Monday, July 20, 2026

The Vole at Skara Brae


The Vole at Skara Brae 



There follows edited extracts from a research document about the bones of rodents that were found at Skara Brae. 

It details the volumes of vole and mice bones found in midden materials,  both inside and outside the monument, drawing conclusions about the possible utilisation of the vole as a food item.

The report is :-

Rodents: food or pests in Neolithic Orkney, by 

Andrzej A. Romaniuk, Alexandra N. Shepherd, David V. Clarke,  Alison J. Sheridan,  Sheena Fraser, László Bartosiewicz, and Jeremy S. Herman.

The Orkney archipelago, situated to the north of the British mainland, is renowned for its outstanding collection of Neolithic sites, a core group of which have been recognized with World Heritage status.

Among the wealth of material recovered from the Orcadian Neolithic sites are copious rodent remains from two settlements, one the celebrated site of Skara Brae, and the other Links of Noltland, Westray. 

These remains are from contexts that have been radiocarbon-dated to the late fourth and early third millennium BC, using either the rodent remains themselves or other associated bone material. 

Most are from the Orkney vole, a form of the European common vole Microtus arvalis (Pallas, 1778) that is found on some islands of the archipelago, where it is isolated from its nearest conspecifics in mainland Europe. The rest are from the wood mouse Apodemus sylvaticus (Linnaeus, 1758), a common species found throughout western Europe and mainland Britain.

Neither could have survived the Pleistocene glaciations in this location and it is generally accepted that small mammals were subsequently introduced to Orkney by human agency. 

The excavations in 1972–1973 and 1977 at Skara Brae yielded over 1.1 kg of sieved micromammal bone material, of which 815 g could be attributed to rodents. The excavations comprised four trenches (I–IV; figure 1), whose location and good preservation provide a remarkable opportunity to study both the human and natural deposition of remains. 

 


Trench I and its stratigraphy represents an undisturbed area inside the settlement complex, covering three phases (phase 0, 1 and 2) of human inhabitation, lasting from ca 3360 to ca 2440 cal BC, with a hiatus of some length (possibly as much as 300 years) between phase 0 and phase 1. Trench II represents the build-up of deposits at the northeastern edge of the settlement, dating from ca 2900 to ca 2490 cal BC. Unlike Trenches I and II, which are located within the core and periphery of the main settlement, respectively, Trenches III and IV were excavated 30–45 m to the west of the modern guardianship area around the settlement. These latter trenches showed only basal survival of in situ occupation deposits; otherwise they mainly comprised natural accumulations of sediments, principally sand with some redeposited anthropogenic material associated with interludes of plough cultivation. The dating reflects this, with dates for the basal in situ deposits lying between 2880 and 2470 cal BC, with later material from around 2300 to 2040 cal BC and much later activity still between cal AD 600 and 900.

The sieved microskeletal material included 816 g of identifiable rodent remains. These comprised 30 524 skeletal fragments, including 8369 isolated teeth, attributable to at least 1674 individual animals. Only two species were identified, Orkney vole and wood mouse, supporting the notion that only these two rodents had been introduced to Orkney by the time of the Neolithic.

 


The evidence from Skara Brae indicates that the accumulation and burning of Orkney vole remains were most likely the result of deliberate actions by the inhabitants of the settlement, carried out over a considerable period of time, and the most plausible explanation is the utilization of the voles as a source of food. It is notable that the rodent remains were not found in isolation, but within deposits that contained waste products from a range of other foods, including mammals, fish and shellfish. The presence of bones within the hearth deposit itself may be due to roasting of voles between the embers, as previously seen in two other regions of the world, South Africa and Patagonia. Another possibility is cooking or boiling of animals in a pot, known from some ethnographic studies and also suggested for assemblages from the Pampean region in Argentina. In all of these cases, the burnt elements include mandibles and teeth, as in the case of the Skara Brae material. The predominance of older individuals in the sample from Skara Brae may point towards selective or seasonal ‘hunting’, which would not require any more sophisticated techniques than pit-trapping. 

It is also possible that the vole remains are the outcome of agricultural pest control, although it is unlikely that this was their only source, given their location and intermingling with household refuse.

The presence of Orkney Voles on Orkney in prehistory has only been noted in archaeological contexts where the primary question is to establish the presence of humans.

I have suggested elsewhere that it is likely that the vole was surviving in cold, but ice-free locations east of Scotland and Orkney through the last glacial maximum, and the following deglaciation. 

It is possible therefore that the vole may not have been brought to Orkney by humans, but arrived on its own feet at any time after the retreat of the ice sheet over Orkney. 

The relative abundance of mice and voles, as demonstrated in the graphic suggest that there are background populations of voles in external areas around Skara Brae, in areas where there are relatively few mice.

In contrast, the background population of mice is in the structures of Skara Brae. 

There are also high intensity populations of voles also within the buildings. 

Initially I was skeptical about the idea that voles were a potential food item, but as the idea that these people were likely to be comparatively underresourced survivalists as castaways on Orkney developed, I began to reconsider.

Finding that mice were a common co-inhabitant of Skara Brae dwellings suggests that they were a very present feature of life in neolithic Orkney. It is highly unlikely that this mouse population was a welcome guest, and more likely to have been an outright pest.

In light of that ,some interesting features of the architecture of the dwellings suggest how neolithic people adapted to the invasion of rodents.

Besides the risk of being walked over by tiny feet in the middle of the night, the major risk from the mice would have been two-fold, firstly, eating their stored food, and secondly defacating in the stored food that they didn't eat.

As a result of this very real threat they may have developed a couple of counter measures which we find at Skara Brae. 

 

 


 
A well designed "dresser" would present a significant obstacle to the trespass of mice onto a food storage area. A wooden version of this can be found in the Kirbuster Farm Museum in Orkney which was built in the 18th century,  a piece of furniture that performed the same function up until the early/mid 20th century. 

 


The other major defence against rodent transgression was the lidded container.

Fixed versions of these were the cut into the floor of Skara Brae dwellings. These would have been designed with a lid which would be lifted to access the contained food within.

A more obvious example of the lidded container is the bucket shaped pottery that was developed at around this time.


  


These vessels were also furnished with lids, finely worked stone discs of thin stone, like the item that is propped up against the bedding place wall in the image below. 

  


It's quite likely that the development of the dresser and the development of flat based pottery are not entirely coincidental.

The pottery that precedes bucket shapes was round based which would not sit well on a dresser, and it is possible that for some reason mice were a less serious problem in the earlier years of the Neolithic migration into Orkney. 

A different approach to food is also possible, flat based pottery intended for long term storage, while round based pottery was used for freshly gathered ingredients. 

This might tell us much about the lives of the people who lived in grouped settlements, as compared to those who lived in the more isolated mainland settlements.

Jeffery Nicholls 

South Ronaldsay 

Orkney 

Jiffynorm@yahoo.co.uk 



Friday, July 17, 2026

Relative sea-level

 



Orkney Riddle 


Relative Sea Level


Relative sea-level describes the change in sea level relative to the shorelines of the world's continents. Many countries with a shoreline have undertaken offshore surveys to establish a graph that relates present sealevel to those at prehistoric dates in the last 10,000 to 20,000 years.

For Britain this work was carried out by a team headed by Ian Shennan.

The results for their work are published as:- Relative sea-level changes and crustal movements in Britain and Ireland since the Last Glacial Maximum by Ian Shennan, Sarah L. Bradley, and Robin Edwards

They introduce their results as follows:-


The new sea-level database for Britain and Ireland contains >2100 data points from 86 regions and records relative sea-level (RSL) changes over the last 20 ka and across elevations ranging from ~þ40 to -55 m. It reveals radically different patterns of RSL as we move from regions near the centre of the Celtic ice sheet at the last glacial maximum to regions near and beyond the ice limits. Validated sea-level index points and limiting data show good agreement with the broad patterns of RSL change predicted by current glacial isostatic adjustment (GIA) models

Their graphic presentation of the dates and heights of the 2100 individual data points is presented below:-


 


A more detailed series of graphs has been modelled by the authors to present change in sea level over time as a linear process.

In this interpretation, in some places sea-level has risen more or less consistently over the last 20,000 years.

In others it has fallen, and in some it has remained somewhat the same.

Further modelling attempts to demonstrate how the presence of ice on Britain forced the mountains down into earth's crust, and how the ice sheets were then compressed to force them to flow from the highlands of Scotland, Wales, Ireland, and Northern England out to the Atlantic Ocean and the North Sea 

 

From "Flow pattern evolution of the last British Ice Sheet by Anna L.C. Hughes, Chris D. Clark, and Colm J. Jordan

This is a projection based on the idea hat snow laid a thick ice sheet on Britain, forcing glaciers to cut glacial valleys out towards the coasts.

-×-

The graphic of individual terrestrial and freshwater data points separated out from the graphic above is shown here:-

These red data points are at locations close to the coast. The most extreme top limit for freshwater water at a coastal location is at 15,000BP when a sample appears at well over 100 metres above the level of the sea at that time. [Sea level here is marked by the lower edge of the group of points, beginning here at 40 metres below sea level at 10,000BP, and rising to zero today]. In fact it is likely that all the data points for terrestrial freshwater are in effect either meltwater or, more recently, river water.

At 10,000BP, the last blast of deglaciation, the depth of meltwater draining offshore at some locations exceeded 50 metres. That is 50 metres above sea level where it was at that date.

This is all freshwater traversing down stream, in one direction, away from land.

Further though, the rate of meltwater flowing off the mountains and towards the sea will have changed through an annual cycle, peaking at midsummer and falling back to a trickle in winter.

 


The blue symbols in the graphic above represent locations where evidence of marine organisms have been found, and the dates and elevations of these suggest that sea level relative to land here rose significantly above global sea-level at that time. 

The above chart marks the dates and levels of marine and terrestrial/freshwater samples in the Clyde Valley in Scotland, without the modelled guidelines that suggest how sealevel in that location changed over time, in a linear manner. 

Global sea levels for some of the data points are measured and calculated as follows, and the distances above sealevel, of the samples, are added to these values. 

17,000BP 100+ metres below

14,000BP 80 metres below 

11,000BP 50 metres below 

7,000BP 10 metres below 

5000BP 5 metres below 

The prehistory of this area of coastal land began at 17,000BP when marine water reached 130 (100+30) metres above sealevel as it was at that date.

At 14,000BP seawater reached land at 95 (80+15) metres above the sealevel as it was at that date.

At 11,000BP freshwater rose to 80 (50+30) metres above prehistoric sealevel. At the same time marine water was lapping shores at 50 metres above prehistoric sea level. 

At 7000BP marine organisms are registered at 15 (10+5) metres above sea level at 7000BP. 

At 5000BP freshwater organics are found at 10 (5+5) metres above sea level at 5000BP. 

Some explanation is required, for what is happening at around 11,000BP when there are both, freshwater sample locations, and marine sample locations present in the same area at the same time. 

(Given a lack of detailed information i have to assume that both marine and terrestrial samples were located on verifiable ancient shorelines)

The freshwater sample is 80 metres above prehistoric sealevel and the marine is 45 metres above prehistoric sealevel. 

-×-

The blue symbols, representing marine transgressions, are present on a select few of the charts, in locations in Scotland and Ireland. These are the data points that scientists use to model prehistoric sealevel as a gradual linear event.

Some of those charts are presented here, the munber refers to Shennan et al, and the date is that of marine transgression in that location:-

The locations are:-

Scotland 

13 north east Scotland 18,000 BP

15 Montrose 14,000BP

16 Tay Valley 15,000BP 

17 Forth Valley 15,000 BP

19 Ardyne 15,000 to 11,000BP 

20 Clyde 15,000BP to 7000BP

22 SE Scotland 6000BP

Ireland (not considered in detail below)

59 Solway Firth 10,000BP

84 West Cork global

88 Shannon Inner, global

91 N Mayo 20,000 BP

95 Lough Swilly 20,000 to 17,000BP

96 Derry 8000BP 6000BP 

97 N Antrim 8000BP

98 N Down 15,000BP 2000BP

99 S Down 17,000BP 7000BP 3000BP

100 Dundalk 20,000 to 17,000 BP 



The locations of most of the sample locations are visible in the map above. Only those that are circled are considered in detail. 

-×-

Aberdeenshire 


Source location 13 is on the Northeast coast of Scotland in the county of Aberdeenshire. The samples that were found and dated were at a location that was about 12 metres above our sea level.

The date for the samples is around 18,000BP, and sealevel at that date was more than 100 metres below present sea level. 

At this time ice-sheets were still settled on Scotland and in the middle of the North Sea, but Shetland had probably lost its ice sheet after 50,000BP. [4]

A large embayment separated Shetland from a promontory ridge along the east coast of the Norwegian channel. This embayment extended south as far as Orkney and the North Coast of Scotland 

Owing to this topography it would have been possible for the instability of sediments in the Atlantic Ocean north of Shetland to cause a tsunami, like the Storegga Submarine Landslide to dump material on the Aberdeenshire coast. 

Location 13 is close to another site that was studied by David Long where geological deposits were defined by him as caused by the Storegga Submarine Landslide.

The Storegga Slide happened in 8150BP but was preceded by the Nyegga Slide, from the same undersea source, possibly in 18,000BP

The Nyegga Slide is recorded in "Revised Storegga Slide reconstruction reveals two major submarine landslides 12,000 years apart" by Jens Karstens et al

Based on their observations of the Storegga area, the authors suggest an updated reconstruction of the present-day slide scar. At ~20,000 BP, more than 35 m of rapidly deposited and presumably poorly consolidated glacial sediments failed during the Nyegga Slide. The Nyegga slope failure mobilized sediments deposited between >30,000 and ~20,000 BP, forming the Nyegga discontinuity (ND) that likely corresponds to the internal boundary in the deposits in the northern sidewall and the top of the intact block in the slide scar infill.

At ~8150 BP, parts of the sediments deposited after the LGM failed during the first phase of the Storegga Slide

It is difficult to constrain whether the Nyegga Slide was a local event limited to the northern margin of the slide scar, or a regional event. However, at least three sediment cores from the southern slide scar segment also show indications for LGM slope failure, with C49 showing ~18,000 BP sediments beneath Storegga Slide deposits and C75 even including LGM mass-transport deposits (Fig. 4f, g). While this may indicate that the Nyegga Slide affected the entire Storegga Slide scar area, this is far from certain due to a lack of conclusive evidence for large stretches of slide scar. Based on the available data, we observe that ~70% of the 50 m that failed at the northern margin of the scar failed during the Nyegga Slide, and not during the Storegga Slide, indicating that the Nyegga Slide was a major failure event.

-×-


The Great Glen 

 The following group of locations are in the Great Glen that joins Glasgow, across Scotland to Edinburgh. They are:-










Locations 15, 16,17,19,20 are sampled along the valley which will have been the main drain route for the release of meltwater from the Scottish Highlands at the peak of deglaciation. 

The amount of freshwater entering this valley from the mountains will have been measurable in cubic kilometres per day at the peak of the hot period which saw the most destructive ice-sheet retreat. [1]

This amount of meltwater would have drained into the valley during the hot summers, and drained away, into neighbouring seas in autumn and winter.

The level of water flowing through the valley will have risen and fallen in phase with the seasons. 

In winter, as reduced flows of meltwater were entering coastal waters from the mountains Atlantic storms were generating huge waves and subsea currents that shredded reed beds in inshore waters creating huge floating rafts of uprooted seaweed. 

As sealevel rose and fell these rafts were dragged into sheltered embayments and left stranded on raised beaches. They carried with them the shells of crustaceans and the bones of fish and birds, anything that was caught up in the seafloor environment. 

Winter still brings these floating rafts, and often the bladder wrack, for instance, is actually attached to the shells that are caught up in it.

This phenomenon is likely to have led to the deposition of shells and organic matter at heights well above the local tide line at times when the amount of meltwater escaping to the sea raised water level, not only above global sea-level in prehistory but also above our own present day sealevel. 

 


This is a huge dump of uprooted seaweed on an Orkney beach after a severe winter storm. (My Yorkshire Terrier for scale!)

A fresh tideline, with higher tide lines up the beach


 Mussel shells caught up in the uprooted seaweed of the tideline. 

Mussel shell with strands attaching it to the uprooted tideline debris.


East Lothian 



Location 22 is in East Lothian, near Edinburgh, Scotland. The date of the sample is comparable with the Neolithic period of human prehistory, and the altitude is just a metre above present day sea-level, but also perhaps 10 metres above prehistoric global sea-level.

I cannot hazard a guess that suggests a cause for this deposit. The time of the event though is the period in which the North Sea was developing and when the Dover Strait was being eroded through, joining the English Channel with the North Sea. 


Ireland 


The sample locations that follow the Irish coast, are at present outside the scope of this enquiry for detailed study. 

It may be sufficient to suggest that the high relative positions of marine samples around the North Channel of the Irish Sea is because this is and was a relatively enclosed area of water with meltwater draining from the Great Glen, and possibly also from Northern Ireland. 

The volumes of meltwater arriving at this area would have been huge, and would have taken significant periods of time to flow out to the Irish Sea and Atlantic Ocean. 

-×-

This research follows a radically altered perspective towards Quaternary history which is outlined in a series of blogs, some of which are detailed here.

The general theory of the glaciation and deglaciation of Britain is recorded in Ice Sheet Britain. [1]

The extent of Doggerland is examined in Archaeology in the North Sea. ]2]

Walkable land in the North Sea describes the land bridge that joined Holland to Norfolk in England [3]

Quaternary Addendum quotes sources for the detailed analysis of events in the North Sea. [4]

Jeffery Nicholls 

South Ronaldsay 

Orkney 

Jiffynorm@yahoo.co.uk 








Saturday, June 27, 2026

Ice Age Story




Orkney Riddle 


Ice Age Story



This is a story of Britain, and north-west Europe, as it passed through several periods of extreme cold, Ice Ages, the formative events that created the landscape we live with.

It is not authoritative, and may be taken with a pinch of salt, but I hope that those who have learned, as I have, the geological history of Britain, will withhold any kneejerk response that may lurk unbidden in their bosoms.

The general territory that the story covers is very roughly the Atlantic coast of Europe, but includes the Alpine mountains of southern France, and the northern mass of Scandinavia. 

Specific areas that are covered are Britain, Norway, and the North Sea. These constitute an area that academia deems to have been covered by thick ice sheets, the British and Irish Ice-Sheet and the Scandinavian Ice-Sheet. These ice sheets are thought by some to have been joined across the North Sea for part of the last ice age.

The theory that is proposed, studied, taught and learned is that the ice sheets over northern Europe, and elsewhere flowed as solid ice Formations along glacial valleys, shaping them as they progressed.

The evidence tells a more nuanced story that has to start several million years ago with the movement of Britain away from Europe.

As the Atlantic Ocean opened up a great chasm between Europe/Africa and North/South America, so Britain pulled away from Norway. The result was that a portion of the earth's crust between Britain and Norway collapsed into the crevice that had opened up, creating a groove in which the North Sea would ultimately develop. 

In the last million years, and possibly before, the planet was cold, reflecting the sun's rays off from polar ice caps. There were brief periods of warmth in which ice sheets collapsed crashing into underlying geology, and dumping huge volumes of sediments across landscapes, and eventually into the waters between the continents.

This process would have raised average sealevel on a continuous basis from a million years ago right up to the present day. 

It is difficult to assess what effect this carving out of geology had on landscapes of today, but evidence of sediments in the Trent Valley confirm that some of them go back a long way into prehistory, with sand and gravel beds dated up to a million years.

The period formally assigned to the last ice age period began at 120,000BP, and lasted until about 10,000 years ago. 

Before 120,000BP, there occurred earliest significant event that is recorded in the geology of the North Sea. An extended warm period melted polar ice sheets causing Sea levels to rise allowing an insurgence of sea water to flood the area now the North Sea. 

This condition seems not to have happened before 140,000BP. 

From this warm interglacial period snowfall began to fall from 120,000BP, continuing until around 70,000BP when there was a sharp thaw. At this time ice sheets on the Pennine Hill of Northern England and the mountains of Scotland collapsed, sending tidal waves across what was probably dry land in the North Sea area, to deposit huge volumes of sediments as Dogger Bank. 

There followed a relatively mild period from around 50,000BP to around 23,000BP.

In this period the ice sheets remained at high altitude on the mountains of England Scotland, Wales and Ireland. But in the lowland regions of southern Britain and Ireland meltwater rivers flowed through a cold, and probably wooded landscape with marshy areas near the coasts. These places were home to cold tolerant creatures like the woolly rhinocerous, and to people using Upper Palaeolithic flint tools making technologies.

Also at this time, the ice sheet on Shetland was collapsing, and some of the meltwater from that event flowed south along the Scottish coast into a lagoon that had been formed by the after-wash from glacial meltwater. 

Ice age snowfall returned, possibly as late as 23,000BP laying a variable thickness of snow/ice across the British Isles and the North Sea. Very little snow built up on the south coast of England, though the South Downs in Kent may have had an estimated hundred metres thickness on it.

Additional thickness over the pre-existing mountain snow sheets raised them further, though it is likely that snow had been adding to these sheets throughout the previous, less cold periods.

The mainland ice sheets on England and Scotland extended off present coastlines a short distance and a high ridge of land joining Dogger Bank to the Atlantic Ocean at a point between Shetland and the Norwegian Channel, supported an ice sheet perhaps 250 metres deep. This would be thicker on the British side, and less so on the Norwegian side, where some heat from the Norwegian Channel reduced snow thickness. 

The lagoon off the Scottish coast, near Aberdeenshire remained unfrozen throughout this return to freezing conditions, supporting vegetation and wildlife. 

From about 21,000BP the very brief cold period at the end of the ice age ended, and a 10,000 year long deglaciation began.

Between 21,000BP and 15,000BP the ice sheets retreated from the English Channel in a north-westerly direction, crossing the South Downs of southern England and arriving at the foothills of western England and Wales.

An ice sheet on Dogger Bank and the peninsula that bordered the west coast of the Norwegian channel in the North Sea also retreated, leaving huge gullies in the north of the area, as the Witch Ground, off the Scottish coast.

At about 15,000BP a very severe input of heat to the environment caused huge amounts of meltwater to be released to coastal waters. This effect may have caused the excavation of annual parallel valleys like those on the Welsh border with Herefordshire. Here the melt would have caused the release of meltwater, possibly in the region of half a cubic kilometre of water every day, with peak melt in summer and least melt in winter.

This release caused the sea level at the local coastline to oscillate, up and down annually, as seasons changed.

The meltwater released carried with it considerable amounts of sand and silt, with rocks and blocks of ice. This stream of ice and mud crossed the British landscape creating features in its path, and leaving sediments where the flow of water slowed.

Where the stream of materials reached water the solids either settled out of the stream, or backed up, forming moraines. 

At sea coasts these moraines were formed as parallel linear features aligned with the rise in line with local and global sea levels. 

At around 11,000BP the last of the mountain ice sheets had collapsed, and water from that event was mostly draining away with little effect on local sea levels, but in the valleys that had been gouged out by the collapse of ice sheets there remained, where the sun was less able to reach, rivers of solid ice. The ice carried the stones and sands that had been gouged out of the mountains and it wasn't until about 9000BP that these began to melt.

Again local water sea levels rose as the ice melted in the valleys, and the debris that had been stored within the glacier simply gravitated to the floor of the valley, remainng now as hummocky moraine.

The lagoon, off the Aberdeenshire coast remained liquid during the last cold spell, and as the meltwater water fell off the mountains of England and Scotland it overfilled and overflowed around the southern coast of the north sea, between Belgium, Holland, Denmark, and Dogger Bank. 

The spine of land that divided the North Sea, north to south was available to mesolithic wildlife and people, and as sea levels rose it was gradually whittled away until in a series of collapses in the 4th millennium BC, more recent, softer sediments in the northern North Sea were easily flushed aside, opening up the whole North Sea. 

Mesolithic people roamed Britain, Ireland, and land now under the North Sea. The area that they would roam was across to the Norwegian Channel, a wide deep water Channel out of the Skaggerak that followed the south and west coasts of Norway. The northern extent of the mesolithic territory was at the Atlantic ocean between Shetland and Norway. There was a coastal inlet to the territory east of Shetland that had a southern shoreline just east of Orkney, and when a tidal wave was triggered north of Norway in around 8200BP it was funneled along this inlet to hit the Aberdeenshire coastline. 

In the middle of this mesolithic territory, now just off the coast of Aberdeenshire, was large lagoon left over from the ice age.

The people who found this landscape followed the post-glacial migration of trees, grasses, herbs, birds, reptiles, insects, and mammals.

As sea levels rose two routes were the last to be closed off, separating Britain from Europe. First to go was a crossing between France and Sussex, and the final division came with the demolition of land east to west between Norfolk and Holland, at some time in the 4th millennium BC. 

Jeffery Nicholls 

South Ronaldsay 

Orkney 

The Orkney Riddle (index here) is a series of blogs promoting the notion that Neolithic people walked from Scotland to Orkney to build the Ring of Brodgar. 

Email jiffynorm@yahoo.co.uk 

#Orkney #archaeology #Neolithic #prehistory #British #SkaraBrae #NessofBrodgar #BIIS ##Britice-Chrono 







Friday, June 26, 2026

About



Orkney Riddle 


 

Jeffery Nicholls 


A Potted History 


I first went digging in 1964.

My first "proper" excavation was in 1968 when I assisted in the excavation of a mesloithic site on Hengistbury Head in Dorset.

I was a "Digger" from 1973 to 1984, and an engineer from 1985 to 2007 when I worked on pipeline excavations for 2 years.

I worked two seasons with G de G Sieveking in 1973 and 1974 at Grimes Graves. 

I worked for Peter White on Ancient monuments from 1977 to 1984.

I worked one season at Wroxeter Roman City for Philip Barker, and two seasons putting in the drains for Wroxeter in 1976 and 1977 for Peter Brown and Peter White.

I directed the excavation of a Dorset Barrow in 1975, in which I completely removed the monument from the face of the planet, and found not a bone, nor a pot, nor a sherd, nor anything that might represent the idea that the barrow was a funerary monument, as i was lead to believe.

I don't think I ever recovered from that, and I have questioned every archaeological theory ever since.

I came to Orkney first in 1980, and moved here in 2019.

Here, I started researching Neolithic Britain, and Orkney.

Not satisfied with the idea that people had boats in Neolithic Britain that could cross the English Channel or PentlandFirth, I researched everything that I could to prove that they did have boats., (yes, they had boats).

Then I set out to prove that they did not need boats. That there was land between Europe and England, and land between Scotland and Orkney.

That led me to uncover the extraordinary story of a small group of Neolithic people who became castaways on each of the British Isles.

Jeffery Nicholls 

South Ronaldsay 

Orkney 

The Orkney Riddle (index here) is a series of blogs promoting the notion that Neolithic people walked from Scotland to Orkney to build the Ring of Brodgar. 

Email jiffynorm@yahoo.co.uk 

#Orkney #archaeology #Neolithic #prehistory #British #SkaraBrae #NessofBrodgar #BIIS ##Britice-Chrono 


@Tea_Break@archaeo.social







Sunday, June 7, 2026

Solving the Riddle

The Orkney Riddle 

Solving the Riddle 

The Riddle of neolithic Orkney is that there are insufficient significant structures on Orkney to support the huge numbers of hands that would have been been required to build the Neolithic monuments there, 5000 years ago.



The Orkney Riddle is a group of  blogs based on this theme. It is named for the strand of undersea shallow beach that leads off east, from the Pentland Skerries, above,  in the Pentland Firth which may be the last relic of land that once connected Orkney to Scotland. This undersea feature is called the Sandy Riddle. 


I started to research the geology of Britain over the last 100,000 years about 4 years ago. I began because I could find no real world evidence that Neolithic people had boats capable of transporting them and their animals across the Pentland Firth to Orkney in numbers sufficient to build the structures in Orkney that they clearly did.

In order to get to an evidence based theory of both the Archaeology and the geology of Britain I had to knock a lot of very worthy theories on the head, and replace them with some things that are more realistic, and grounded in what I saw as “logic”.

This led me to write a long and rambling series of blogs called the “Orkney Riddle”. 

[This research, with its sources, needs to be peer reviewed. I would welcome anybody who had an interest to challenge my work with additional or alternative evidence or interpretation.]

Orkney Riddle is long, detailed and possibly yawn inducing, so I have to take an additional approach, with the hope that people will help me by discussing issues with me, correcting me where I am wrong, and guiding me with their own inspiration. 

It didn't take long for me to cook up a theory with some bits of evidence which could be used to justify my belief that Neolithic people walked from Scotland to Orkney and back, becoming stranded on the archipelago when land joining the two places was removed by rising sea levels. 

When I popped this notion online, just to gauge reaction I was roundly dismissed. Some said “they had boats” others said “they must have had boats”, and one highly placed scholar demonstrated that some prehistoric people had crossed water to camp on an island off the Norwegian Coast. 

Yes, there were boats, big boats in the Mediterranean Sea 5000 years ago, but the Mediterranean is land locked, and only very slightly tidal. 

I was up against a lot of inertia!

A bit later on in my investigation I thought I had enough quite strong evidence to suggest that people were walking between Scotland and Orkney in neolithic Britain. 

I took myself to see if I could talk about this to a proper archaeologist, but when I found one, that person would not even discuss my findings, declaring from the outset that Neolithic people had boats, which I couldn't deny, because its true.

My argument was and is, that the boats that they had would not make a crossing of the Pentland Firth. Rowing across it now would be suicidal, same then!

Said archaeologist obviously viewed me as a crank, which I found a little hurtful, especially as I was offering a smorgasbord of evidence for my theory, and this person offered nothing to support his emphatic refusal to even discuss the topic.

The result of this and all of my setbacks was, and is, to redouble my research and plaster on more layers of evidence. 

To the extent that I am now considering a review of the evidence for the tectonics of the European Continental Shelf of the Atlantic Ocean and how the British isles broke away from Scandinavia and Europe in deep, deep geological prehistory. 

How i got there is a long story.

-×-

The story became complicated by scientific research that found that a vole that is unique on Orkney, the Orkney Vole, was not related to the Common Vole of Britain.  This, to me and the original researchers at the time of me reading the original research meant that the Orkney vole was somehow transported from Belgium to orkney without landing on British soil.

This feat was thought to have been accomplished by boats travelling between the two places, or by animals being castaway on natural floating pontoons.

For me though this looked as if the vole had found a way to transit between mainland Europe and Orkney by walking along land that had remained at a high enough level with reference to ancient sea levels. I decided that this land ran up the centre of the North Sea from Dogger Bank and across to orkney in the northern North Sea,  without touching Britain. 

I set off looking for this land, and thought I had found it. 

Only at the latest stage of the research did I discover that the premise of the original evidence was wrong.

Bones of the same vole have been found in a cave in England. 

In spite of that revelation though I had still found a terrain that would have supported people and animals throughout much of the last ice age.

-×-

The first part of the plan for my research was to find out as much as I could about Neolithic Orkney, reading about the monuments,  the henges, and the excavations. 

I began with Barnhouse on the shore of Harray Loch,  a group of small lightweight structures with a system of drains running into and between them. I looked on the plan that had been drawn, at the channels in the ground, and thought it unlikely these would have been useful during the worst of winter.

I was living in a caravan at the time and knew that if I were to try and walk on a home ground like that in a wet winter I would be arse over tit in short order. I therefore decided that this was probably a summer camp of some sort.

It didn't seem too unreasonable to me to suggest that the people who camped at Barnhouse were a seasonal workforce who were building the Stones of Stenness, or any of the other Brodgar monuments. 

I then turned my attention to the Stones of Stenness, a small stone circle from which a significant number of its standing Stones had been removed. Also, in a couple of places, where we might reasonably expect to find a stone, holes seem to have been dug, but nothing lasting had been placed in them.

Here I concluded that the henge had actually never been completed, and that since the dating for Barnhouse tended to precede 3000BC, that it was likely that work on the project had ended at around that time.

Looking at the Ring of Brodgar I found a much less orderly design of stone circle in which it was very unclear exactly how may Stones were raised for the monument. 

At a place called Vestra Fiold, a stone was found though that was laying flat on ground close to where it had been hewn from bedrock. It had the same size and general shape of many of the remaining Brodgar stones, and again it suggested that any work on the monument itself had been abandoned before its completion.

I then turned my attention to cairns

In Britain these monuments are quite monumental, but in Orkney they become more numerous and alongside simple passage graves, a small but varied group are diverse in their layout and construction,  including the greatest of them all, the Maeshowe Chambered Cairn

Analysing the dates of bones found in these structures i found that the human bones generally came from before 3000BC,  but any animal bones in them usually died sometime after that date. To me this suggested that the idea that the animal bones were associated with the interment of human skeletons was not feasible. 

-×-

Working with the idea that something happened in the North Sea to transform a vast landscape in the area to a seascape I began studying the seabed and coastal features of that area. 

Quite by chance I came across the report of an excavation of a beach deposit in Rogaland,  on the Norwegian Coast on which the roots of an Alder tree were found where the tree itself had been ripped away, leaving only said roots.

It seemed reasonable that this broken tree would have been subject to some sort of tsunami, and it was interesting that it was dated to around 3000BC.  

In my estimation it seemed possible that this tsunami may have occurred as a result of a cliff collapse on the west wall of the Norwegian channel,  the deep and wide trench that runs along the Norwegian Coast, and out to the Atlantic Ocean at the North. 

In my mind this established interesting evidence for turbulence in the north sea that might have lead to an erosive episode breaking through between Orkney and Scotland. 

-×-

Up to this point I cannot say that I had actually proved anything, and even now proof is probably somewhere out of reach.

If there has been material, sand, clay, and silt, in the floor of the North Sea that has, on a millennium scale, been washed away by rising sea levels, it seemed to me to be necessary to establish where that material came from, how it arrived where it was, and how it was removed.

This was the call that demanded that I look at geological sources. These I found in online searches, articles from sources like the British Geological Survey, and the Journal of Quaternary Science. Reports about field work that has been conducted for various reasons, including oil exploration and testing for placement for wind turbine platforms. There is also research with the intention to attempt to predict the effects of climate change on global sea levels.

I'm afraid that as I began to read through these articles, looking at the pictures, the plans, the sections, and the lines on maps I grew more and more dubious about the reliability of what I was studying.

Physically, the science that I was being asked to believe did not make sense. Not to me anyway.

I was on very dodgy ground. I was saying that a huge scientific subject, some of which I had learned as a child, was wrong. The lives, education, and careers of hundreds,even thousands of people were based on a false theory. 

I wasn't backing down though. 

The existing theories could not be justified without ignoring some pertinent observations. Obviously these people were honourable in their work, but often I would read their reports to discover what they believed, and why they believed it.

This usually meant that they make a statement with a reference to another author, someone who had asserted an observation which justified their own theory. This reference though was often dubious, stated as a possibility rather than a fact, or did not actually mean precisely what the authority asserted.

The worst information available was the lines on maps. These are often a result of computer modelling,  and if the information fed into the program that produced the model was inaccurate the result would be meaningless. 

-×-

Given the lack of coherence I found in the story of prehistoric ice ages I started looking at my own experience in the landscape of Britain. 

As an archaeologist I had frequently been up close and personal with the geology of Britain, its what you arrive at when you run out of human influenced soils.

One place where the geology of Britain was particularly present was at Longtown Castle which is at the Welsh border of Herefordshire. There the castle that I worked on sits upon a ridge that carries a prehistoric track from Abergavenny to Hay on Wye. On both sides of the ridge with the track on it are long valleys. The valley on the west side is the Olchon River valley, and on the west side of that is the massive Black Mountain on which the actual border between Wales and England lies.

At the time that I was working at Longtown I would gaze at this valley and wonder at its formation, understanding that it would probably be regarded as a glacial valley. 

Knowing that it was thought to have been created by glaciers I had to recognise in myself serious skepticism about the theory.

I couldn't see where any ice that formed in this valley was coming from, why it was moving, how it was cutting the valley, and why it was flowing at all in that precise location. 

I wasn't a deep thinker. That was 1978, long ago, and far away, I just filed this particular nugget into a box in my brain along with a lot of other nuggets of useless information. 

When I started developing an alternative narrative to describe how the British ice age worked, I came here first to test the theories that I was working on.

Another place though, that triggered the whole process was on top the Cotswold hills where I excavated a pit that had clearly been formed by water falling on a surface,gouging out a hole and smoothing the sides of the pit. To me this had to be glacial meltwater runoff, and the fill of the pit, a pale yellow homogeneous silt must have weathered out of the glacier that had melted to erode the pit.

The germ of an idea began to form that the Olchon Valley at Longtown might have been cut by the fall of melting ice, solid blocks of ice, as it was undercut by meltwater puddling at its edge.

This melting water event, and falling ice, may not have been continuous, but may have happened more quickly in summer, and more slowing in winter.

If an edge were formed along which the ice collapsed it might cause a valley to be cut in the underlying geology. The valley might be cut more deeply in summer when the ice was melting more quickly, and less deeply in winter. 

Where the ice was melting along a receding front this would theoretically create a series of parallel valleys, a new valley cut every year. 

Once I had conjured up the idea of parallel valleys I set out in search of them, and found them all over northern Europe and Southern Europe. Where there were mountains the foothills had valleys that ran along the contours , rather than down the slope.

There were islands where valleys crossed from side to side. By traditional means the glaciers in the valleys would have to be pushed uphill, and then slide downhill for this to be possible,  and I'm deeply skeptical of any theory that makes this suggestion. 

Conversely there are ribbon lakes where linear valleys are blocked at both ends. 

I have been told that the thickness of the ice sheet over Scotland was up to 1500 metres  or one and a half kilometres.  Whether this is true or not I do not yet know, and perhaps I never will. It is enough to say that impacts of small areas of thick ice falling from hundreds of metre heights will have been enormous on solid geology above sea level. The power lost in this collapse could have equated commonly with the most powerful atomic bombs we have ever detonated.

We commonly see videos of ice edge collapse into sea water, at the ends of rivers of ice but the impact of these falls will have been muted by it landing in water.

The impacts that I am describing here would have been largely onto dry land.

-×-

Having discovered that not only were there parallel valleys either side of the Longtown Castle ridge, I looked on topographic maps of the area and found that these ridges and valleys continued into Herefordshire quite some way. Half a dozen parallel valleys  running north to south parallel to the Welsh border on the Black Mountain. 

Now I was hooked on the hunt for valleys that were parallel to each other and that sometimes followed contours on rising ground.

I found them almost everywhere across northern England, Scotland, Wales,  northern Ireland, southern Europe, and Scandinavia. 

I didn't find them anywhere else on the planet, simply because I wasn't looking .

It is highly possible that these valleys are unique to this area  the European Coast of the Atlantic Ocean. As far as I understand it this, the Atlantic Ocean, is the only deep water crack in the earth's surface that joins the oceans that circle the southern hemisphere with the North Pole. Warm water will have ( I believe), always found a way to embrace this coastline,as it does now, with cyclonic storms roaming up from equatorial seas.

The other place that I found parallel valleys was in the North Sea and the English Channel. 

By reading reports about the geology of the North Sea and Britain I began to piece together a story of Britain in the last ice age. The story was a bit furry round the edges as the timeline disappeared into the distant past, and I began to wonder how this was helping me on my original quest, about land bridges between the islands of Britain. I was now sucked into it though. Everything that I was uncovering was in complete opposition to everything I learned at school, and everything that masters, professors and students imbibe today in educational institutions .

Gradually though,  I began to draw a map in my mind of the ice sheet that covered Britain before, and then during the last ice age.

-×-

Until about 70,000 years ago the thickest snow was on the mountains of England, Scotland, Wales, and Northern Ireland. It is not clear how much snow was landed on the remainder of Britain,  but the thickness of the ice sheets on the mountains would have been significant, several hundreds of metres. These ice sheets would, except in exceptional circumstances have been static. The ice sheets on the mountains did not move, and there is no evidence that they did.

At 70,000 years ago there was a sharp thaw at which the edges of the mountain ice sheets collapsed sending mud and rocks in all directions around the mountain tops. From Scotland and Northern England tidal waves of sludge caused by this melt and collapse, were propelled across the dry North Sea to dump the raised ground of Dogger Bank in the southern North Sea. 

Thereafter the remaining ice sheets on the mountains continued to add height while the lowlands of southern and Eastern England were cold with snowy winters, but probably summers that thawed the snow making year on year build up of snow discontinuous.

Between 30,000 years and 20,000 years ago colder climate controlled the laying of snow. Up to this time the ice sheet over Shetland collapsed breaking up a much larger area of land than is present as the Shetland Isles today.  

At this same time a ridge of land joined Dogger bank in the southern North Sea to a promontory between Shetland and Norway facing the north Atlantic Ocean. 

Dogger Bank was connected to Britain and Europe at this time,  but would be separated  from them both as deglaciation proceeded.

Between the ridge running north from Dogger Bank and the east coast of Scotland a shallow lagoon remained unfrozen during the last cold snap of the glaciation. 

Around this lagoon, and in an area north of it near Orkney there is likely to have been a woodland environment.

The last period of cold weather, that ended at around 21,000 years ago, saw more snow landing and compacting on British mountains,  thin or absent snow in the south west, and thicker deposits on eastern and southeastern England. The high ground in the north sea area, from Dogger Bank up to the Atlantic Ocean also saw thick ice sheets. 

From about 21,000 years ago these ice sheets started to collapse creating parallel valleys in the north sea, and offshore from England and Scotland. The English Channel was also cut at this time partially severing Britain from Europe.

By about 16,000 years ago the ice sheets were restricted to the mountains of England and Scotland.  At about this time the amounts of water running from melting ice sheets was raising sea levels locally around British and Norwegian Coasts. 

The final flush of raised sea levels occurred around 11,000 years ago.

Throughout these times the collapse of the ice sheets, and the cutting of the valleys  with the huge volumes of meltwater, sent ice streams loaded with rocks, sediment, and ice downhill towards coastal waters. Where these ice streams were intercepted by the water's edge, linear moraines were laid. As these mobile ice streams passed over exposed rocks the sludge and rocks they carried scarred the surface of the stones (striations).

In Scotland, where the ice sheets collapsed, in some places the resulting rock, ice, and sediment stream became stuck in the valleys that had been cut. 

Meltwater then drained off from the collapse,  leaving the "glacier", a river of ice, cool in the valley floor.

Gradually,  from about 9000 years ago these rivers of ice melted in place,  dropping their contents on the valley floor. This was an uneven deposition of material which remains as hummocky moraine. 

-×-

After deglaciation,  habitats like woodland and marshes, extended out from northern Europe to much of the British Isles and North Sea. 

As sea levels rose Doggerland was lost, but a thin strand of woodland at the southern coast of the North Sea remained,  linking Holland to Lincolnshire and Norfolk. 

Mammals, reptiles, plants and trees migrated along this corridor of land in the early post-glacial period, followed by people with sheep and dogs.

The corridor of land was gradually eroded away as water depths either side of it increased, allowing greater wave energy to develop in the North Sea, and stronger tides to filter along the English Channel. 

Cores have been drilled into the seabed at locations near the Norfolk coast to analyse the nature of geological deposits there. The findings indicate, in general terms that there are buried peats there which were drowned at a depth of around 20 metres in about 8000 years ago. No peat are present at shallower depths, or later dates, leading to the suggestion that sea level reached 20 metres below our sea level at 8000 years ago.

At that date marine agitation was sufficient to flood the existing peats, and to crop off any later peats at shallower depths.

In a few other places large thicknesses of sediments are added to the seabed, at a date in the 4th millennium BC, suggesting that sediments have been eroded from elsewhere to be dumped in a large scale submarine event.

There is probably evidence to provide a reasonable assessment that the English Channel was gradually eroded away from about 8000 years ago, and was finally broken through in the 4th millennium BC,  at a time when early neolithic people were still extending their ranges into Britain,  and out of Europe. 

Following the breakthrough of the English Channel from the Atlantic Ocean to the North Sea,  the latter became fully tidal, with complex tidal flows around all of its shorelines, including the Pentland Firth between Orkney and Scotland. 

-×-

When I began to research the Archaeology and geology of the British Isles,  to comprehend where land was, until early neolithic dates, I knew it would be a challenge.  Looking for something that isn't there any more but once was there, is obviously fraught with problems. The evidence that I had to be contend with would be shadows and footprints, scars and halos.

Also obviously, the discovery of a single footprint does not make a human civilisation. I had to find a fabric of shadows to feel for the landscape that time had eliminated.

I believe that I have provided the fabric. I hope you agree, but even if you don't I will continue to explore, looking for a solution to the Riddle. 

Jeffery Nicholls 

South Ronaldsay 

Orkney 

The Orkney Riddle (indec here) is a series of blogs promoting the notion that Neolithic people walked from Scotland to Orkney to build the Ring of Brodgar. 

Email jiffynorm@yahoo.co.uk 

#Orkney #archaeology #Neolithic #prehistory #British #SkaraBrae #NessofBrodgar #BIIS ##Britice-Chrono 

 

Monday, June 1, 2026

Stones of Brodgar

 The Stones of Brodgar 


When I went to the Ring of Brodgar today I took a photo of each stone from outside the ditch.

I have a theory that the Stones of Brodgar were set in their places with a sloping edge facing in the same relative direction in rotation around the circle.

They obviously don't all have an obvious slope on one side.

Also at least one of the stones fell over in historic or prehistoric times, and may have been re-erected by Historic Scotland staff. Could they have put them up wrongly?

























I don't know if my theory works.

What do you think?




Jeffery Nicholls 



Orkney Riddle Index

  Orkney Riddle  Index This is the southern tip of South Ronaldsay,  close to the Tomb of the Eagles.  The island offshore is called the Pen...