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This is a list of all airline codes. The table lists the IATA airline designators , the ICAO airline designators and the airline call signs (telephony designator). Historical assignments are also included for completeness.
Allen, J R L, Thomas, R L, and Williams, B P J. 1982. The Old Red Sandstone north of Milford Haven. 123–149 in Geological excursions in Dyfed, south-west Wales. BASSETT, M G (editor). (Cardiff: Published for the Geologists’ Association by the National Museum of Wales.) (Allen et al 1982)
The Carreg Cennen Disturbance is a zone of geological faults and folds in south and mid Wales which forms a part of both the Church Stretton Fault Zone and the Welsh Borderland Fault System. To the southwest it is known as the 'Llandyfaelog Disturbance'.
Southwest built a 5-gate international terminal at William P. Hobby Airport that opened in 2015. Southwest also built a 5-gate international terminal in Fort Lauderdale that opened in 2017. [9] In 2021, a 5-gate extension of terminal A at Baltimore/Washington International Airport opened. Southwest is the sole occupant of Terminal A and it ...
It lies on the northeast-southwest aligned geological structure known as the Cribarth Disturbance and indeed gives its name to that regionally important structure. The Disturbance is characterised locally by a tight anticline which follows the alignment of the summit ridge and which is accompanied by one or two lesser folds on its northwestern ...
Chevron folds with flat-lying axial planes, Millook Haven, North Cornwall, UK. Chevron folds are a structural feature characterized by repeated well behaved folded beds with straight limbs and sharp hinges. Well developed, these folds develop repeated set of v-shaped beds. [1] They develop in response to regional or local compressive stress.
Topographic map showing detachment folds in the eastern Sichuan Basin, China.. A detachment fold, in geology, occurs as layer parallel thrusting along a decollement (or detachment) develops without upward propagation of a fault; the accommodation of the strain produced by continued displacement along the underlying thrust results in the folding of the overlying rock units.
Smith et al. 2005 Structure & Evolution of the south-west Pennine Basin and adjacent area. Subsurface memoir of the British Geological Survey. (Smith et al. 2005) Toghill, P. 2006 Geology of Shropshire (2nd edn) Crowood Press, Wilts (Toghill P 2006) Webby, B.D. 1965 Proceedings of the Geologists' Association volume 76, part 1 (Webby, B.D. 1965)