Monday, 5 August 2013

Poster advertising exhibition of a human fossil

Poster advertising exhibition of a human fossil
BGS image ID: P849851
This poster was found in the back of a scrapbook that belonged to Roderick Murchison (1792-1871) who was Director of the Geological Survey of Great Britain, 1855-1871. The Cuvier referred to is Jean Léopold Nicolas Frédéric Cuvier (1769-1832), generally known as Georges Cuvier. He was a comparative anatomist, zoologist, geologist and vertebrate palaeontologist and a proponent of catastrophism.

Andrew L Morrison

Saturday, 3 August 2013

Cinder cones on Etna, 1892.

Cinder cones on Etna. This is one of a series of photographs taken July to September 1892 that gave rise to the Monti Silvestri crater row.   Presented by Professor G. Platania of Aci Reale, Sicily. Photograph held in the BGS Archives, Keyworth. Archive reference GSM/GX/Pa/1.
BGS Image ID: P711323
This is one of a series of photographs taken July to September 1892 that gave rise to the Monti Silvestri crater row. 

Presented by Professor G. Platania of Aci Reale, Sicily. Photograph held in the BGS Archives, Keyworth. Archive reference GSM/GX/Pa/1.

Friday, 2 August 2013

Some Account of the Strata and Volcanic Appearances... 1790.

Fig. 1. View of the Glen near Ardlun Head in Mull. Fig. 2. View of the insulated Rock at the termination of the Glen. Fig. 3. A view of the great Fissure, the Cave and the suspended Stones, in the Island of Mull. The fissure ranges N. and S., is about ten feet wide and forty yards deep: the sides and the suspended stones are granite.  From: Some account of the Strata and Volcanic Appearances in the North of Ireland and Western Isles of Scotland. In two letters from Abraham Mills Esq. to John Lloyd, Esq. F.R.S. Read January 21, 1790. Published in Phil. Trans. Vol LXXX.

Fig. 1. View of the Glen near Ardlun Head in Mull.
Fig. 2. View of the insulated Rock at the termination of the Glen.
Fig. 3. A view of the great Fissure, the Cave and the suspended Stones, in the Island of Mull. The fissure ranges N. and S., is about ten feet wide and forty yards deep: the sides and the suspended stones are granite.

From: Some account of the Strata and Volcanic Appearances in the North of Ireland and Western Isles of Scotland. In two letters from Abraham Mills Esq. to John Lloyd, Esq. F.R.S. Read January 21, 1790. Published in Phil. Trans. Vol LXXX. 

Tuesday, 30 July 2013

James Croll

BGS image ID: P742383
James Croll was born in 1821, the son of a Perthshire stonemason and crofter. He was to suffer from ill health throughout his life. In 1864, while working as janitor, he published the paper The physical cause of the change of climate during geological epochs. This proposed the theory that variations in the earth’s orbit were responsible for cyclical climate changes, including ice ages. In 1867 he was offered the position of office-keeper at the Scottish branch of the Geological Survey. This job left him sufficient freedom to pursue his climate studies and resulted in the publication of the book Climate and Time (1875).

In 2010 the Quaternary Research Association established the James Croll Medal, its highest award for merit.
Andrew L Morrison

Friday, 12 July 2013

Letter about C B Wedd being a German spy

Letter about C B Wedd being a German spy
BGS image ID: P842013
This letter is from W H Spaull who was a magistrate at Oswestry. He is enquiring about geologist Charles Bertie Wedd (1868-1945) who was allegedly up a tree sketching near an army camp and mistaken for a German spy and almost lynched! This letter as well as showing some of the dangers a field geologist may face also demonstrates the fear of German spies less than two months after the outbreak of World War 1.

Posters about the Geological Survey and World War I

Andrew L Morrison   

Monday, 1 July 2013

Parish's Loam Work, Erith.

Parish's Loam Work, Erith. Looking S. This is (really) the southern portion of the great pit, entered along the southern tramline. View looking south and shows mode of working. A small adit is made at foot of the face. The overlying sand is shovelled down, with the truck placed at mouth of adit. This causes the curious aspect of the face. The sand does not show bedding unless seen very closely. This exposes the whole thickness of the Thanet Sand, about 70 feet, with an ill-defined capping of the pebbly series.
BGS image ID: P201180
Parish's Loam Work, Erith. This is the southern portion of the great pit, entered along the southern tramline. View looking south and shows mode of working. A small adit is made at foot of the face. The overlying sand is shovelled down, with the truck placed at mouth of adit. This causes the curious aspect of the face. The sand does not show bedding unless seen very closely. This exposes the whole thickness of the Thanet Sand, about 70 feet, with an ill-defined capping of the pebbly series.

Date taken: 27/06/1911

Old photograph number: A01191

Bob McIntosh

Sunday, 30 June 2013

Oblique aerial view of Blindwells Opencast Site, Tranent, 1996.

Oblique aerial view of Blindwells Opencast Site, Tranent, looking from the east-north-east. Working opencast coal site, in coals of the Limestone Coal Formation, showing various stages in the process. The working face is in the foreground; backfilled spoil in the centre - colours of each load derive from different materials, white and pale brown = sandstone, pale and dark grey = siltstone and shale, dark brown = glacial till overburden; black area = coal storage, pale brown areas = restored overburden. Top left is worked area fully restored to agricultural use. Bottom right is undisturbed ground.
BGS image ID: P001315
Oblique aerial view of Blindwells Opencast Site, Tranent, East Lothian, looking from the east-north-east. Working opencast coal site, in coals of the Limestone Coal Formation, showing various stages in the process. The working face is in the foreground; backfilled spoil in the centre - colours of each load derive from different materials, white and pale brown = sandstone, pale and dark grey = siltstone and shale, dark brown = glacial till overburden; black area = coal storage, pale brown areas = restored overburden. Top left is worked area fully restored to agricultural use. Bottom right is undisturbed ground.


Bob McIntosh

Saturday, 29 June 2013

Joseph Beete Jukes M.A., F.R.S.

 Joseph Beete Jukes 1811-1869. Born at Summerhill, near Birmingham. Studied under Sedgwick. Worked in Newfoundland and on H.M. Ship 'Fly' surveying the coast of Australia and New Guinea. Joined the Geological Survey of Great Britain and Ireland in 1846 and by 1850 was appointed to the post of Director of Geological Survey Ireland.
BGS image ID:  P505852

Joseph Beete Jukes 1811-1869. Born at Summerhill, near Birmingham. Studied under Sedgwick. Worked in Newfoundland and on H.M. Ship 'Fly' surveying the coast of Australia and New Guinea. Joined the Geological Survey of Great Britain and Ireland in 1846 and by 1850 was appointed to the post of Director of Geological Survey Ireland.

More details can be found in Joseph Beete Jukes page in the new biographical resource: Pioneers of the British Geological Survey. Browse the 'Pioneers'


 Joseph Beete Jukes 1811-1869. Born at Summerhill, near Birmingham. Studied under Sedgwick. Worked in Newfoundland and on H.M. Ship 'Fly' surveying the coast of Australia and New Guinea. Joined the Geological Survey of Great Britain and Ireland in 1846 and by 1850 was appointed to the post of Director of Geological Survey Ireland.
BGS image ID:  P575755
Bob McIntosh

Friday, 28 June 2013

Scottish oil shale distillates, 1905 vintage.

Samples of the different distillates and products that are produced during the processing of Scottish oil-shale. Samples on the left contain distillates that are intermediary stages in the process such as the crude oil, crude distillate (green oil), blue oil. Samples on the right are the final products that are marketed for a range of uses e.g. motor spirit, lighthouse oil, cleaning spirit.
BGS image ID: P528115
Samples of the different distillates and products that are produced during the processing of Scottish oil-shale. Samples on the left contain distillates that are intermediary stages in the process such as the crude oil, crude distillate (green oil), blue oil. Samples on the right are the final products that are marketed for a range of uses e.g. motor spirit, lighthouse oil, cleaning spirit.

Top row, left to right: Crude Shale Oil, Crude Distillate, Blue Oil, Heavy Oil and Paraffin, Crude Naptha, Crude Burning Oil. 
Bottom row, left to right: Crude Scrubber Naptha, Sulphate of Ammonia, Ammoniacal Liquor, Motor Spirit, Lighthouse Oil, Power Oil, Cleaning Spirit.


Diagram illustrating processes of manufacture in the Scottish oil-shale industry. The diagram shows the complete process from the original shale through the various treatments and distillations and showing the end products. The process can be conveniently considered in two stages. The raw oil-shale is distilled/heated in retorts in the absence of air and in the presence of steam. This allows the shale to undergo decomposition and distillation into crude oil and ammonia. The second stage is refining the crude oil. The object is to obtain from the crude oil various types of refined oil and wax as required by the prevailing markets at the lowest possible working cost and with the smallest amount of capital spent on refining plant.
BGS image ID: P528117
Diagram illustrating processes of manufacture in the Scottish oil-shale industry.

The diagram shows the complete process from the original shale through the various treatments and distillations and showing the end products. The process can be conveniently considered in two stages. The raw oil-shale is distilled/heated in retorts in the absence of air and in the presence of steam. This allows the shale to undergo decomposition and distillation into crude oil and ammonia. The second stage is refining the crude oil. The object is to obtain from the crude oil various types of refined oil and wax as required by the prevailing markets at the lowest possible working cost and with the smallest amount of capital spent on refining plant.

Other samples from the Scottish Shale oil industry

Bob McIntosh

Thursday, 27 June 2013

Westfield Opencast Coal Mine, 1977.

Oblique aerial view of the Westfield Opencast Coal Mine from the north-east Fife Region. Cut to extract the abnormally thick development of coals (Boglochty Beds) in the Passage Group of the Namurian of the Scottish Carboniferous succession. The excavation is about 200 metres deep and has cut through strata from just above the top of the Middle Coal Measures (Westphalian B) down to the Calmy Limestone of Namurian (E2) age. At the top are the processing plants. The Westfield Open Pit was worked by Costain Mining Limited on behalf of the National Coal Board Opencast Executive.
BGS image ID: P001513
Oblique aerial view of the Westfield Opencast Coal Mine from the north-east Fife Region. Cut to extract the abnormally thick development of coals (Boglochty Beds) in the Passage Group of the Namurian of the Scottish Carboniferous succession. The excavation is about 200 metres deep and has cut through strata from just above the top of the Middle Coal Measures (Westphalian B) down to the Calmy Limestone of Namurian (E2) age. At the top are the processing plants. The Westfield Open Pit was worked by Costain Mining Limited on behalf of the National Coal Board Opencast Executive.

Excavation commenced in 1955 on the site of the former Kirkness Colliery, production started the following year, 1956. It was regarded at the time as the largest opencast in the UK and possibly Europe.


Old photograph number: D02514

Photograph taken 1977.

Bob McIntosh