1957
DOI: 10.2307/2256962
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The Ecology of the Lough Ine Rapids with Special Reference to Water Currents: VI. Effects of the Rapids on the Hydrography of the South Basin

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Cited by 53 publications
(39 citation statements)
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“…The Rapids population (R) had a more similar genetic structure to the populations within Lough Hyne, although there was some evidence of gene flow with Irish coastal populations. The tidal flow regime during inflow probably explains why the Rapids site exchanged more genetic material with Lough Hyne sites than between Lough Hyne sites (some of the water moves towards L1 and L2, whereas no direct water flow occurs between L1 and L2; Bassindale et al 1957).…”
Section: Discussion (A) Marine Reserves Connectivity and Isolationmentioning
confidence: 99%
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“…The Rapids population (R) had a more similar genetic structure to the populations within Lough Hyne, although there was some evidence of gene flow with Irish coastal populations. The tidal flow regime during inflow probably explains why the Rapids site exchanged more genetic material with Lough Hyne sites than between Lough Hyne sites (some of the water moves towards L1 and L2, whereas no direct water flow occurs between L1 and L2; Bassindale et al 1957).…”
Section: Discussion (A) Marine Reserves Connectivity and Isolationmentioning
confidence: 99%
“…) in eastern parts of the lough, decrease westwards across the lough and are negligible in the north basin (Bassindale et al 1957). Outflow of water lasts approximately 8 h, with very slight water currents (as water is skimmed from the surface in the vicinity of the rapids) in all parts of the lough, with the exception of the Rapids.…”
Section: K1mentioning
confidence: 99%
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“…The lough is connected to the open sea via a shallow narrow channel (The Rapids) in which tidal currents achieve a maximum velocity of approximately 2 m S-' (Bassindale et al 1957). This study was conducted to the floor of the lough, at the base of a shell-gravel ramp l e a d n g down from The Rapids, at a depth of approximately 19 m. The sediment in this area has a median particle size of 1.68 mm and is composed of approximately 50% gravel, 35 % sand and 8 % silt-clay.…”
Section: Methodsmentioning
confidence: 99%
“…Whirlpool Cliff is subjected to unidirectional flow, with current speeds reaching \ 100 cm s − 1 at peak inflow (Maughan and Barnes, 2000), whilst Glannafeen experiences moderate water currents (: 35 cm s − 1 ) resulting in considerable sedimentation. Goleen, Labhra Cliff and West Cliff are essentially very similar sites, with current velocities rarely reaching 5 cm s − 1 (Bassindale et al, 1957). Bullock Island, which is the site on the adjacent Atlantic coast, experiences severe wave action especially during winter storms.…”
Section: Study Sitementioning
confidence: 99%