Card design by A.G'ruffalo.
Excursions [and other notes] involved in the exploration of Hallowe'en Rift; a cave, so far, formed within Triassic Dolomitic Conglomerate.
The exploration of Hallowe'en Rift was started in 1982 by Trevor Hughes with other members of the Bristol Exploration Club, then during the early 1990's Vince Simmonds and other, mostly, local diggers were active at a number of locations within the cave, including the start of the present dig with Graham Johnson in December 1991. The current phase of exploration was commenced in 2009, with the majority of the early work being carried out by Vince Simmonds and Alex Gee, now the regular team includes Rob 'Tav' Taviner, Graham 'Jake' Johnson, Nick Hawkes, Matt Tuck, Jonathon Riley, Paul 'Brockers' Brock and Roz Simmonds. There has also been assistance from John 'Tangent' Williams, Pete Bolt, Duncan Price, Bob Smith, Mike Moxon, Callum and Hazel Simmonds, with a couple of guest appearances by that well-known antipodean, Ray Deasy.
24th July 2016:
Sunday morning and the dog needed a walk so decided that I would go over to Hallowe'en Rift and get the lump of flowstone that I had left there. Parked at the end of Dursdon Drove and walked along the hilltop at Rookham before crossing fields down to Hallowe'en Rift. At the cave I took some photographs, put the lump of flowstone into my bag before spending a few minutes placing some more stones onto the retaining wall.
As previously mentioned (23/07/2016 entry) after splitting a lump of flowstone yesterday another older speleothem was revealed encased within it, as is clearly seen in the image below.
The other lump of flowstone also reveals an older speleothem. Just to the right of centre the remains of a small stalagmite 'boss' can be seen below successive layers of flowstone.
Both these remnants of flowstone have been recovered from the sediments removed from the ongoing dig at the end of Merlin's Magic Milk Parlour. It would be interesting to get these dated to establish whether the ages are similar to the dates from previous samples.
Here is a video clip about digging to amuse you, it made me smile anyway. WARNING: this video contains an earworm!
It's not a theme song for the team working at Hallowe'en Rift as Jake and Alex are both far too tall.
An evening stroll up to Hallowe'en Rift with Don McFarlane and Joyce Lundberg who are interested in carrying out some more stal dating on material from the cave. They weren't dressed for an underground trip and seemed content to pick over the spoil heap for suitable material. I did venture down the shaft if only to get a hammer to break up some larger lumps of stal.
Don is Professor of Environmental Science at Claremont Colleges in California, USA; Joyce is Associate Professor at Carleton University, Ottawa, Canada.
Once upon a time at the
foot of a great mountain
There was a town where the people known as Wookeyfolk lived,
Their very existence a mystery to the rest of the world,
Obscured as it was by great clouds.
Here, they played out their peaceful lives,
Innocent of the litany of excess and violence
That was growing in the world below,
To live in harmony with the spirit of the mountain called Mendip was enough.
Then, one day, Strangefolk arrived in the town;
They came in ragged caving clothes, hidden under hats,
But, no one noticed them, they only saw shadows.
You see, without the Truth of the eyes, the Wookeyfolk were blind.
In time, the Strangefolk found their way into the high reaches of the mountain
And it was there that they found caves of unimaginable sincerity and beauty.
By chance, they stumbled upon the place where all the good souls come to rest.
The Strangefolk, they coveted the jewels in these caves above all things
And soon they began to dig into the mountain,
Its rich seam fuelling the chaos of their own world.
Meanwhile, down in the town, the Wookeyfolk slept restlessly
Their dreams invaded by the shadowy figures digging away in the holes.
Every day, people would wake and stare at the mountain,
Why was it bringing curiosity into their lives?
And, as the Strangefolk dug deeper and deeper into the mountain
Following a cold and cheering draught that touched their very souls,
For the first time
The Wookeyfolk felt cheerful.
For they knew that soon that the mountain called Mendip would reveal its hidden secret.
And then came a sound, distant at first
It grew into a cacophony
So immense it could be heard far away in space
There were no screams, there was no time,
The mountain called Mendip had spoken; there was only wide open space,
And then, joy!
Adapted from ‘Fire coming out of the Monkey’s Head’ on Demon Days by Gorillaz, written by Damon Albarn and Jamie Hewlett. Released May 2005
3000-Year-Old Remains of Baby Found at Halloween's Birthplace
Jun 10, 2014 01:36 PM ET // by Rossella Lorenzi
Remains of a baby dating back to 3,000 years ago have been found at a site in Ireland that is believed to be the birthplace of Halloween.
The fully intact skeleton, possibly belonging to a 7-10 month child, was unearthed during a three week excavation at Tlachtga, on the Hill of Ward near Athboy Co. Meath.
One of Ireland’s most enigmatic sites, the Hill of Tlachtga features impressive circular earthworks which are best seen from the air. Medieval texts link the site to Samhain, the ancient Celtic Festival which is the precursor to modern Halloween.
“We may never know what caused the death of the child. The skeleton probably dates back 3,000 years and was found on the bedrock at the base of a 1.5m (3-foot, 28-inch) ditch,” lead archaeologist Stephen Davis, at University College Dublin, told the Irish Examiner.
Excavation and surveys carried out using airborne laser revealed the area was a “key ritual site.”
“The site has several different phases of monumental enclosures and we believe them to be associated with festivals and rituals potentially dating back as far as 1,000 B.C.,” Davis said.
Sitting on top of the Hill of Ward, Tlachtga is a site steeped in folklore. According to Irish mythology, it got its name from the daughter of the powerful druid Mug Ruith. According to legend, the remains of the druidess, who is said to have died on the hill after giving birth to triplets, are buried there.
Tlachtga is also believed to be the site of the Great Fire Festival in which sacrifices were offered to gods on Samhain eve. All hearth fires throughout Ireland were extinguished and then lit again from a central fire on the hill.
Meaning summer’s end, Samhain was a great festival of the dead — a time when the doorways to the otherworld opened and journeys could be made from one side to the other.
The veil between the worlds of the living and the dead was believed to be the thinnest on Oct. 31, a day which lies exactly between the autumnal equinox and the winter solstice.
The excavation revealed the monument of Tlachtga is actually the last of at least three phases of enclosure on the hill.
“As a working model for the phases of construction, at least one small enclosure, about 15 inches in diameter, was enclosed by a very large, tri- or quadrivallate enclosure, about 650 feet in diameter, which was replaced by the monument we see today,” the archaeologists said.
The excavations also brought to light evidence of burning, which could have been ritual fires or the result of glass-making, Davis said.
He believes the child was most likely not the victim of any human sacrifice on the ritual site.
The remains have been taken to the School of Archaeology at
University College Dublin for further examination.
Unfortunately it's been very quiet on the cave digging front over the last few weeks due to other weekend happenings [on my part, anyway], such as archaeological conferences and the continuing Stanton Drew Survey Project, this involves geophysical and other archaeological investigations of the environs surrounding the stone circle complex, this has taken up two long weekends.
We will get back to the task ahead in Hallowe'en Rift soon!
This bone was found in the sediment in October 2011 along the left side of the tube ('Toil and Trouble') leading from the base of Witches Cauldron. Despite very careful scutiny of sediments no other bones have, since been uncovered.
A visit to the Wells and Mendip Museum to look at the collections displayed in the Balch Room led to a positive indentification of the bone as being from the foreleg of Bison priscus, the museum specimen is dated from the Pleistocene and was found at Milton Hill.
Higham, T. 2006. AMS 14C Dating of Ancient Bone Using Ultrafiltration gives dates for Bison priscus recovered from Banwell Bone Cave as 52,700 +/- 1900 14C age BP to >59,500 14C age BP and for Hunter's Lodge Sink as >54,800 14C age BP.
1st April 2012. A busmans holiday to look at someone elses digsites. Willie Stanton originally dug at these sites but permission has recently been given to Stu Lindsay, Trever Hughes, et. al. (BEC) to continue the excavation.
Interesting closed basin development seems in places to follow washed out mineral vein. Colourful rocks comprising greys, red, white, yellow, orange (see below) and calcite with gravel and clay infill.
Spent a while in conversation with Stu Lindsay who suggested that there is some historical confusion about which site is which. Barrington and Stanton (1977) descriptions are as follows:
"Brimble Pit Swallet ST 5081 5075 alternative names Westbury Hill Swallet, Frog Hole.
50 yards east of Priddy-Westbury road at Brimble Pit Pool, in a depression by a wall taking the overflow from a small covered reservoir in the next field. Tight vertical rift dug by MNRC 1957-58, blocked by a boulder 50 feet down. Entrance collapsed about 1960. MNRC flood-tested the stream to Rodney Stoke rising in 1956. The Brimble Pit closed basin and overflow channel, and those of Cross Swallet nearby are scheduled as an SSSI; taken together they show all the geomorphic features of Mendip closed basins.
Locke's Hole ST 5088 5072 alternative name Westbury Hill Swallet.
100 yards east of Priddy-Westbury road at Brimble Pit Pool, in a depression taking the natural overflow of the pool. Entrance shaft dug open by MNRC, 1955-56, entered sloping passage ending in sand-choked chamber. Digging stoppedwhen entrance shaft collapsed. A cow is said to have died in the entrance shaft about 1964, when the farmer half-filled the depression with rubble."
Reference: Barrington, N. and Stanton, W. 1977 (third revised edition). Mendip: The Complete Caves and a view of the hills. Barton Productions in conjunction with Cheddar Valley Press.
Boulder of Dolomitic Conglomerate removed from Hallowe'en Rift, the purple-red colour is the result of high iron content and evidence of haematitization (see below).
On the Mendip Hills, the Dolomitic Conglomerate mostly comprises clasts of Carboniferous limestone cemented into a matrix of sandy marl or fine grained limestone debris, locally derived material from the Old Red Sandstone and Quartzitic Sandstone Group is also present. The rock clasts are angular to rounded and range in size from varying sized gravels to very large boulders. The Dolomitic Conglomerate forms bold crags, it might be eroded into gorges, and it can support underground drainage systems including caves and swallets and is the locus for extensive lead/zinc mineralization. The formation represents Triassic scree and outwash fans adjacent the ancient hills of Paleozoic rocks, and it fills 'fossil' wadis or gorges that had been cut into the hills. Recent erosion has partially re-excavated some of these gorges, as at Burrington Combe.
Exposure of surface weathered Dolomitic Conglomerate [slightly silicified] in Harptree Combe.
The conglomerate found on the Mendip Hills has, in many cases undergone considerable secondary changes, in particular silicification, haematitization and dolomitization. Haematitization is the conversion of the conglomerate into an 'earthy' iron ore known as 'red ochre'. The presence of all gradations from unaltered conglomerate to impure haematite rock show that the formation of the latter is the result of metasomatic replacement of calcium carbonate by haematite.
The most widespread form of alteration is dolomitization, hence the name 'Dolomitic Conglomerate'. All stages of dolomitization are present, both matrix and clasts showing varying degrees of alteration. Dolomitization is usually accompanied by hydration or partial hydration of the originally disseminated haematite to limonite so that macroscopically the colour has changed from red to yellow and yellow-brown. Dolomitization affects more than one level in the Dolomitic Conglomerate though it is most marked in the upper parts of the succession.
metasomatism is a metamorphic process [where rocks are changed by heat, pressure and fluids] in which the chemical composition of the rock is changed significantly, usually as a result of fluid flow.
Green, G.W. et. al. 1965. Geology of the country around Wells and Cheddar. HMSO, London.
Keary, P. 2001. The New Penguin Dictionary of Geology, 2nd Edition. Penguin.