Sticklepath lustleigh fault
http://mr.crossref.org/iPage?doi=10.1144%2Fgsjgs.143.3.0447 WebSticklepath is a village on Dartmoor, in the county of Devon, England. It gives its name to one of the most important geological faults in south-west England, thought to have originated during the Tertiary period and known variously as the Sticklepath Fault, Sticklepath Fault Zone, Lustleigh-Sticklepath Fault or Sticklepath-Lustleigh Fault.[1]
Sticklepath lustleigh fault
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WebThe Sticklepath-Lustleigh Fault zone and associated Tertiary pull-apart basins e.g. Bovey Basin (Edwards, 1976); Petrockstow Basin (Bristow et al., 1992) are important ... Parrett Valley Fault, 1 km west of Ham Hill, has a dextral displacement on the basis that the E-W Coker Fault appears to have been offset. Harvey and Stewart (1998) have ... WebOct 13, 2024 · Devon has a naturally occurring dissecting line called the Sticklepath - Lustleigh Fault Zone referred to in some text as Devon’s own San Andreas fault line. Running from North-West to South-East from near Clovelly in North Devon, it passes through the Dartmoor village of Sticklepath near Okehampton before ending in Torquay in South Devon.
WebWe present an alternative model for the history of the Sticklepath-Lustleigh fault zone, summarized below: 1 Late Variscan strike-slip movement, with a total displacement of up … WebComplex faulting in the Lustleigh area is described. The fracture-pattern consists of a late NW-SE fault-system with associated NNW-SSE faults, which is superimposed on an …
WebThe hot, wet climatic conditions were continuing, as was the erosion of the region’s deeply weathered uplands. However, now, a massive fault known as the Sticklepath-Lustleigh … WebThe Sticklepath-Lustleigh Fault Zone, a structure known to have experienced multiple displacements[4], will be used as a control. The student will build and interpret 3D structural models of the fault zones. Dr Peacock is an expert in the safe and effective use of drones for geological studies[10] and will supervise these
WebA strong aeromagnetic anomaly, with a maximum over the peridotite SW of Coverack, extends both offshore and to the NW, across the mapped contact of the Crousa gabbro and western peridotite, and over the Traboe cumulate complex. At ground level, this anomaly appears to be discontinuous.
http://ussher.org.uk/wp-content/uploads/journal/2005/14-Prudden.pdf free papercraft mask templatesWebApart from map-scale structures, identification of minor structures associated with major faults, such as slickensides observed within the near-surface parts of fault zones, horsetail splays,... farmers ins in little rock arWebMar 26, 2024 · Lustleigh Cleave, means “cliff” or “cleft”, in old English. The Cleave itself is a large geological fault line (the steep valley) which forms part of the Sticklepath fault line that starts in Torquay and forms a line through the Bovey Basin, along the eastern edge of Dartmoor (including Lustleigh Cleave) and on to Bideford Bay in north Devon. free papercraft log cottage templatesWebWe present an alternative model for the history of the Sticklepath-Lustleigh fault zone, summarized below: 1 Late Variscan strike-slip movement, with a total displacement of up to 10 km, produced the SLFZ and offset dextrally an earlier Variscan thrust. 2. Extensional reactivation of this thrust led to rapid Permo-Triassic subsidence in the ... farmers ins. in boise idahoWebDextral strike-slip movement on the Sticklepath-Lustleigh fault zone (SLFZ) is indicated by displacements of ?Permian and older rocks. Previous authors have inferred that the main … free papercraft pdf downloadWebThe Sticklepath Fault provided an almost unique set of circumstances which allowed formation and maintenance of these ball clay pits: erosion of rocks into fresh or brackish … farmers ins in vistacaWebMar 28, 2011 · The Sticklepath fault runs NW to SE in direction, and is thought to start at near Bideford in the North, running across the NE corner of Dartmoor and through to … farmers ins in kansas city mo