Question: What is the name of the peak in County Kerry of the country in the Eurasian plate?

<P0-S0> :Ireland is an island in Northwestern Europe in the north Atlantic Ocean. <P0-S1>  The island lies on the European continental shelf, part of the Eurasian Plate. <P0-S2>  The island's main geographical features include low central plains surrounded by coastal mountains. <P0-S3>  The highest peak is Carrauntoohil (Irish: "Corrán Tuathail" ), which is 1041 meters above sea level. <P0-S4>  The western coastline is rugged, with many islands, peninsulas, headlands and bays. <P0-S5>  The island is bisected by the River Shannon, which at 360.5 km with a 102.1 km estuary is the longest river in Ireland and flows south from County Cavan in Ulster to meet the Atlantic just south of Limerick. <P0-S6>  There are a number of sizeable lakes along Ireland's rivers, of which Lough Neagh is the largest. <SEP> <P1-S0> Carrauntoohil ( ,Irish: Corrán Tuathail ) is the highest peak on the island of Ireland. <P1-S1>  Located in County Kerry, it is 1038 m high and is the central peak of the Macgillycuddy's Reeks range. <P1-S2>  The ridge northward leads to Ireland's second-highest peak, Beenkeragh (1,010 m), while the ridge westward leads to the third-highest peak, Caher (1,001 m). <P1-S3>  Carrauntoohil overlooks three bowl-shaped valleys, each with its own lakes. <P1-S4>  To the east is Hag's Glen or Coomcallee ("Com Caillí", "hollow of the Cailleach"), to the west is Coomloughra ("Com Luachra", "hollow of the rushes") and to the south is Curragh More ("Currach Mór", "great marsh"). <SEP> <P2-S0> The Adriatic/Apulian Plate is thought to still move independently of the Eurasian Plate in NNE direction with a small component of counter-clockwise rotation. <P2-S1>  The fault zone that separates the two is the Periadriatic Seam that runs through the Alps. <P2-S2>  Studies indicate that in addition to deforming, the Eurasian continental crust has actually subducted to some extent below the Adriatic/Apulian Plate, an unusual circumstance in plate tectonics. <P2-S3>  Oceanic crust of the African Plate is also subducting under the Adriatic/Apulian Plate off the western and southern coasts of the Italian Peninsula, creating a berm of assorted debris which rises from the seafloor and continues onshore. <P2-S4>  This subduction is also responsible for the volcanics of southern Italy. <SEP> <P3-S0> The geological deformation of Iceland is the way that the rocks of the island of Iceland are changing due to tectonic forces. <P3-S1>  The geological deformation explains the location of earthquakes, volcanoes, fissures, and the shape of the island. <P3-S2>  Iceland is the largest landmass (102,775 km²) situated on an oceanic ridge. <P3-S3>  It is an elevated plateau of the sea floor, situated at the crossing of the Mid-Atlantic Ridge and the Greenland-Iceland-Faeroe Ridge. <P3-S4>  It lies along the oceanic divergent plate boundary of North American Plate and Eurasian Plate. <P3-S5>  The western part of Iceland sits on the North American Plate and the eastern part sits on the Eurasian Plate. <P3-S6>  The Reykjanes Ridge of the Mid-Atlantic ridge system in this region crosses the island from southwest and connects to the Kolbeinsey Ridge in the northeast.