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![]() ![]() The work was edited by Ní Chinnéide and appeared under the title Peig. Her son Mícheál returned to live with her on the island when his health failed.Įncouraged by two visitors to the island, Máire Ní Chinnéide and Léan Ní Chonnalláin, to record her life story, she dictated it to her son Mícheál as she could neither read nor write Irish. When her surviving children emigrated permanently to America she decided to live with her blind brother-in-law Mícheál, who had helped the family after the death of her husband. Her husband, who had suffered ill health for a long period, died shortly afterwards. ![]() Three died in infancy, her daughter Siobhán died of the measles at the age of eight, and her son Tomás was killed in 1920 when he fell off a cliff while gathering heather. Life on the island was harsh, and of her ten children only five survived. A different version appears in another account of her life, Beatha Pheig Sayers (1970), written by her son Mícheál Ó Gaoithín (qv) (‘Maidhc file’), which stated that Peig had seen her future husband beforehand and had fallen in love with him. Her marriage was arranged, and (according to her account in Peig) she had never set eyes on her future husband until the night the match was made. She married (13 February 1892) Pádraig Ó Gaoithín (Peatsaí Flint), twelve years her senior, from the Great Blasket Island and was to spend the next fifty years on the island. She was deeply unhappy with her second mistress and finally returned home to her parents. Her elder siblings had emigrated to the USA and she also had hoped to follow them when the fare for her passage was sent to her by her friend Cáit Jim, but when it did not arrive she was forced to enter service for a second time. At the age of fourteen she entered domestic service in Dingle, where she remained for four years until her health failed. At the age of six she attended the local national school in Dunquin, where she was taught by Seán Ó Dálaigh, receiving her education through the medium of English. She learned many of her tales from her father, who had recounted a substantial number to Jeremiah Curtin (qv). Kerry, six months before she was born, as nine of their children had died there and her mother had hoped that the change would bring the family luck. Her parents had moved to Vicarstown from Ventry, Co. Of English protestant descent on her father's side, the family had converted to catholicism during her grandfather's generation. She was baptised 29 March 1873 in Ballyferriter, Co. Kerry, one of thirteen children of Tomás Sayers, storyteller and small farmer, and his wife Peig (née Ní Bhrosnacháin). 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We performed three-dimensional thermal modelling that suggests the anomaly is probably due to extensive serpentinization down to ~16 km, overlying a hydrated, shear mylonite zone down to 32 km. Here we present ultra-long offset seismic data from the Romanche transform fault in the equatorial Atlantic Ocean that indicates the presence of a low-velocity anomaly extending to ~60 km below sea level. However, the deep structure of these faults remains enigmatic. Away from active transform boundaries, former oceanic transform faults also form the fracture zones that cover the ocean floor. Seismic studies of earthquakes from transform faults soon revealed that the motion was opposite, as predicted.Transform faults accommodate the lateral motions between lithospheric plates, producing large earthquakes. This is clear when it is realized that the plate boundaries are confined to the spreading centres and transform faults, not to the inactive part of the fracture zone. For example, if a ridge crest was offset to the left by a transform fault, implying leftward movement on a fault joining the offset crests, the movement across the transform fault was instead to the right. Morgan’s theory made a very dramatic prediction: namely, that the direction of motion on the transform faults was opposite to the offsets of the ridge crests. Tuzo Wilson recognized the seismic nature of transform faults and other features and explained the phenomenon as a transfer of motion from one spreading centre to another. About the same time Morgan was forming his theory, the Canadian geologist and geophysicist J. The inactive portions of the fracture zone on the ridge flanks are scars on the ocean floor created in the transform faults. ![]() Morgan proposed that opposing plates along an oceanic ridge crest offset by fracture zones are divided by the spreading centres and transform faults. Jason Morgan, one of the several outstanding pioneers in plate tectonics, recognized that transform faults are zones where opposing lithospheric plates slip past one another. Transform faults are the only segments of fracture zones that are seismically active. The spatial orientation of transform faults is typically parallel to plate motions however, this is not always the case. A transform fault may occur in the portion of a fracture zone that exists between different offset spreading centres or that connects spreading centres to deep-sea trenches in subduction zones. Transform fault, in geology and oceanography, a type of fault in which two tectonic plates slide past one another. SpaceNext50 Britannica presents SpaceNext50, From the race to the Moon to space stewardship, we explore a wide range of subjects that feed our curiosity about space!.Learn about the major environmental problems facing our planet and what can be done about them! 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