye as they approach their confluence. A large tract of woodland and waste land there was reserved for royal hunting before 1066 and survived into the modern period as one of the principal Crown forests in England, the largest after the New Forest. The name Forest of Dean was recorded from c. 1080 and was probably taken from the valley on the north-east of the area, where a manor called Dean was the Forest's administrative centre in the late 11th century.
In modern times the name Forest of Dean was sometimes used loosely for the part of Gloucestershire between the Severn and Wye, but all that land belonged to the Forest (used in the specific sense of the area subject to the forest law) only for a period in the early Middle Ages. In the 13th century the Forest's bounds were the two rivers and it extended northwards as far as Ross-on-Wye (Herefs.), Newent, and Gloucester; it then included 33 Gloucestershire and Herefordshire parishes, besides a central, uncultivated area which the Crown retained in demesne. Revised bounds, perambulated in 1300 and accepted by the Crown in 1327, reduced the extent of the Forest to the royal demesne and 14 parishes or parts of parishes, most of them, like the demesne itself, in St. Briavels hundred. The royal demesne remained extraparochial until the 1840s when, villages and hamlets having grown up within it, it was formed into the civil townships (later parishes) of East Dean and West Dean and into ecclesiastical districts.
......
The formerly extraparochial land of the Forest of Dean lies mainly at over 200 m. (656 ft.), reaching its highest point, 290 m. (951 ft.), at Ruardean hill in the north. Sometimes described as a plateau but actually comprising steep ridges and the valleys of streams draining to the Severn and Wye, its boundaries with the surrounding cultivated and ancient parochial lands are in most places defined by a scarp where the underlying carboniferous limestone of the region outcrops. On the west, however, the limestone outcrops at a shallower angle and there is a less obvious distinction in height between the Forest and the cultivated land of the large ancient parish of Newland. The long valley of Cannop brook, earlier called the Newerne stream, crosses the west part of the Forest from north to south, and a stream called in its northern part Cinderford brook and in its southern Soudley brook forms a long winding valley through the east part. Blackpool brook, so called by 1282, carves another deep valley through the south-eastern edge of the high land to meet Soudley brook at Blakeney below the Forest's scarp, and at the Forest's northern edge Greathough brook, formerly Lyd brook, descends a valley to the Wye. The streams were dammed in places for ironworks, notably in the Cannop valley where two large ponds were made in the 1820s to provide power for works at Parkend. Other large ponds on a tributary stream of Soudley brook at Sutton bottom, near Soudley, were built as fishponds in the mid 19th century for a privately-owned estate in that part of the Forest called Abbots wood. In the late 20th century the Forestry Commission maintained the Forest's ponds as nature reserves and as a public amenity; new ones were made at Woorgreen, near the centre of the Forest, as part of landscape restoration following opencast coal mining in the 1970s, and at Mallards Pike, near the head of Blackpool brook, in 1980.
Geology has given the Forest its rich industrial history. The land is formed of basin-shaped strata of the Carboniferous series. Underlying and outcropping at the rim are limestones which, especially the stratum called Crease Limestone, contain deposits of iron ore. Above are beds of sandstone, shale, and coal. The lowest bed of sandstone is known by the local name of Drybrook Sandstone, and the highest is the Pennant Sandstone. There are over 20 separate coal seams, varying in thickness from a few inches to 5 ft., the highest yielding being the Coleford High Delf which rises close to the surface near the rim of the Forest. Surface workings, shallow pits, or levels driven into the hillsides were the means of winning the iron ore and coal until the late 18th century when deeper mines were sunk. There were also numerous quarries, notably those in the Pennant Sandstone at Bixhead and elsewhere on the west side of the Cannop valley; that stone, which varies in colour but is mainly dark grey, was the principal building material used in the Forest's 19th-century industrial hamlets.
The Forest was most significant as a producer of oak timber, which was the principal reason for its survival in the modern period. Until the early 17th century, however, there was as much beech as oak among its large timber trees, and chestnut trees once grew in profusion on the north-east side of the Forest near Flaxley and gave the name by 1282 to a wood called the Chestnuts. The underwood was composed of a variety of small species such as hazel, birch, sallow, holly, and alder. The ancient forest contained many open areas. In 1282 various 'lands', or forest glades, maintained by the Crown presumably as grazing for the deer, included several with names later familiar in the Forest's history, Kensley, Moseley, Cannop, Crump meadow, and Whitemead (later a part of Newland parish). Numerous smaller clearings called 'trenches' had also been made as corridors alongside roads for securing travellers against ambush or for the grazing and passage of the deer. Larger areas of waste, or 'meends', such as Clearwell Meend and Mitcheldean Meend, lay on the borders adjoining the manorial lands, whose inhabitants used them for commoning their animals.
Although the royal demesne land was without permanent habitation until the early modern period, it was crossed by many ancient tracks, used by ironworkers, miners, and charcoal burners; large numbers, many termed 'mersty' (meaning a boundary path), were recorded in 1282 in a perambulation of the Forest bailiwicks, its administrative divisions. One of the more important ancient routes, known as the Dean road, had a pitched stone surface and borders of kerbstones. It ran between Lydney and Mitcheldean across the eastern part of the demesne by way of Oldcroft, a crossing of Blackpool brook, recorded as Blackpool ford in 1282, and a crossing of Soudley brook at Upper Soudley. The survival of much pitching and kerbing after the road went out of use in the turnpike era, and the possibility that it had linked two important Roman sites at Lydney and Ariconium, in Weston under Penyard (Herefs.), has led to the suggestion that it was a Roman road, though much of the stonework probably dates from the medieval and early modern periods; an estimate was made for renewing long stretches of the road, including the provision of new border stones, as late as the 1760s.
Two main routes crossed the extraparochial Forest from north-east to south-west and on them were sited the principal points of reference in a terrain with few landmarks. A route from the Severn crossing at Newnham to Monmouth recorded in 1255, when 'trenches' were ordered to be made beside it, was presumably that through Littledean, the central Forest, and Coleford. It entered over a high ridge west of Littledean, where a hermitage of St. White had been founded by 1225, and crossed Soudley (or Cinderford) brook at the place called Cinder ford in 1258, long before its name was taken by the principal settlement of the extraparochial Forest that formed on the hillside to the north-east of the crossing. Further west, near the centre of the Forest, the road passed the clearing called Kensley, where a courthouse stood by 1338 close to the site of the later Speech House, and crossed Newerne (or Cannop) brook at Cannop. The road emerged into the cultivated land of Coleford tithing at a place later called Broadwell Lane End, where a tree called Woolman oak in 1608 (fn. 34) was probably the 'W(o)lfmyen' oak which in 1282 was a landmark at the boundary of four of the Forest's bailiwicks. The other main route, recorded in 1282 as the high road to Monmouth, was that crossing the high north-western part of the extraparochial land from Mitcheldean, by way of Nailbridge, Brierley, Mirystock, where it crossed a tributary of Cannop brook above Lydbrook, to Coleford. The two remained the principal routes through the Forest but the northern one, described in the 1760s as the great road through the Forest from Gloucester to South Wales, was much altered in its course by later improvements.
The rivers Severn and Wye played a vital role in the development of Dean's industry but few of the various tracks and hollow ways that led from the central Forest to riverside landing-places and ferries were usable other than by packhorses before the 19th century. One of the few routes negotiable by wagons and timber rigs was the central main road out to Littledean with its branch down to Newnham; that was the usual route for carrying timber out of the Forest in 1737 when the Crown was asked to assist Newnham parish to repair part of it. Later in the 18th century a road leading from the south part of the woodlands by way of Parkend and Viney Hill to Gatcombe and Purton on the Severn became the principal route for timber destined for the naval dockyards.
The Crown's hunting rights, which provided the original motive for the Forest's preservation, were much used in the 13th century. The frequent orders made at the period for taking deer for gifts by the Crown and to meet the needs of the royal household suggest that fallow deer were the majority species in Dean, with red deer and roe present in smaller numbers. In 1278 the Forest was sufficiently well stocked for royal huntsmen to take 100 fallow bucks. At that period all three species of deer were classed as beasts of the forest, reserved for the exclusive use of the Crown, but roe were not classified as such after 1340.
http://www.british-history.ac.uk/vch/glos/vol5/pp285-294
Forest of Dean: Forest administration
http://www.british-history.ac.uk/vch/glos/vol5/pp354-377
Forest of Dean: search
http://www.british-history.ac.uk/search?query=forest%20of%20dean
