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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Atlantic Ocean
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North Atlantic
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Irish Sea (1)
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Canada
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Eastern Canada
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Newfoundland and Labrador
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Newfoundland
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Notre Dame Bay (1)
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Europe
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Western Europe
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Ireland (4)
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United Kingdom
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Great Britain
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England (1)
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Scotland
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Galloway Scotland (2)
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Mexico
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Baja California Mexico (1)
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Southern Uplands (9)
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commodities
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brines (1)
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metal ores
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cobalt ores (1)
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copper ores (1)
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zinc ores (1)
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mineral deposits, genesis (1)
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petroleum (1)
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elements, isotopes
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isotope ratios (1)
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isotopes
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stable isotopes
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Sr-87/Sr-86 (1)
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metals
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alkaline earth metals
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strontium
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Sr-87/Sr-86 (1)
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lead (1)
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rare earths (1)
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fossils
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Graptolithina (1)
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Invertebrata
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Mollusca (1)
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Protista
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Radiolaria (1)
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microfossils
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Conodonta (1)
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geochronology methods
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K/Ar (1)
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geologic age
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Cenozoic
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Quaternary
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Pleistocene
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upper Pleistocene
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Devensian (1)
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-
-
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Tertiary (1)
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Mesozoic
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Triassic
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Sherwood Sandstone (1)
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Upper Triassic
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Mercia Mudstone (1)
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Paleozoic
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Devonian (1)
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lower Paleozoic (1)
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Ordovician (4)
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Permian (1)
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Silurian
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Lower Silurian
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Llandovery (2)
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Wenlock (2)
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igneous rocks
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igneous rocks (1)
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minerals
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oxides
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manganese oxides (1)
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-
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Primary terms
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absolute age (1)
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Atlantic Ocean
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North Atlantic
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Irish Sea (1)
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-
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brines (1)
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Canada
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Eastern Canada
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Newfoundland and Labrador
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Newfoundland
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Notre Dame Bay (1)
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-
-
-
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Cenozoic
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Quaternary
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Pleistocene
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upper Pleistocene
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Devensian (1)
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-
-
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Tertiary (1)
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continental drift (1)
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deformation (4)
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diagenesis (1)
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epeirogeny (1)
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Europe
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Western Europe
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Ireland (4)
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United Kingdom
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Great Britain
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England (1)
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Scotland
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Galloway Scotland (2)
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-
-
-
-
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faults (7)
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folds (3)
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foliation (1)
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Graptolithina (1)
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igneous rocks (1)
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Invertebrata
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Mollusca (1)
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Protista
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Radiolaria (1)
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-
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isotopes
-
stable isotopes
-
Sr-87/Sr-86 (1)
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-
-
Mesozoic
-
Triassic
-
Sherwood Sandstone (1)
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Upper Triassic
-
Mercia Mudstone (1)
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-
-
-
metal ores
-
cobalt ores (1)
-
copper ores (1)
-
zinc ores (1)
-
-
metals
-
alkaline earth metals
-
strontium
-
Sr-87/Sr-86 (1)
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-
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lead (1)
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rare earths (1)
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Mexico
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Baja California Mexico (1)
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mineral deposits, genesis (1)
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paleoclimatology (1)
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paleogeography (1)
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Paleozoic
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Devonian (1)
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lower Paleozoic (1)
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Ordovician (4)
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Permian (1)
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Silurian
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Lower Silurian
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Llandovery (2)
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Wenlock (2)
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paragenesis (1)
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petroleum (1)
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petrology (1)
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plate tectonics (2)
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sedimentary petrology (2)
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sedimentary rocks
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clastic rocks
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sandstone (1)
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sedimentary structures
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soft sediment deformation (1)
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stratigraphy (4)
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structural analysis (1)
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structural geology (4)
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symposia (1)
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tectonics (7)
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tectonophysics (2)
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sedimentary rocks
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sedimentary rocks
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clastic rocks
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sandstone (1)
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sedimentary structures
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sedimentary structures
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soft sediment deformation (1)
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Wigtownshire
The Portencorkrie complex of Wigtownshire
Along-strike variation in the stratigraphical and structural profile of the Southern Uplands Central Belt in Galloway and Down
Pre-Late Devensian high-arctic marine deposits in SW Scotland
The Southern Uplands of Scotland: A Lower Palaeozoic accretionary prism
Structural histories in the SW Southern Uplands, Scotland
A sequential back-arc and foreland basin thrust duplex model for the Southern Uplands of Scotland
The Northern Belt of the Longford-Down Inlier, Ireland and Southern Uplands, Scotland: an Ordovician back-arc basin
Style, scale and significance of sand bodies in the Northern and Central Belts, southwest Southern Uplands
Tectonic development of the Southern Belt of the Southern Uplands accretionary complex
Deformation of soft sediments
A correlation of Silurian rocks in the British Isles
Structural constraints on closure geometry across the Iapetus suture in eastern Ireland
Stratigraphy and Structure of Northeastern Newfoundland Bearing on Drift in North Atlantic
The structure of the western part of the Southern Uplands of Scotland
Geology and petroleum prospectivity of the Larne and Portpatrick basins, North Channel, offshore SW Scotland and Northern Ireland
Metalliferous Manganese Oxide Mineralization Associated with the Boléo Cu-Co-Zn District, Mexico
‘A charm to impose on the vulgar’: the medicinal and magical applications of the snakestone bead within the British Isles
Abstract: The medicinal uses of the snakestone bead within the British Isles are surveyed and considered for the first time. The snakestone beads of the British Isles – often annular beads formed of glass or paste, but also other items similar in form – were employed against a variety of ailments, including several of the most deadly childhood diseases of the nineteenth century: teething, whooping cough and ague. In addition, they were used in the treatment of livestock and as a remedy for eye diseases. The eighteenth century saw the snakestone beads conflated with the hag-stone and employed as an amulet against witches and evil spirits.
Themes in the early history of Scottish geology
Abstract In this chapter, new to this edition of The Geology of Scotland, we discuss some of the more interesting and important themes and personalities relating to the early history of Scottish geology. The topic is vast, and clearly it is impossible to cover all possible themes. A ‘regional’ approach is adopted, concentrating on selected areas of particular importance. Present debates are necessarily rooted in the past. They grow from a complex intertwining of geographical, theoretical, personal, social, methodological, institutional and economic factors. We have sought to refer, albeit briefly, to all such aspects, but different features receive different emphases in the different regional accounts. The emphasis is chiefly on 19th century geology, but in most cases discussion has been carried through to the early 20th century, and in some cases we have briefly indicated how matters developed closer to the present. Although the material is organised chiefly by regions, an effort has also been made, as far as the subject matter allows, to provide a historically integrated account. Thus, we hope to offer a useful historical background to the more technical topics that appear in following chapters. The aim, however, is not to see the past from the eyes of the present; rather to see the present with the assistance of some knowledge of the past. Reversing the old adage, we should like to show that ‘the past is the key to the present’.