
17. An ~8 miles/12 km circular walk
from Goathland - Mallyan Spout - Wheeldale Moor - Roman Road (Wade's
Causeway - Beckhole
- The Incline - Goathland
Scenes
of
Whitby and surrounding area including
Pictures
of Goathland

You walk through some most
pleasant countryside down into the valley of Wheeldale Beck starting
from by the side of the Mallyan spout Hotel in Goathland village.
*
*


The path goes down by the Mallyan Spot Coffee shop, by
the side of the Mallyan Spout Hotel

The path is a bit steep and a
rocky-muddy scramble in places, so take care!

Eventually Mallyan Spout is
reached.

You follow the river bank
of Wheeldale Beck climbing gently upwards ...

... to Hunt House (dated 1900).

Near Wheeldale Lodge (once
a YHA youth hostel), what remains alive of this
old Scots pine is growing down wind!
Wheeldale Beck is crossed
by stepping stones, whose orange-brown colouration betrays the iron in
the stones. Wheeldale Lodge is on the distant right of the picture.

After the stepping stones
you climb up onto Wheeldale Moor.
TOP OF PAGE

Eventually the Roman Road
is reached. You can see the camber clearly on this stretch of the road.




The original curb stones
can be seen quite clearly as a neat line on the left of the road.

On Wheeldale Moor the Roman Road heads
downhill to the junction of two river-streams.






But, before reaching the
footbridge and ford, the Roman way seems to continue as a discarded
traditional North Yorkshire red
roofing tiles road!

Did the Roman Road cross
the river at this ford?

Climbing up from the river
you go up a very sunken 'green' road-track, with a very 'medieval' feel to
it.


There are many handsome
farmhouse buildings with fine stonework on the walk, here Hazel Head Farm (1908) ...

... and Hollin farmhouse with the
village of Goathland in the distance.

After more woodland and
another river crossing you deviate from the incline track to Goathland
for a some welcome refreshment at Beck Hole.

While partaking of
refreshment you will hear the sounds of the locomotives of the North
Yorkshire Moors Railway and just up the road is a bridge from which they
can be observed. In this case (for steam buffs only!), Southern Railway
Schools Class 4-4-0 30926 "Repton" is working hard to overcome the
gradient to Goathland Station.

From Incline Cottage you
then walk up the path of the original railway incline from the early
19th century ...

... and eventually you climb
back up incline into Goathland Village.
TOP OF PAGE
Alternative
route back to Goathland

You can descend of Wheeldale Moor and return to
Goathland passed the house that was once a YHA youth hostel.

Crossing the iron-stained Wheeldale Beck
Ex YHA Youth Hostel, now a private house.

Just before Goathland the path passes an prehistoric
standing stone, its not very big, but it is very ancient.

TOP OF PAGE
 |
 |
 |
The Birch Hall
Inn cum 'cafe' in the tiny village of Beck Hole near Goathland on the
North York Moors, North
Yorkshire. A welcome 'watering hole' for
many walking
tourists, especially if you have just climbed up the 'old
incline' of the original Grosmont-Goathland railway. You can
hear the sounds of the steam trains on the 'modern' line of
the North Yorkshire Moors Railway which is just up the road
and links up Whitby-Pickering. |
Holidays in the
North York Moors National Park, interesting places to visit in the North
York Moors an areas of outstanding natural beauty, good places to say in
the North York Moors, pretty villages and scenic walks in the North York
Moors, holiday cottages in North Yorkshire, weekend breaks in luxury
hotels in North Yorkshire, places to dine out in North Yorkshire.
seaside holiday bookings for Whitby, seaside holiday bookings for
Scarborough, hotels and holiday cottages in Whitby, hotels and holiday
cottages in Scarborough |
More on
the Roman Road on Wheeldale Moor - Wade's Causeway (from
Wikipedia)
Wade's Causeway is a sinuous, linear monument up to
6,000 years old in the North York Moors national park in North
Yorkshire, England. The name may refer to either scheduled ancient
monument number 1004876—a length of stone course just over 1 mile
(1.6 km) long on Wheeldale Moor, or to a postulated extension of
this structure, incorporating ancient monuments numbers 1004108 and
1004104 extending to the north and south for up to 25 miles (40 km).
The visible course on Wheeldale Moor consists of an embankment of
soil, peat, gravel and loose pebbles 0.7 metres (2.3 ft) in height
and 4 to 7 metres (13 to 23 ft) in width. The gently cambered
embankment is capped with unmortared and loosely abutted flagstones.
Its original form is uncertain since it has been subjected to
weathering and human damage.
The structure has been the subject of folklore in the surrounding
area for several hundred years and possibly more than a millennium.
Its construction was commonly attributed to a giant known as Wade, a
figure from Germanic or Norse mythology. In the 1720s the causeway
was mentioned in a published text and became known outside the local
area. Within a few years it became of interest to antiquarians who
visited the site and exchanged commentary on its probable
historicity. They interpreted the structure as a causeway across
marshy ground, attributing its construction to the Roman military,
an explanation largely unchallenged throughout the eighteenth and
nineteenth centuries.
The stretch of causeway on Wheeldale Moor was cleared of vegetation
and excavated in the early twentieth century by a local gamekeeper
with an interest in archaeology. Historian Ivan Margary agreed with
its identification as a Roman road, and assigned it the catalogue
number 81b in the first edition of his Roman Roads In Britain
(1957). The causeway was further excavated and studied by
archaeologist Raymond Hayes in the 1950s and 1960s, partly funded by
the Council for British Archaeology. The results of his
investigation, which concluded that the structure was a Roman road,
were published in 1964 by the Scarborough Archaeological and
Historical Society.
In the late twentieth and early twenty-first centuries, its
identification as a Roman road has been questioned by academics, and
alternative interpretations suggested for its purpose and date of
construction. The monument's co-manager, English Heritage, in 2012
proposed several avenues of research that might be used to settle
some of the questions that have arisen regarding its origins and
usage.
The area through which the Wheeldale structure runs
is predominantly uncultivated heather moorland. Hayes believes its
appearance has remained fundamentally unchanged since the Bronze Age
when its forest cover was removed to permit cultivation and grazing.
Wheeldale Moor is poorly drained in places making it susceptible to
flooding in both the ancient and modern eras. The underlying geology
consists of patches of sand and gravel on top of mixed sandstone and
oolitic limestone, known as Ravenscar Group strata.
Construction - Cross-sectional diagram of the Skivick section of
Wade's Causeway, based on description given in Young (1817) and
Hayes and Rutter (1964)
Cross-sectional diagram of Wade's Causeway, based on description
given in Young (1817) and Hayes and Rutter (1964) The causeway's
visible section on Wheeldale Moor shows the remains of a continuous
surface metalled with closely fitted slabs of sandstone[4] with flat
upper surfaces. The average size of a slab is 45 centimetres (18 in)
square, but some examples are 1.5 metres (4.9 ft) in breadth. The
purpose of a central ridge along one section of the causeway,
described in two independent excavations, is unknown.[6] The stone
flags are seated on a cambered base of mixed gravel, clay[13] and
either rubble, peat or soil, that forms a raised embankment. The
embankment is from 3.6 to 7 metres (12 to 23 ft) wide[6] at its
raised surface. Its width in some sections is increased by 1 metre
(3.3 ft) of ditch to either side, which may or may not be associated
with its original construction, making an approximately uniform
total width of 5 to 8 metres (16 to 26 ft). Its height above
surrounding soil level is approximately 0.4 metres (1.3 ft).
Hayes and Rutter state that the primary purpose of such an
embankment would have been to provide good drainage for a road
surface.[2] Archaeologist David E Johnston states that the structure
is crossed by numerous perpendicular drainage culverts with small
becks trickling through them since the ground is often boggy.[15]
This could suggest a reason for the embankment, and its early
attribution as a causeway—a route across wetland,[16] normally
supported on earth or stone in the form of a raised embankment.
Nineteenth-century antiquarian Thomas Codrington argued that Roman
roads in Britain were generally built on embankments regardless of
the underlying ground's drainage. He states that the common
appellation of "causeway" in the names of Roman roads may,
therefore, relate to their embankments rather than indicate that the
ground on which they were constructed was ill-drained. Some
historians translate Livy's phrase for Roman military construction
of roads, via munire, as "making a causeway".
Johnston, historian Nikolaus Pevsner and landscape historian Richard
Muir all agree that an original gravel surface dressing was once
present on top of the stone of the Wheeldale structure. Whereas
Johnston and Pevsner believe that the gravel was washed away through
weathering,[8] Muir states that human agents were primarily
responsible for its removal. Both agree that the stonework remaining
does not represent the original road surface. Statements by the
eighteenth-century antiquary Francis Drake and nineteenth-century
topographer Samuel Lewis that the writers found it to be "paved with
a flint pebble" may support this theory,[9] although Hayes and
Rutter cast doubt on the accuracy of Drake's reports. Codrington
states that in 1817 the causeway consisted of a "strong pavement of
stones ... [with] above these another stratum of gravel ...", Hayes
and Rutter state that "traces of a surface layer of gravel and small
stones" remained visible in the 1960s, and professor of structural
engineering John Knapton states that there remained some evidence of
smaller surface-dressing pebbles as late as 1996. Codrington and
archaeologist Frank Elgee consider the structure was flanked in a
few sections by lateral parallel ditches but Hayes is doubtful
whether they were part of the original construction or if they even
existed.
The structure is believed by several writers to extend far beyond
its visible portion, but no significant sections of its conjectured
course remain visible to the naked eye or have been excavated or
extensively surveyed, and there is little agreement on an exact
course that an extension may have taken. The total original length
of the structure is therefore unknown, but may have been up to 25
miles (40 km).
Early records of the causeway's course to the north—when its remains
were apparently more readily visible than today—differ considerably
from one another: the early geologist and natural historian George
Young, who wrote in relation to the causeway in his History of
Whitby, makes no clear mention of the route of the structure north
of Wheeldale Moor; it is unmarked on the 1854 Ordnance Survey map of
the area; and eighteenth-century historian Thomas Hinderwell's
mention of it passing near Hunt House suggests a greatly differing
route to that marked on 2012 Ordnance Survey mapping. At least one
source states that a "conjectural" continuation to the north is
visible in vertical aerial photography. Hayes reports that in his
survey in the 1950s, he found "trace of the embankment" in one short
section and "a patch of the metalling" in four additional sections
along a route past Hazle Head and Julian Park.
Beyond Julian Park, it has been conjectured that the structure
originally continued to the Roman garrison fort at Lease Rigg, south
west of Sleights, based on reports from antiquarians in the
eighteenth and nineteenth centuries that fragments were visible at
numerous points along this course. Hayes and Rutter appear confident
of the structure's extent as far as Lease Rigg, but admit that its
extent is conjectural from well short of that point, from Dowson
Garth Quarry northwards.[33]
Numerous authors have conjectured that the structure was a road that
continued past Lease Rigg all the way to Roman coastal
fortifications or signal stations somewhere near Whitby, but this is
debated. Drake reports in 1736 that an associate had followed its
course from Wheeldale Moor to the coast at Dunsley Bay, but
Codrington is dismissive of his account, and whether the author
meant to imply that a visible structure had been followed, or simply
that the associate had followed a proposed route without
encountering it, is unclear. In either case, the author did not
verify sight of the structure along this course himself. Several
sources after 1805 report the same endpoint for the road but it is
unclear whether they are echoing Drake or had visited the site
themselves. Several authorities state that any termini beyond Lease
Rigg are "doubtful" and "unproven", and Elgee states that the
causeway's northern course "is obscure and its termination unknown".
Hayes and Rutter in 1964 found no evidence for a continuation of the
structure any further north than Lease Rigg. Other authorities argue
for possible courses extending northwards to Goldsborough,
Guisborough, or Sandsend Bay.
It has also been suggested that the structure originally extended
southwards from Wheeldale Moor to link up to the Roman Cawthorne
Camp (sometimes spelled 'Cawthorn'). In the twentieth century
English Heritage identified two sections of ground on Flamborough
Rigg and Pickering Moor as extensions of the Wheeldale structure.
Hayes states that the Flamborough Rigg section remained "clearly
visible" as late as 1961, and that additional sections near Keys
Beck were visible in aerial photography from 1946. The accounts of
Hinderwell, Young, and Hayes & Rutter, as well as the 1854 and 2012
Ordnance Survey maps, appear to corroborate the stated course of the
structure along this section.
There is further conjecture that the original structure's course may
have gone beyond Cawthorne Camp to the Roman settlement of Derventio
Brigantum (possibly either Stamford Bridge[19] or modern-day
Amotherby near Malton). Any postulated extension further south than
Cawthorn is contested. Hinderwell reports in 1811 that the late
Robert King had found evidence of a continuation of the causeway
between "Newsom-bridge" and Broughton (a former township located
near Appleton-le-Street). Hayes and Rutter failed to find any trace
of the causeway south of Cawthorn along a route via Amotherby,
Barugh or Newsham in their survey in the 1950s, and note that its
course could not be determined as early as 1726.
Beyond Malton, there is a postulated stretch of Roman road leading
towards York, which it is possible may be an extension of the
causeway. Evidence for it is very slim: it is mentioned by Drake in
1736, but Codrington could find no trace of it in 1903, and writes
that there is "some uncertainty as to the connexion". Archaeologists
Philip Corder and John Kirk reported a possible section of Roman
road at Brandrith Farm (grid reference SE 698692) in 1928, but it is
unknown whether this relates to the same structure as Drake
observed, or has any association with the Wheeldale structure.
Historian Hector Munro Chadwick states that historical explanations
for ancient structures would have been known to educated clergymen
from the seventh century, but that structures were generally named
by less educated people, often after mythological characters. Oral
folklore in the North York Moors area from the Early Middle Ages has
not generally survived into the modern era, but social historian
Adam Fox states that the attribution of the causeway to Wade existed
in oral folklore dating from at least as early as the Renaissance
era. The folklore held that the causeway was built by a giant called
Wade[6] for his wife to take her cow to either market or pasture. In
1890, historian Thomas Bulmer records that Wade is represented as
having been of gigantic stature ... His wife ... was also of
enormous size, and, according to the legend, carried in her apron
the stones with which her husband made the causeway that still bears
his name.
The legend of Wade and his wife are reflected in alternative names
for the structure that include "Old Wife's Trod", "Auld Wife's Trod"
and "Wade's Wife's Causey". The folklore of Wade was still common
locally in the early nineteenth century. There is some confusion as
to whether the name Bel or Bell relates to Wade's wife, or to his
cow. Bulmer refers in 1890 to "[Wade's] wife, Bell" and Young also
assigns the name to Wade's wife in 1817. Hayes (1964) accepts this
attribution but antiquarian Hilda Ellis Davidson believes that the
folkloric Bel refers to Wade's cow and reflects an earlier tradition
of the "fairy" or bountiful cow.The earliest published source of the
legend, from 1779, is ambiguous and refers to "Bell Wade's cow".
Etymological history of early names: Several of the earliest sources
refer to the structure as "Wade's Causeway", "Wade's Causey", and
"Wade's Wife's Causey". The word causeway derives from the earlier
English causey way or simply causey. Causey derives from the Middle
English cauci, which derives from the Anglo-French causee, itself
derived from the Medieval Latin calciata ("paved highway"), which
ultimately may derive from the Latin calx (meaning "heel"). The
derivation from calx can most likely be explained by the practice in
the Ancient Roman era of consolidating earthworks through trampling
with the heel of the foot.
Origin of the name Wade: It is not known for certain who the
causeway is named after, but the figure was at the latest
pre-Renaissance, and the majority of sources agree that it has its
origins in the medieval period or earlier. The name Wade appears as
one of the most common surnames in a 1381 poll tax register from
Suffolk, and philologist P H Reaney reports multiple instances of it
from the 11th and 12th centuries. The names Wade or Wada were common
in pre-medieval English history and historian William Searle records
around a dozen historic Wades in his Onomasticon of early
Anglo-Saxon names. The earliest figure from the region identified as
Wade in extant writings is Duke Wada, a historical personage of
Saxon descent who is recorded in 1083 as having been a prominent
figure living in the Yorkshire area around 798. It is possible that
this person was either named after—or has been conflated over time
with one of several earlier, mythological figures known as Wade.
Chadwick states that it is most probable that the causeway is named
directly after a well-known mythological, rather than historical,
Wada.
The earliest origins of tales relating to a mythological Wade are
confused and diverse. Linguist George McKnight states that the epic
of Wade, although becoming a "mass of tales ... of the most diverse
origin imaginable", was one of only a few clear examples of an epic
from the Early Middle Ages surviving into Middle English. Geoffrey
Chaucer, writing in the fourteenth century, makes reference to early
English legends of Wade but these no longer exist in their complete
form. Walter Map, writing in the twelfth century, also mentions a
Vandal prince Gado (thought to be a Latin form of Wade) in his
fantastical lay De Nugus Curialium.
The Wades in these early English works likely relate to one or more
earlier legendary figures known as Wade, or variations thereof, in
Northern European folklore and legend. Various authors suggest links
to: the giant Vađi, (also known as Witege, Vathe, Vidia, Widga,
Vidga, Wadi or Vade) mentioned in the Norse Saga of Bern in the
Ţiđrekssaga; the Danish hero Wate, also called Wada; the Anglo-Saxon
deity Wōden (also Wōđanaz or Wōđinaz), who was historically referred
to as "heaven's giant"; and the German figure Wa-te, a fierce
sea-king similar to Neptune, who reigns in Sturmland in the
7th-century saga Kudrun. Nurse and Chadwick identify all the above
figures as being later facets of a single legendary character
present in an early, shared mythology of tribes living around the
rim of the Baltic and North Seas. There are possible etymological
links between Wade's causeway and other UK archaeological sites:
Wade's Gap on Hadrian's Wall in Northumbria; the Wansdyke that runs
between Wiltshire and Somerset; and Wat's Dyke in the Welsh borders:
all three have pre-modern origins and the latter two have sections
contested as Roman in part.
It is thought that Skivick or Skivik, the local name for the section
of structure visible on Wheeldale Moor, could derive from two
morphemes from Old Norse. The first syllable could derive from
skeiđ, which could mean either a track or farm road through a field,
or from a word used to describe a course or boundary.[ The second
syllable could derive from vík, meaning a bay or a nook between
hills. Scandinavian or Norse place-names are common in Yorkshire and
Norse peoples settled in the Yorkshire area from 870 AD onwards
following raiding over the previous seventy years.[69] Sawyer states
that early Norse colonists had a profound effect on place-names in
the areas in which they settled. Sedgefield states that the skeiđ
derivation specifically in place-names within northern England
points to Scandinavian settlement of the area, but that due to the
inheritance of language across generations, a place-name containing
skeiđ may in any individual case have been applied any time between
the ninth and fifteenth centuries. Historian Mary Atkin states that
skeiđ place-names appear near Roman sites frequently enough to
suggest an associative link.
Theories on structure's origins and purpose: A wide variety of
interpretations for the structure have led, in the absence of any
hard evidence, to a broad range of proposed dates for its
construction, from 4,500 BC to around 1485 AD. In archaeological
excavations, no coins or other artefacts have been found on or
around the structure to aid its dating, and no evidence has been
gathered as of 2013 through radiometric surveys. This has led to
great difficulty in establishing even an approximate date for the
causeway's construction. Attempts to date the structure have
therefore relied on less precise means including etymology,[55] the
structure's probable relationship in the landscape to other
structures of more precisely established date and function, and the
comparison of the causeway's structure and fabrication to structures
such as Roman roads.
One objection to identifying the road as Roman was that, based on
readings of the Iter Britanniarum—the section of the 4th-century
Itinerary of Antoninus that lists major Roman Roads and stations
within Britain—there had never been any major Roman roads in the
area. In 1817, Young attempted to address this problem by arguing
that the course of one of the identified had been misinterpreted and
ran between Malton and Dunsley, passing through Wheeldale.[96] Such
an argument was possible because the Iter Britanniarum was not a
map, but rather a list or itinerary of roads and their distance
between various settlements. Roman names for settlements were used
in the document and, since many of these named sites had not been
conclusively matched to contemporary settlements, identification of
exact routes listed in the Iter was often difficult. There were few
other objections at the time to the causeway's identification as a
Roman road and by the twentieth century the causeway was commonly
being referred to as the "Wheeldale Roman Road", or "Goathland Roman
Road".
There was also support for the identification of the structure as a
Roman road on etymological grounds. The early twentieth-century
literary scholar Raymond Chambers argued that the name "Wade's
causeway" is an example of Angle and Saxon settlers arriving in
Britain and assigning the name of one of their heroes to a
pre-existing local feature or area: if his argument that the
structure was given its current name sometime during the Saxon
era—between approximately 410 and 1066 AD is accepted, then it must
have been constructed prior to these dates. Atkin reaches a similar
conclusion, arguing that the Norse morpheme skeiđ that is a partial
root for Skivick, a local name for a section of the structure, is
commonly found amongst Roman structures that are discernible by
later Saxon or Viking settlers. Hayes and Rutter also identify the
structure as a Roman road, but using a quite different etymological
argument: they state that there is an absence among the names of
settlements along the causeway of the Anglo-Saxon morphemes ceaster
and stret and that, as per Codrington, these morphemes would be
expected to be found in the names of several sites that lie
alongside a former Roman road. They conclude that the absence of
settlements with such names along the postulated extended course of
Wade's Causeway indicates that the structure must already have been
abandoned and of little significance by the Anglo-Saxon period (c.
400–600 AD), most likely by around 120 AD, and must therefore be of
early Roman origin.
Several authorities who accepted the structure's interpretation as a
Roman road attempted to make more precise estimates of the date of
its construction by identifying periods of Roman military activity
in the region, since the majority of Roman roads were of military
construction. Historian Albert Norman, writing in 1960, states that
the Wheeldale structure most probably dates from either the first or
fourth century AD[89] but most sources appear to favour a
first-century date: both historian Brian Hartley and Hayes & Rutter
estimate around 80 AD; and Elgee estimates 86 AD. The earlier,
first-century, estimates assume that the road is Roman and that
Roman road-building in the region occurred around the time that
Gnaeus Julius Agricola was the Roman governor of Britain. Agricola
made a concerted effort to expand and consolidate Roman control over
lands of the Brigantes tribes in the North York Moors area in the
80s AD[64] and is thought to have ordered the construction of nearby
Lease Rigg fort. The fourth-century estimates, by contrast, assume
that the tribes in the North York Moors area were either bypassed or
subdued in the first century but that, being of little importance
strategically, their lands were not subject to Roman occupation or
construction until the fourth century. A second wave of Roman
military activity appears to have occurred in the region during this
later period in response to new military incursions and raiding by
Saxons, Picti, Scoti and Attacotti. The east coast of the North York
Moors area formed the northern flank of the Saxon Shore defences
believed to have been constructed against this perceived threat.
The above explanations all place the causeway within a Roman
military context. An alternative, or perhaps secondary, usage for
the causeway in Roman times is suggested by landscape author Michael
Dunn and others, who state that it may have been constructed for the
transport of jet inland from Whitby.[67] Hayes and Rutter are
dismissive, stating that the value of jet mined in the Roman period
would not have justified the expense of the causeway's
construction.[99]
A possible issue with the causeway's identification as a Roman
structure in the latter half of the twentieth century was its
incorporation of many small bends along its course. Roman military
roads are usually straight in both their overall course, and also
typically from one vantage point to the next. Both the Foss Way[102]
and the Stanegate, roads of established Roman provenance, have
sinuous courses similar to Wade's causeway, so the objection is not
conclusive.
The use of dressed stone rather than gravel as a surface dressing
was also occasionally held to be a sign against the causeway being
of Roman construction: the majority of Roman roads that were
finished with a material other than simple packed earth were dressed
in either packed gravel or pebbles. There are other examples of
Roman roads paved with stone blocks, including the 11 miles (18 km)
section of the Via Appia—the oldest major Roman route in Italy—near
Albano. Historians Richard A Gabriel and Michael Grant state that of
the 400,000 kilometres (250,000 mi) of known Roman roads, over
80,000 kilometres (50,000 mi) may have been stone-paved. The Roman
writer Ulpian specifically differentiates between via munita, which
always had a paved stone surface, and via glareata, which were
earthed roads with either gravelled surfaces, or a gravelled
subsurface and paving on top. The causeway may well have had a
gravel surface dressing originally, which has been removed since
through robbing and natural weathering. Another difference in
construction detail between Wade's Causeway and a typical Roman road
is its lack of a foundation of large stones. Codrington and
archaeologist John Ward stress that the structure of Roman roads
varied greatly depending upon their situation and the materials
available, especially within Britain.
For much of the twentieth century, the consensus remained that the
road was most probably Roman. It was still referenced as an
undoubted Roman road in a 1947 UK Government report and in 1957
Margary, the leading authority on Roman roads at the time, accepted
the road as Roman and assigned it the catalogue number 81b in his
list of Roman roads in Britain. In the late 1950s and early 1960s
this was a definitive and unquestioned interpretation of the
monument.[75] Several works in the 1980s and 1990s stated that
Roman-era road construction was still the most probable explanation
of the structure.
Whilst nineteenth- and to a lesser extent twentieth-century
attitudes often suggested that any well-constructed pre-modern road
surface must be Roman, late twentieth-century archaeologists were
more open to evaluating the structure within the context of a wider
span of historical periods. After an early allowance by Phillips in
1853 that the causeway could be British rather than Roman[109] there
was little further investigation of such a possibility. In 1994, the
Royal Commission on the Historical Monuments of England began a
review of the date or origin for the Wheeldale causeway. Detailed
air photography of the Cawthorn camps in 1999 site failed to find
evidence of a road leading towards Wheeldale Moor from the camps to
which it is historically related,[111] and the causeway does not
obviously connect to the main Roman road network. Several writers
around the turn of the millennium began to express doubt about the
established narrative for the structure as a Roman road.
Twenty-first century archaeologists then found several exemplars of
other cambered, metalled roads that pre-date the Roman presence in
Britain, and hence set precedence for the possibility of a pre-Roman
origin for the Wheeldale causeway. Several sources from the
mid-1990s onwards have suggested that the structure may be a
pre-Roman (Iron Age) road of uncertain route or purpose.
Blood and Markham (1992) have proposed an interpretation of the
structure as a post-Roman (medieval) road, possibly relating to the
wool trade, although this is harder to reconcile chronologically
with etymological explanations for the structure's naming. English
Heritage state that it is "quite possible" that the causeway was
used as a road during the medieval period despite being built much
earlier. Similarly Hartley, whilst accepting the structure as a
Roman military road, believes it is unlikely that the causeway
immediately fell out of use once its military use ceased. Drake
recorded that by 1736 the causeway was "not now made use of", but
there is no historical record covering its possible use as a road
during the medieval period.
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Whitby
and Scarborough Index
Pictures of North Yorkshire, England
docspics photos
images © Dr Phil Brown
Whitby and Scarborough
between the sea and
the edge of the North York Moors, North Yorkshire
Northern England * docspics photos
images pictures photographs of Roman Road Wheeldale Moor © Phil Brown * Tourist information Top tourist
attractions, self-catering holiday cottages, luxury hotels, B&B,
hostels to suit all budgets, pubs, inns, dining out, coach tours, varied
tourist attractions, cafes, restaurants,
eating out, quality local food, historic towns, pretty villages, museums, weekend-breaks,
museums, historic churches buildings, good places to stay for walking
holidays, outstanding scenery in the area, friendly people, interesting
walks, weekend-breaks docspics images photos
of Roman Road Wheeldale Moor © Phil Brown Tourist information on Roman
Road Wheeldale Moor, top tourist
attractions near Roman Road Wheeldale Moor Things to do near Roman Road
Wheeldale Moor, What to see near Roman Road Wheeldale Moor, Walks
near Roman Road Wheeldale Moor, weekend breaks near Roman Road Wheeldale
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Moor docspics images photos of Roman Road Wheeldale Moor © Phil Brown Tourist information on
Roman Road Wheeldale Moor, top tourist
attractions in Roman Road Wheeldale Moor Things to do in Roman Road
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Holidays in the
North York Moors National Park, interesting places to visit in the North
York Moors an areas of outstanding natural beauty, good places to say in
the North York Moors, pretty villages and scenic walks in the North York
Moors, holiday cottages in North Yorkshire, weekend breaks in luxury
hotels in North Yorkshire, places to dine out in North Yorkshire.
seaside holiday bookings for Whitby, seaside holiday bookings for
Scarborough, hotels and holiday cottages in Whitby, hotels and holiday
cottages in Scarborough |
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