What is the name of the peak in County Kerry of the country in the Eurasian plate?
Carrauntoohil
Carrauntoohil
Carrauntoohil ( ,Irish: Corrán Tuathail ) is the highest peak on the island of Ireland.
 Located in County Kerry, it is 1038 m high and is the central peak of the Macgillycuddy's Reeks range.
 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).
 Carrauntoohil overlooks three bowl-shaped valleys, each with its own lakes.
 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").
Geography of Ireland
:Ireland is an island in Northwestern Europe in the north Atlantic Ocean.
 The island lies on the European continental shelf, part of the Eurasian Plate.
 The island's main geographical features include low central plains surrounded by coastal mountains.
 The highest peak is Carrauntoohil (Irish: "Corrán Tuathail" ), which is 1041 meters above sea level.
 The western coastline is rugged, with many islands, peninsulas, headlands and bays.
 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.
 There are a number of sizeable lakes along Ireland's rivers, of which Lough Neagh is the largest.
Okhotsk Plate
The Okhotsk Plate is a minor tectonic plate covering the Sea of Okhotsk, the Kamchatka Peninsula, Sakhalin Island and Tōhoku and Hokkaidō in Japan.
 It was formerly considered a part of the North American Plate, but recent studies indicate that it is an independent plate, bounded on the north by the North American Plate.
 The boundary is a left-lateral moving transform fault, the Ulakhan Fault.
 On the east, the plate is bounded by the Pacific Plate at the Kuril-Kamchatka Trench and the Japan Trench, on the south by the Philippine Sea Plate at the Nankai Trough, on the west by the Eurasian Plate, and possibly on the southwest by the Amurian Plate. Sorong Fault
Sorong fault also (Sorong Fault Zone, SFZ) is an active, broad zone of inferred left lateral shear at the triple junction of the Australian plate, Eurasian plate, and Pacific plates, where many plate fragments exist, such as the Philippine Sea Plate, Bird's Head Plate, Halmahera Plate and the Molucca Sea Plate.
 It has been implicated in numerous large earthquakes.
 It is one of the two major faults created by the Australian and Pacific plate convergence, the other being the Ramu-Markham Fault zone. Jan Mayen Microcontinent
The Jan Mayen Microcontinent is a fragment of continental crust within the oceanic part of the western Eurasian Plate lying northeast of Iceland.
 At the onset of separation between the Greenland and Eurasian plates 55 million years ago, it formed part of the eastern margin of the Greenland Plate.
 Propagation of a new spreading center from the Reykjanes Ridge separated this microcontinent from the Greenland Plate.
 For a short period it formed a microplate, until the Aegir Ridge became inactive, after which it formed part of the Eurasian Plate.
 The island of Jan Mayen is a much younger feature, formed of volcanic rock, built up at the northernmost tip of the microcontinent. Geological deformation of Iceland
The geological deformation of Iceland is the way that the rocks of the island of Iceland are changing due to tectonic forces.
 The geological deformation explains the location of earthquakes, volcanoes, fissures, and the shape of the island.
 Iceland is the largest landmass (102,775 km²) situated on an oceanic ridge.
 It is an elevated plateau of the sea floor, situated at the crossing of the Mid-Atlantic Ridge and the Greenland-Iceland-Faeroe Ridge.
 It lies along the oceanic divergent plate boundary of North American Plate and Eurasian Plate.
 The western part of Iceland sits on the North American Plate and the eastern part sits on the Eurasian Plate.
 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. Sunda Trench
The Sunda Trench, earlier known as, and sometimes still indicated as the Java Trench, is located near Sumatra, formed where the Australian Plate subducts under a part of the Eurasian Plate.
 With a length of 3200 km .
 The maximum depth of 7725 m (at 10°19'S, 109°58'E, about 320 km south of Yogyakarta), is the deepest point in the Indian Ocean.
 The trench stretches from the Lesser Sunda Islands past Java, around the southern coast of Sumatra on to the Andaman Islands, and forms the boundary between Indo-Australian Plate and Eurasian plate (more specifically, Sunda Plate).
 The trench is considered to be part of the Pacific Ring of Fire as well as one of a ring of oceanic trenches around the northern edges of the Australian Plate. Chaman Fault
The Chaman Fault is a major, active geological fault in Pakistan and Afghanistan that runs for over 850 km.
 Tectonically, it is actually a system of related geologic faults that separates the Eurasian Plate from the Indo-Australian Plate.
 It is a terrestrial, primarily transform, left-lateral strike-slip fault.
 The slippage rate along the Chaman fault system as the Indo-Australian Plate moves northward (relative to the Eurasian Plate) has been estimated at 10 mm/yr or more.
 In addition to its primary transform aspect, the Chaman fault system has a compressional component as the Indian Plate is colliding with the Eurasian Plate.
 This type of plate boundary is sometimes called a transpressional boundary. Adriatic Plate
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.
 The fault zone that separates the two is the Periadriatic Seam that runs through the Alps.
 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.
 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.
 This subduction is also responsible for the volcanics of southern Italy. Amurian Plate
The Amurian Plate (or Amur Plate; also occasionally referred to as the China Plate) is a minor tectonic plate in the northern and eastern hemispheres.
 It covers Manchuria, the Korean Peninsula, Western Japan, and Primorsky Krai.
 Once thought to be a part of the Eurasian Plate, the Amur Plate is now generally considered to be a separate plate moving southeast with respect to the Eurasian Plate.