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NARROW
GeoRef Subject
-
all geography including DSDP/ODP Sites and Legs
-
Africa
-
Limpopo Belt (1)
-
North Africa
-
Egypt
-
Eastern Desert (1)
-
-
-
Southern Africa
-
Namibia (1)
-
Zimbabwe (1)
-
-
Zimbabwe Craton (1)
-
-
Arctic Ocean
-
Nares Strait (1)
-
-
Arctic region
-
Greenland (2)
-
-
Atlantic Ocean
-
Mid-Atlantic Ridge (1)
-
North Atlantic
-
Labrador Sea (1)
-
-
-
Atlantic Ocean Islands
-
Falkland Islands (1)
-
-
Australasia
-
Australia
-
Queensland Australia (1)
-
South Australia
-
Gawler Craton (1)
-
Olympic Dam Deposit (1)
-
-
-
New Zealand (1)
-
-
Baffin Bay (1)
-
Canada
-
Arctic Archipelago (1)
-
Western Canada
-
Northwest Territories (1)
-
-
-
Europe
-
Alps (1)
-
Central Europe
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Germany (1)
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Upper Rhine Graben (1)
-
-
Western Europe
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Iceland
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Hekla (1)
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Katla (1)
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Vatnajokull (1)
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Vestmannaeyjar (1)
-
-
United Kingdom
-
Great Britain
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England
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Cornwall England (2)
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Derbyshire England (1)
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Devon England (2)
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Essex England (1)
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Kent England
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Isle of Sheppey (1)
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-
London England (1)
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Northamptonshire England (1)
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Yorkshire England
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North Yorkshire England (1)
-
-
-
Wales
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South Wales (1)
-
-
-
-
-
-
Iron Mountain (1)
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Mexico (1)
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North America
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Rocky Mountains (1)
-
-
Owens Valley (1)
-
Pacific Ocean (1)
-
San Andreas Fault (1)
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Santa Cruz Mountains (1)
-
Searles Lake (1)
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Sierra Nevada (1)
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South America
-
Andes (1)
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Argentina (1)
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Chile (1)
-
Falkland Islands (1)
-
Patagonia (1)
-
Tierra del Fuego (1)
-
-
Storegga Slide (1)
-
Twin Lakes (1)
-
United States
-
Arkansas (1)
-
California
-
Inyo County California
-
Coso Range (1)
-
Owens Lake (1)
-
-
Southern California (1)
-
-
Colorado
-
Fremont County Colorado
-
Canon City Colorado (1)
-
-
-
Eastern U.S.
-
Northeastern U.S. (1)
-
-
Kansas (1)
-
Massachusetts
-
Middlesex County Massachusetts (1)
-
-
Missouri
-
Greene County Missouri
-
Springfield Missouri (1)
-
-
Saint Francois Mountains (1)
-
Taney County Missouri (1)
-
-
Montana
-
Silver Bow County Montana
-
Butte Montana (1)
-
-
-
Ohio
-
Mahoning County Ohio (1)
-
-
Oklahoma (1)
-
Ozark Mountains (2)
-
Pennsylvania
-
Lawrence County Pennsylvania (1)
-
-
Texas (1)
-
-
-
commodities
-
coal deposits (1)
-
construction materials
-
building stone (1)
-
dimension stone (1)
-
-
fluorspar deposits (1)
-
geothermal energy (2)
-
heavy mineral deposits (1)
-
limestone deposits (1)
-
metal ores
-
aluminum ores (1)
-
antimony ores (1)
-
arsenic ores (4)
-
chromite ores (1)
-
copper ores (8)
-
gold ores (3)
-
IOCG deposits (2)
-
iron ores (2)
-
lead ores (1)
-
lead-zinc deposits (1)
-
magnesium ores (1)
-
molybdenum ores (1)
-
nickel ores (2)
-
niobium ores (1)
-
rare earth deposits (1)
-
tantalum ores (1)
-
tin ores (2)
-
titanium ores (1)
-
zinc ores (1)
-
-
mineral deposits, genesis (5)
-
mineral exploration (6)
-
mineral resources (5)
-
new energy sources (1)
-
petroleum
-
natural gas (1)
-
-
placers (1)
-
sand deposits (1)
-
zircon deposits (1)
-
-
elements, isotopes
-
carbon
-
C-13/C-12 (1)
-
organic carbon (1)
-
-
hydrogen
-
D/H (1)
-
-
isotope ratios (3)
-
isotopes
-
radioactive isotopes
-
Pb-210 (1)
-
Ra-226 (1)
-
U-238 (1)
-
-
stable isotopes
-
C-13/C-12 (1)
-
D/H (1)
-
Nd-144/Nd-143 (1)
-
O-18/O-16 (2)
-
S-34/S-32 (1)
-
-
-
metals
-
actinides
-
uranium
-
U-238 (1)
-
-
-
alkaline earth metals
-
calcium (1)
-
radium
-
Ra-226 (1)
-
-
strontium (1)
-
-
aluminum (1)
-
antimony (2)
-
arsenic (5)
-
bismuth (1)
-
cadmium (1)
-
lead
-
Pb-210 (1)
-
-
mercury (1)
-
nickel (1)
-
rare earths
-
neodymium
-
Nd-144/Nd-143 (1)
-
-
-
thallium (1)
-
-
noble gases
-
radon (1)
-
-
oxygen
-
O-18/O-16 (2)
-
-
selenium (1)
-
sulfur
-
S-34/S-32 (1)
-
-
tellurium (1)
-
-
fossils
-
bacteria (1)
-
Chordata
-
Vertebrata
-
Agnatha (1)
-
Tetrapoda
-
Mammalia (1)
-
-
-
-
Invertebrata
-
Cnidaria
-
Anthozoa (1)
-
-
Protista
-
Foraminifera (1)
-
-
-
microfossils (1)
-
palynomorphs
-
Dinoflagellata (1)
-
miospores (1)
-
-
-
geochronology methods
-
paleomagnetism (1)
-
tree rings (1)
-
U/Pb (1)
-
-
geologic age
-
Anthropocene (2)
-
Cenozoic
-
Quaternary
-
Holocene (2)
-
Pleistocene
-
upper Pleistocene
-
Weichselian
-
upper Weichselian
-
Younger Dryas (1)
-
-
-
-
-
-
Tertiary
-
Paleogene
-
Eocene
-
lower Eocene
-
Ypresian
-
London Clay (1)
-
-
-
-
Paleocene
-
lower Paleocene
-
Danian (1)
-
-
-
-
-
-
Mesozoic
-
Cretaceous
-
Comanchean
-
Comanche Peak Limestone (1)
-
Glen Rose Formation (1)
-
Pearsall Formation (1)
-
-
Lower Cretaceous
-
Comanche Peak Limestone (1)
-
Glen Rose Formation (1)
-
Hosston Formation (1)
-
Pearsall Formation (1)
-
Sligo Formation (1)
-
-
-
-
Paleozoic
-
Carboniferous
-
Mississippian
-
Lower Mississippian
-
Osagian
-
Burlington Limestone (1)
-
Keokuk Limestone (1)
-
-
-
-
-
-
Precambrian
-
Archean
-
Mesoarchean (1)
-
Neoarchean (1)
-
-
upper Precambrian
-
Proterozoic
-
Mesoproterozoic (1)
-
Neoproterozoic (1)
-
Paleoproterozoic (1)
-
-
-
-
-
igneous rocks
-
igneous rocks
-
plutonic rocks
-
granites (4)
-
pegmatite (2)
-
syenites
-
nepheline syenite
-
agpaite (1)
-
-
-
ultramafics
-
chromitite (1)
-
-
-
volcanic rocks
-
basalts
-
columnar basalt (1)
-
-
komatiite (1)
-
pyroclastics
-
tuff (1)
-
-
-
-
-
metamorphic rocks
-
metamorphic rocks
-
metasomatic rocks
-
fenite (1)
-
skarn (1)
-
-
schists
-
greenstone (1)
-
-
-
-
minerals
-
arsenates (3)
-
arsenides
-
arsenopyrite (1)
-
-
arsenites (3)
-
oxides
-
ilmenite (1)
-
iron oxides (1)
-
leucoxene (1)
-
magnetite (1)
-
rutile (1)
-
-
phosphates
-
fluorapatite (1)
-
monazite (1)
-
xenotime (1)
-
-
platinum minerals (1)
-
silicates
-
asbestos (1)
-
orthosilicates
-
nesosilicates
-
zircon group
-
zircon (1)
-
-
-
-
-
sulfates
-
alunite (1)
-
-
sulfides
-
arsenopyrite (1)
-
chalcopyrite (1)
-
copper sulfides (1)
-
digenite (1)
-
galena (1)
-
iron sulfides (1)
-
nickel sulfides (1)
-
pyrite (1)
-
sphalerite (1)
-
stibnite (1)
-
-
sulfosalts (2)
-
-
Primary terms
-
Africa
-
Limpopo Belt (1)
-
North Africa
-
Egypt
-
Eastern Desert (1)
-
-
-
Southern Africa
-
Namibia (1)
-
Zimbabwe (1)
-
-
Zimbabwe Craton (1)
-
-
Arctic Ocean
-
Nares Strait (1)
-
-
Arctic region
-
Greenland (2)
-
-
Atlantic Ocean
-
Mid-Atlantic Ridge (1)
-
North Atlantic
-
Labrador Sea (1)
-
-
-
Atlantic Ocean Islands
-
Falkland Islands (1)
-
-
Australasia
-
Australia
-
Queensland Australia (1)
-
South Australia
-
Gawler Craton (1)
-
Olympic Dam Deposit (1)
-
-
-
New Zealand (1)
-
-
bacteria (1)
-
Canada
-
Arctic Archipelago (1)
-
Western Canada
-
Northwest Territories (1)
-
-
-
carbon
-
C-13/C-12 (1)
-
organic carbon (1)
-
-
Cenozoic
-
Quaternary
-
Holocene (2)
-
Pleistocene
-
upper Pleistocene
-
Weichselian
-
upper Weichselian
-
Younger Dryas (1)
-
-
-
-
-
-
Tertiary
-
Paleogene
-
Eocene
-
lower Eocene
-
Ypresian
-
London Clay (1)
-
-
-
-
Paleocene
-
lower Paleocene
-
Danian (1)
-
-
-
-
-
-
chemical analysis (1)
-
Chordata
-
Vertebrata
-
Agnatha (1)
-
Tetrapoda
-
Mammalia (1)
-
-
-
-
coal deposits (1)
-
construction materials
-
building stone (1)
-
dimension stone (1)
-
-
crust (2)
-
crystal chemistry (3)
-
crystal structure (1)
-
dams (2)
-
deformation (2)
-
earthquakes (2)
-
economic geology (1)
-
engineering geology (1)
-
Europe
-
Alps (1)
-
Central Europe
-
Germany (1)
-
Upper Rhine Graben (1)
-
-
Western Europe
-
Iceland
-
Hekla (1)
-
Katla (1)
-
Vatnajokull (1)
-
Vestmannaeyjar (1)
-
-
United Kingdom
-
Great Britain
-
England
-
Cornwall England (2)
-
Derbyshire England (1)
-
Devon England (2)
-
Essex England (1)
-
Kent England
-
Isle of Sheppey (1)
-
-
London England (1)
-
Northamptonshire England (1)
-
Yorkshire England
-
North Yorkshire England (1)
-
-
-
Wales
-
South Wales (1)
-
-
-
-
-
-
explosions (1)
-
faults (3)
-
fluorspar deposits (1)
-
foundations (1)
-
geochemistry (2)
-
geology (1)
-
geomorphology (3)
-
geophysical methods (1)
-
geothermal energy (2)
-
glacial geology (1)
-
ground water (5)
-
heavy mineral deposits (1)
-
hydrogen
-
D/H (1)
-
-
hydrology (1)
-
igneous rocks
-
plutonic rocks
-
granites (4)
-
pegmatite (2)
-
syenites
-
nepheline syenite
-
agpaite (1)
-
-
-
ultramafics
-
chromitite (1)
-
-
-
volcanic rocks
-
basalts
-
columnar basalt (1)
-
-
komatiite (1)
-
pyroclastics
-
tuff (1)
-
-
-
-
intrusions (6)
-
Invertebrata
-
Cnidaria
-
Anthozoa (1)
-
-
Protista
-
Foraminifera (1)
-
-
-
isotopes
-
radioactive isotopes
-
Pb-210 (1)
-
Ra-226 (1)
-
U-238 (1)
-
-
stable isotopes
-
C-13/C-12 (1)
-
D/H (1)
-
Nd-144/Nd-143 (1)
-
O-18/O-16 (2)
-
S-34/S-32 (1)
-
-
-
land subsidence (1)
-
land use (1)
-
limestone deposits (1)
-
magmas (2)
-
mantle (3)
-
maps (1)
-
Mesozoic
-
Cretaceous
-
Comanchean
-
Comanche Peak Limestone (1)
-
Glen Rose Formation (1)
-
Pearsall Formation (1)
-
-
Lower Cretaceous
-
Comanche Peak Limestone (1)
-
Glen Rose Formation (1)
-
Hosston Formation (1)
-
Pearsall Formation (1)
-
Sligo Formation (1)
-
-
-
-
metal ores
-
aluminum ores (1)
-
antimony ores (1)
-
arsenic ores (4)
-
chromite ores (1)
-
copper ores (8)
-
gold ores (3)
-
IOCG deposits (2)
-
iron ores (2)
-
lead ores (1)
-
lead-zinc deposits (1)
-
magnesium ores (1)
-
molybdenum ores (1)
-
nickel ores (2)
-
niobium ores (1)
-
rare earth deposits (1)
-
tantalum ores (1)
-
tin ores (2)
-
titanium ores (1)
-
zinc ores (1)
-
-
metals
-
actinides
-
uranium
-
U-238 (1)
-
-
-
alkaline earth metals
-
calcium (1)
-
radium
-
Ra-226 (1)
-
-
strontium (1)
-
-
aluminum (1)
-
antimony (2)
-
arsenic (5)
-
bismuth (1)
-
cadmium (1)
-
lead
-
Pb-210 (1)
-
-
mercury (1)
-
nickel (1)
-
rare earths
-
neodymium
-
Nd-144/Nd-143 (1)
-
-
-
thallium (1)
-
-
metamorphic rocks
-
metasomatic rocks
-
fenite (1)
-
skarn (1)
-
-
schists
-
greenstone (1)
-
-
-
metamorphism (1)
-
Mexico (1)
-
mineral deposits, genesis (5)
-
mineral exploration (6)
-
mineral resources (5)
-
mining geology (1)
-
noble gases
-
radon (1)
-
-
North America
-
Rocky Mountains (1)
-
-
orogeny (1)
-
oxygen
-
O-18/O-16 (2)
-
-
Pacific Ocean (1)
-
paleoclimatology (1)
-
paleoecology (1)
-
paleomagnetism (1)
-
Paleozoic
-
Carboniferous
-
Mississippian
-
Lower Mississippian
-
Osagian
-
Burlington Limestone (1)
-
Keokuk Limestone (1)
-
-
-
-
-
-
palynomorphs
-
Dinoflagellata (1)
-
miospores (1)
-
-
paragenesis (3)
-
petroleum
-
natural gas (1)
-
-
phase equilibria (1)
-
placers (1)
-
plate tectonics (2)
-
pollution (6)
-
Precambrian
-
Archean
-
Mesoarchean (1)
-
Neoarchean (1)
-
-
upper Precambrian
-
Proterozoic
-
Mesoproterozoic (1)
-
Neoproterozoic (1)
-
Paleoproterozoic (1)
-
-
-
-
reclamation (2)
-
remote sensing (1)
-
roads (2)
-
rock mechanics (2)
-
sand deposits (1)
-
sea-floor spreading (1)
-
sea-level changes (1)
-
sedimentary rocks
-
chemically precipitated rocks
-
chert (1)
-
-
clastic rocks
-
conglomerate (1)
-
-
coal (1)
-
-
sedimentation (1)
-
sediments
-
clastic sediments
-
dust (1)
-
-
marine sediments (1)
-
-
seismology (1)
-
selenium (1)
-
shorelines (1)
-
slope stability (1)
-
soil mechanics (2)
-
soils
-
Anthrosols (1)
-
-
South America
-
Andes (1)
-
Argentina (1)
-
Chile (1)
-
Falkland Islands (1)
-
Patagonia (1)
-
Tierra del Fuego (1)
-
-
springs (2)
-
stratigraphy (1)
-
sulfur
-
S-34/S-32 (1)
-
-
tectonics
-
neotectonics (1)
-
-
tellurium (1)
-
thermal waters (2)
-
tunnels (1)
-
United States
-
Arkansas (1)
-
California
-
Inyo County California
-
Coso Range (1)
-
Owens Lake (1)
-
-
Southern California (1)
-
-
Colorado
-
Fremont County Colorado
-
Canon City Colorado (1)
-
-
-
Eastern U.S.
-
Northeastern U.S. (1)
-
-
Kansas (1)
-
Massachusetts
-
Middlesex County Massachusetts (1)
-
-
Missouri
-
Greene County Missouri
-
Springfield Missouri (1)
-
-
Saint Francois Mountains (1)
-
Taney County Missouri (1)
-
-
Montana
-
Silver Bow County Montana
-
Butte Montana (1)
-
-
-
Ohio
-
Mahoning County Ohio (1)
-
-
Oklahoma (1)
-
Ozark Mountains (2)
-
Pennsylvania
-
Lawrence County Pennsylvania (1)
-
-
Texas (1)
-
-
waste disposal (2)
-
weathering (1)
-
X-ray analysis (1)
-
zircon deposits (1)
-
-
sedimentary rocks
-
sedimentary rocks
-
chemically precipitated rocks
-
chert (1)
-
-
clastic rocks
-
conglomerate (1)
-
-
coal (1)
-
-
-
sediments
-
sediments
-
clastic sediments
-
dust (1)
-
-
marine sediments (1)
-
-
-
soils
-
soils
-
Anthrosols (1)
-
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Smelt Hill Dam
Abstract In the northeastern United States, we have been removing dams for almost as long as we have been building them, yet many communities involved in current decisions to repair, replace, or remove a dam are not aware of this. This paper highlights some of the stories that have been recorded regarding the history of decision points for dams, including the colorful history of the Billerica Dam in Massachusetts, which has been removed and rebuilt numerous times and is now under consideration for removal for at least the sixth time in its 300 yr history. By understanding that dam removal is just one of the potential dam safety decisions that needs to be analyzed over the life cycle of a dam, and that dams are man-made structures with finite life spans, we can deconstruct the notion of dam removal as a radical concept. Dam removal is just one of many dam safety options that may be discussed over the course of a dam’s history. It is most commonly implemented when a dam no longer serves any economic purpose that justifies the expense of maintaining the dam structure. In the past, dams have been removed for many of the same reasons that we remove dams today; however, the procedures currently required to remove a dam are far more complex and highly regulated. This has led to increased documentation of dam removal efforts and now allows us to compare and categorize dam removal projects, such that the lessons learned from these projects can be incorporated into a more informed decision-making process in the future.
Geologic Road Log of Pan-american Highway, Laredo to Mexico City
THE IMPORTANCE OF GEOLOGY IN ASSESSING BY- AND COPRODUCT METAL SUPPLY POTENTIAL; A CASE STUDY OF ANTIMONY, BISMUTH, SELENIUM, AND TELLURIUM WITHIN THE COPPER PRODUCTION STREAM
History and Historical Resources of the Vermont Copper Belt
Abstract The Vermont copper belt includes the Elizabeth mine in South Strafford, the Ely Mine in Vershire, and the Pike Hill mines in Corinth. Of these the Elizabeth mine operated over the longest period of time, produced the highest tonnage of copper and left the largest and most complex collection of historic resources. The Elizabeth mine site is complex and represents approximately 160 years of industrial activity from 1809 to 1958. It was the site of a major 19th century U.S. copperas manufacturing plant, and several important firsts in American copper smelting. It was the site of no less than nine copper ore smelting campaigns and multiple ore concentration milling phases. The extent of industrial operations encompassed hundreds of acres. The Elizabeth mine produced an estimated 4,726,800 kg (10,500,000 lbs) of copper before its World War II revival. During the subsequent campaign the mine became the largest and most productive copper mine in New England, and yielded another 41,502,495 kg (91,495,800 lbs) of copper. Briefly during the 1950s it was one of the top 20 U.S. copper producers. The unique copperas works remains and the World War II-era remains constitute one of the largest and least disturbed historic mining sites in New England. This landscape includes the only intact cluster of historic hard-rock metal-mine plant buildings in the region. The Ely mine orebody was discovered in 1813 and explored during the 1830s, but it was most active between the mid-1850s and about 1905. Mining began seriously in 1853 with the incorporation of the Vermont Copper Mining Company. For the next 13 years the ore was shipped to east coast smelters. The mine eventually came under the control of Smith Ely, for which it is named. In 1867 the company built its own smelter on the mine site. This plant was periodically expanded to become a massive mid-19th century nonferrous metallurgical works, more than 122 m (700 ft) long with 24 smelting furnaces. By the mid-1870s the town of Ely had become a mining boomtown and in 1883, the town was the site of the “Ely War” labor conflict. The Ely mine was the only copper mine in Vermont where all technological aspects of refined copper production, from mining of raw ore to smelting of refined ingot copper, were successfully integrated on a large scale. The site geography at the Ely mine dictated a confined, straight-line flow of materials and processes, and today the historic landscape expresses copper production in a linear, understandable way. Total copper output for the Vermont copper belt mines between 1793 and 1958 has been estimated at about 65.8 million kg (145 million lbs), with about 25 million kg (100 million lbs) from the Elizabeth mine, about 16 million kg (35 million lbs) from Ely and under 4.5 million kg (10 million lbs) from Pike Hill ( Abbott, 1964 ; Howard, 1969 ). In addition to their economic contribution, the Vermont copper belt mines also contributed to the historic legacy and landscape of New England. They have left unusual stories and sites that convey the drama and impact of hard rock mining, an industry not usually associated with New England.