View allAll Photos Tagged bituminous
University of Southampton Faculty of Engineering, Science and Mathematics,
School of Civil Engineering and the Environment, "Bituplaning: A Low Dry Friction Phenomenon of New Bituminous Road Surfaces" By John Charles Bullas BSc MSc MIAT MIHT FGS May 2007 Thesis for the Degree of Doctor of Philosophy
University of Southampton Faculty of Engineering, Science and Mathematics,
School of Civil Engineering and the Environment, "Bituplaning: A Low Dry Friction Phenomenon of New Bituminous Road Surfaces" By John Charles Bullas BSc MSc MIAT MIHT FGS May 2007 Thesis for the Degree of Doctor of Philosophy
University of Southampton Faculty of Engineering, Science and Mathematics,
School of Civil Engineering and the Environment, "Bituplaning: A Low Dry Friction Phenomenon of New Bituminous Road Surfaces" By John Charles Bullas BSc MSc MIAT MIHT FGS May 2007 Thesis for the Degree of Doctor of Philosophy
Semi-anthracite coal from the Mississippian of Virginia, USA.
This sample is from the best outcrop anywhere of the only economically significant Mississippian-aged coal occurrence in the world. The beds are structurally tilted - this occurred during the Allegheny Orogeny in the Pennsylvanian.
The coal shown above is from the Langhorne Coal. At this site, the unit is tectonically-thickened and sheared. The rank is semi-anthracite coal, which results from very low grade metamorphism of bituminous coal. Adjacent beds (shales and sandstones) are not metamorphosed. The Langhorne Coal has been mined in the past.
Stratigraphy: lowermost upper member, Price Formation, Osagean Stage, upper Lower Mississippian
Locality: roadcut on the eastern side of Rt. 100, western end of Cloyds Mountain, south of the town of Poplar Hill, Pulaski County, Valley Coalfield, southwestern Virginia, USA (= locality shown in figure 9 of Bartholomew & Brown, 1992) (37° 10' 42.39" North latitude, 80° 42' 48.48" West longitude)
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Some info. from:
Bartholomew, M.J. & K.E. Brown. 1992. The Valley Coalfield (Mississippian age) in Montgomery and Pulaski Counties, Virginia. Virginia Division of Mineral Resources Publication 124. 33 pp. 2 pls.
Gensel, P.G. & K.B. Pigg. 2010. An arborescent lycopsid from the Lower Carboniferous Price Formation, southwestern Virginia, USA and the problem of species delimitation. International Journal of Coal Geology 83: 132-145.
University of Southampton Faculty of Engineering, Science and Mathematics,
School of Civil Engineering and the Environment, "Bituplaning: A Low Dry Friction Phenomenon of New Bituminous Road Surfaces" By John Charles Bullas BSc MSc MIAT MIHT FGS May 2007 Thesis for the Degree of Doctor of Philosophy
University of Southampton Faculty of Engineering, Science and Mathematics,
School of Civil Engineering and the Environment, "Bituplaning: A Low Dry Friction Phenomenon of New Bituminous Road Surfaces" By John Charles Bullas BSc MSc MIAT MIHT FGS May 2007 Thesis for the Degree of Doctor of Philosophy
Cannel coal from the Pennsylvanian of England. (~5.1 centimeters across at its widest along the base)
Cannel is an odd variety of coal. It doesn’t have the look and feel of ordinary coal ranks such as lignite, bituminous, and anthracite. Cannel coals are low-density (lightweight for their size), as all coals are, but are surprisingly tight and solid - they hold up to natural weathering pretty well, considering they’re coals. They tend to have a satiny or velvety luster, are not sooty to the touch, and frequently have conchoidal fracture (smooth & curved fracture surfaces). Cannel coals lack the well-developed horizontal bedding & laminations seen in lignites and bituminous coals.
Not surprisingly, the differences in physical characterstics between cannel coal and other ranks of coal are due to the organic matter content. Cannel coals are composed principally of fossil spores (sporinite phytoclasts). Garden-variety coals are composed principally of a mix of altered fragmented plant debris that was originally woody tissue, leaves, fungi, and spores. Cannel coals are generally interpreted as having formed in pond, lagoon, or channel facies within a larger coal swamp setting.
The sample seen here is from the Wigan area of England. Cannel coal has been mined in the area for many centuries.
Stratigraphy: unrecorded / undisclosed Pennsylvanian-aged unit ("Upper Carboniferous")
Location: unrecorded / undisclosed locality at or near the town of Wigan, west of Manchester, England
Semi-anthracite coal in the Mississippian of Virginia, USA.
This is the best outcrop anywhere of the only economically significant Mississippian-aged coal occurrence in the world. The beds are structurally tilted - this occurred during the Allegheny Orogeny in the Pennsylvanian.
The coal bed shown here is the Merrimac Coal. Its rank is semi-anthracite coal, which results from very low grade metamorphism of bituminous coal. Adjacent beds are not metamorphosed. The Merrimac Coal (& the subjacent Langhorne Coal - not visible in this shot) have been mined in the past. Thin interbeds of fossiliferous clayshale are present within the Merrimac Coal.
Stratigraphy: Merrimac Coal, lower part of the upper member, Price Formation, Osagean Stage, upper Lower Mississippian
Locality: roadcut on the eastern side of Rt. 100, western end of Cloyds Mountain, south of the town of Poplar Hill, Pulaski County, Valley Coalfield, southwestern Virginia, USA (= locality shown in figure 9 of Bartholomew & Brown, 1992) (37° 10' 42.39" North latitude, 80° 42' 48.48" West longitude)
----------------------
Some info. from:
Bartholomew, M.J. & K.E. Brown. 1992. The Valley Coalfield (Mississippian age) in Montgomery and Pulaski Counties, Virginia. Virginia Division of Mineral Resources Publication 124. 33 pp. 2 pls.
Gensel, P.G. & K.B. Pigg. 2010. An arborescent lycopsid from the Lower Carboniferous Price Formation, southwestern Virginia, USA and the problem of species delimitation. International Journal of Coal Geology 83: 132-145.
Bituminous coal in the Burgoon Sandstone, lower Osagean, Lower Mississippian. Covington Township, Clearfield County, Pennsylvania, USA. Hammer for scale. Abundant crusts of sulfur and iron sulfate are derived not from the coal, but from thin pyrite horizons overlying it (visible at the base of the hammer handle).
In winter those trees will lose their leaves and the car parking below will be revealed in all its bituminous majesty.
This conveyer belt moves coal from the bituminous coal mines at Black Mesa to the tower next to the highway. From here it's loaded onto a train that brings it to the Navajo Generating Station outside Page, Arizona. Anyone ever read the Monkey Wrench Gang by Edward Abbey? Both the conveyer and the train were sabotaged by Hayduke & Co.
University of Southampton Faculty of Engineering, Science and Mathematics,
School of Civil Engineering and the Environment, "Bituplaning: A Low Dry Friction Phenomenon of New Bituminous Road Surfaces" By John Charles Bullas BSc MSc MIAT MIHT FGS May 2007 Thesis for the Degree of Doctor of Philosophy
Fforio/Explore : Cwm Coke Works
Cwm Coke Works
1958 - 2002
"In the 1970s, the cokeworks employed 1,500 men and produced some 515,000 tonnes of coke each year. It continued to do so until 1986, when coal was privatised."
llantwitfardrecommunitycouncil.org
"Coke is a fuel with few impurities and a high carbon content, usually made from coal. It is the solid carbonaceous material derived from destructive distillation of low-ash, low-sulfur bituminous coal. Coke made from coal are grey, hard, and porous. While coke can be formed naturally, the commonly used form is man-made. The form known as petroleum coke, or pet coke, is derived from oil refinery coker units or other cracking processes."
Wiki
Fforio/Explore : Cwm Coke Works
Cwm Coke Works
1958 - 2002
"In the 1970s, the cokeworks employed 1,500 men and produced some 515,000 tonnes of coke each year. It continued to do so until 1986, when coal was privatised."
llantwitfardrecommunitycouncil.org
"Coke is a fuel with few impurities and a high carbon content, usually made from coal. It is the solid carbonaceous material derived from destructive distillation of low-ash, low-sulfur bituminous coal. Coke made from coal are grey, hard, and porous. While coke can be formed naturally, the commonly used form is man-made. The form known as petroleum coke, or pet coke, is derived from oil refinery coker units or other cracking processes."
Wiki
Fforio/Explore : Cwm Coke Works
Cwm Coke Works
1958 - 2002
"In the 1970s, the cokeworks employed 1,500 men and produced some 515,000 tonnes of coke each year. It continued to do so until 1986, when coal was privatised."
llantwitfardrecommunitycouncil.org
"Coke is a fuel with few impurities and a high carbon content, usually made from coal. It is the solid carbonaceous material derived from destructive distillation of low-ash, low-sulfur bituminous coal. Coke made from coal are grey, hard, and porous. While coke can be formed naturally, the commonly used form is man-made. The form known as petroleum coke, or pet coke, is derived from oil refinery coker units or other cracking processes."
Wiki
Fforio/Explore : Cwm Coke Works
Cwm Coke Works
1958 - 2002
"In the 1970s, the cokeworks employed 1,500 men and produced some 515,000 tonnes of coke each year. It continued to do so until 1986, when coal was privatised."
llantwitfardrecommunitycouncil.org
"Coke is a fuel with few impurities and a high carbon content, usually made from coal. It is the solid carbonaceous material derived from destructive distillation of low-ash, low-sulfur bituminous coal. Coke made from coal are grey, hard, and porous. While coke can be formed naturally, the commonly used form is man-made. The form known as petroleum coke, or pet coke, is derived from oil refinery coker units or other cracking processes."
Wiki
University of Southampton Faculty of Engineering, Science and Mathematics,
School of Civil Engineering and the Environment, "Bituplaning: A Low Dry Friction Phenomenon of New Bituminous Road Surfaces" By John Charles Bullas BSc MSc MIAT MIHT FGS May 2007 Thesis for the Degree of Doctor of Philosophy
The Coal House is a distinctive building built of coal masonry. The bituminous coal was quarried as blocks and dressed as stone using 65 tons of coal from the nearby Winifrede Seam. At the time of its construction it was the only coal building in West Virginia. The house was designed by architect Hassel T. Hicks, who was supervised by David M. Goode. The coal masonry was varnished for weather-resistance. Located adjacent to the Mingo County Courthouse, it houses the Tug Valley Chamber of Commerce.
The building's construction in 1933 was organized as a publicity stunt by O.W. Evans of the Norfolk and Western Railway, who wished to create a symbol of the "Billion Dollar Coalfield" centered on Williamson. While it is known as the "Coal House", it has never been a residence.
It was placed on the National Register of Historic Places in 1980.
Information from: en.wikipedia.org/wiki/Coal_House_(Williamson,_West_Virginia)
Williamson, West Virginia is a small town located on the Tug Fork (directly across from Kentucky) in the southwest of the state. It serves as the seat of Mingo County.
University of Southampton Faculty of Engineering, Science and Mathematics,
School of Civil Engineering and the Environment, "Bituplaning: A Low Dry Friction Phenomenon of New Bituminous Road Surfaces" By John Charles Bullas BSc MSc MIAT MIHT FGS May 2007 Thesis for the Degree of Doctor of Philosophy
University of Southampton Faculty of Engineering, Science and Mathematics,
School of Civil Engineering and the Environment, "Bituplaning: A Low Dry Friction Phenomenon of New Bituminous Road Surfaces" By John Charles Bullas BSc MSc MIAT MIHT FGS May 2007 Thesis for the Degree of Doctor of Philosophy
Fforio/Explore : Cwm Coke Works
Cwm Coke Works
1958 - 2002
"In the 1970s, the cokeworks employed 1,500 men and produced some 515,000 tonnes of coke each year. It continued to do so until 1986, when coal was privatised."
llantwitfardrecommunitycouncil.org
"Coke is a fuel with few impurities and a high carbon content, usually made from coal. It is the solid carbonaceous material derived from destructive distillation of low-ash, low-sulfur bituminous coal. Coke made from coal are grey, hard, and porous. While coke can be formed naturally, the commonly used form is man-made. The form known as petroleum coke, or pet coke, is derived from oil refinery coker units or other cracking processes."
Wiki
Fforio/Explore : Cwm Coke Works
Cwm Coke Works
1958 - 2002
"In the 1970s, the cokeworks employed 1,500 men and produced some 515,000 tonnes of coke each year. It continued to do so until 1986, when coal was privatised."
llantwitfardrecommunitycouncil.org
"Coke is a fuel with few impurities and a high carbon content, usually made from coal. It is the solid carbonaceous material derived from destructive distillation of low-ash, low-sulfur bituminous coal. Coke made from coal are grey, hard, and porous. While coke can be formed naturally, the commonly used form is man-made. The form known as petroleum coke, or pet coke, is derived from oil refinery coker units or other cracking processes."
Wiki