Read online The Geology of Lower Strathspey: Explanation of Sheet 85 (Classic Reprint) - Lionel Wordsworth Hinxman | ePub
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Zaleski e (1983) the geology of strathspey and lower findhorn granitoids—a study involving field relations, petrography, mineralogy, geochemistry and geochronology.
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The pre-cambrian rocks of england and wales make their appearance in a number of isolated inliers, rising from beneath cambrian or newer rocks.
Principal vegetation types also significant, particularly the nw-se lineation in lower strathspey which combines.
Two lithostratigraphic formations were recognised in the lower glenshirra succession, while four formations as well as a transitional lithostratigraphic unit were recognised in the overlying corrieyairack succession.
Strathspey brent geology • favorable mobility ratio has led to efficient sweep in general –main field wells • geological heterogeneity and complex faulting in the slumped areas has led to localized early water breakthrough and poorer waterflood efficiencies. Top brent depth structure 1km brent central brent south ms19 ms9 m10 m6 ms14 m5 m11 12 m3 5 m7 m9 m15z.
—the geology and vegetation of late-glacial retreat stages in scotland.
In the very heart of the scottish highlands, the name strathspey strikes an instant chord with strathspey self catering cottages.
—memoirs of the geological survey of scotland - the geology of mid-strathspey and strathdearn.
Strathspey at least as far as grantown-on-spey (young, 1974, 1975a, b, 1977a. 1978), as for however, evidence for strong northward flow had been identified in the lower dulnain memoir of the geological survey of scotland, sheet.
The field was discovered in 1975 by well 3/4-4 and lies wholly within block 3/4a. The field is a tilted fault block, unconformity trap and consists of two separate reservoirs, a volatile oil and a gas condensate reservoir: the middle jurassic, brent group and the lower jurassic/upper triassic, banks group respectively.
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The geology of lower strathspey (explanation of sheet 85) (with petrological chapter and notes by js flett) mem geol surv g b (scotl) (sheet) (edinburgh) full entry 1923.
The geology of upper strathspey, gaick and the forest of atholl. Memoir of the geological survey of scotland, sheet 64 (scotland). Memoir of the geological survey of scotland, sheet 64 (scotland).
An area of 120km2 extending from loch laggan to the upper reaches of the river spey has been mapped in detail on a scale of 1:10,000. The metasediments cropping out in this area have been assigned to the grampian division and consist of varied assemblages of psammltes, semi-psammites and semi-pelites which can be subdivided into two lithostratigraphic successions separated by a tectonic.
The metasedimentary rocks of the loch laggan-upper strathspey area form part of the grampian division of the caledonides in the grampian highlands. They comprise two lithostratigraphic successions, the glenshirra and the corrieyairack successions, which are separated by a zone of high strain, the gairbeinn slide. Both successions consist dominantly of non-calcareous clastic metasediments.
Major and minor structures in the moinian and dalradian rocks of the monadhliath mountains are described and the tectonic history of the area outlined. Early major structures, isoclinal recumbent folds with north-east trending axial planes, are refolded by late asymmetric folds with north-east trending axial planes dipping steeply to the south-east.
There is little simple relationship between geology and relief in upper spey and a complex that separates the lower dulnain valley from strathspey.
Geology of the lower suwannee river basin previous investigations our knowledge of the geology of the counties included in the lower suwannee river basin has mostly been pioneered by cooke (1945), who made some observations on the geology of these counties in his geology of florida.
5-minute quadrangle, located in the core of the southeast idaho phosphate resource area, includes mississippian to triassic marine sedimentary rocks, pliocene to pleistocene basalt, and tertiary to holocene surficial deposits.
The lower section in california, nevada, and arizona is younger than the upper portion in utah and colorado. The age of the younger portion of the river is estimated to be between 5 and 6 million years based on the various constraints listed in the ages section.
Aviemore lies on the b9152 (the old a9 road since the main road from inverness to perth was rebuilt further west in 1980). Aviemore railway station is on the highland main line and aviemore is also the southern terminus of the strathspey railway, a heritage railway.
976 paludal sediment: organic silt, sand, and organic accumulations deposited in swamps or marshes. 72 ice-contact stratified drift: coarse to fine sand and/or gravel. Inferred where constructional topography suggests collapse of subjacent.
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The balcomie beds of east fife, formerly classified in the upper old red sandstone, are now considered to be of the same general age as the lithologically similar downie's loup sandstones of stirling and the calcareous sandstones of west fife. It therefore follows that ballagan beds (cementstones) may be present at depth at balcomie. It is suggested that all three fluvial sandstone formations.
The cairngorms are a mountain range in the eastern highlands of scotland closely associated such as the angus glens and the monadhliath, and lower areas like strathspey.
The saltwick formation is composed of 10 sedimentary fa-cies – coal (c1), claystone (cl1), root-penetrated siltstone (sl1), very fine to fine-grained sandstone sheets (fs1), very fine to fine-grained sandstone channels (fs2), medium-grained sandstone.
Since the onset of production in 1993, extraction and injection in strathspey has focused on the central region of the field, around the ‘central fault’.
Memoir of the geological survey, scotland, sheet 85 (scotland).
The cainozoic geology and landscape evolution of north-east scotland. Memoir of the british geological survey, sheets 66e, 67, 76e, 77, 86e, 87w, 87e, 95, 96w, 96e and 97 (scotland) 1:50k maps on which the lithostratigraphical unit is found, and map code used:.
Surficial geology –it’s more than what you see at the surface! 9complex surficial geology in the lower mainland 9thick sedimentary package overlying bedrock 9glacial, fluvial and bog deposits; varying porosity, organic content and mineralogy. Introduction gsc map 1486a, surficial geology vancouver, 1980.
The geology of lower strathspey (explanation of sheet 85) (with petrological chapter and notes by js flett) mem geol surv g b (scotl) (sheet) (edinburgh) ref no dp085.
During deglaciation meltwaters laid down extensive spreads of sand and gravel, particularly on the low ground on the south side of the moray firth from the north end of the great glen to near elgin, and also in strathspey.
The geology of lower strathspey (explanation of sheet 85) / by 1855-1936.
Plate 16 appears by kind permission of seafield and strathspey estates/mr will anderson. Plates 2, 8b, 8c, 9c, 9d, 12b, 19 and 25 are reproduced here by kind permission of the forestry commission. Plate 3 is reproduced here by kind permission of the national library.
Shaffner 1951 well symbols gas tj- dry, shallow dry, oriskany preliminary map of geologic structure on base of lower kittanning coal in new florence quadrangle pennsylvania elevation in feet above sea level contour interval 100 feet pennsylvania geological survey series, progress report 137 1951 earth and mineral l(3r.
Most of the surficial geologic maps are available for the southern part of the lower peninsula while county scale bedrock geologic and bedrock topographic maps are available for northern part of lower peninsula. There are limited mappings done in the upper peninsula of michigan.
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