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Bowmore Sandstone Group
The Bowmore Sandstone Group is a sequence of metasedimentary rocks, dominantly sandstones, of probable Neoproterozoic age. Their outcrop on the island of Islay in the Inner Hebrides The Inner Hebrides (; Scottish Gaelic: ''Na h-Eileanan a-staigh'', "the inner isles") is an archipelago off the west coast of mainland Scotland, to the south east of the Outer Hebrides. Together these two island chains form the Hebrides, whic ... is entirely fault-bounded, between the Loch Gruinart Fault to the west and the Loch Skerrols Shear Zone to the east. References {{Islay Geology of Scotland Islay ...
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Bowmore
Bowmore ( gd, Bogh Mòr, 'Big Bend') is a small town on the Scottish island of Islay. It serves as administrative capital of the island, and gives its name to the noted Bowmore distillery producing Bowmore single malt scotch whisky. History Bowmore is a planned village with wide streets on a grid-iron pattern. It has its origins in an earlier settlement, Kilarrow, which until c. 1770 occupied the site of the present grounds of Islay House near Bridgend.The ruined monastery of Kilarrow on Islay
British Library
In May 1685, Kilarrow was the scene of the first stages of , when rebels under the

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Group (stratigraphy)
In geology, a group is a lithostratigraphic unit consisting of a series of related formations that have been classified together to form a group. Formations are the fundamental unit of stratigraphy. Groups may sometimes be combined into supergroups. Groups are useful for showing relationships between formations, and they are also useful for small-scale mapping or for studying the stratigraphy of large regions. Geologists exploring a new area have sometimes defined groups when they believe the strata within the groups can be divided into formations during subsequent investigations of the area. It is possible for only some of the strata making up a group to be divided into formations. An example of a group is the Glen Canyon Group, which includes (in ascending order) the Wingate Sandstone, the Moenave Formation, the Kayenta Formation, and the Navajo Sandstone. Each of the formations can be distinguished from its neighbor by its lithology, but all were deposited in the sam ...
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Neoproterozoic
The Neoproterozoic Era is the unit of geologic time from 1 billion to 538.8 million years ago. It is the last era of the Precambrian Supereon and the Proterozoic Eon; it is subdivided into the Tonian, Cryogenian, and Ediacaran periods. It is preceded by the Mesoproterozoic Era and succeeded by the Paleozoic Era of the Phanerozoic Eon. The most severe glaciation known in the geologic record occurred during the Cryogenian, when ice sheets may have reached the equator and formed a " Snowball Earth". The earliest fossils of complex multicellular life are found in the Ediacaran Period. These organisms make up the Ediacaran biota, including the oldest definitive animals in the fossil record. According to Rino and co-workers, the sum of the continental crust formed in the Pan-African orogeny and the Grenville orogeny makes the Neoproterozoic the period of Earth's history that has produced most continental crust. Geology At the onset of the Neoproterozoic the supercon ...
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Inner Hebrides
The Inner Hebrides (; Scottish Gaelic: ''Na h-Eileanan a-staigh'', "the inner isles") is an archipelago off the west coast of mainland Scotland, to the south east of the Outer Hebrides. Together these two island chains form the Hebrides, which experience a mild oceanic climate. The Inner Hebrides comprise 35 inhabited islands as well as 44 uninhabited islands with an area greater than . Skye, Mull, and Islay are the three largest, and also have the highest populations. The main commercial activities are tourism, crofting, fishing and whisky distilling. In modern times the Inner Hebrides have formed part of two separate local government jurisdictions, one to the north and the other to the south. Together, the islands have an area of about , and had a population of 18,948 in 2011. The population density is therefore about . There are various important prehistoric structures, many of which pre-date the first written references to the islands by Roman and Greek authors. In t ...
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Laggan Formation
Laggan (''Lagan'', Gaelic for 'little hollow') is the name of numerous places in Scotland, including: *Laggan, Badenoch *Laggan, Great Glen * Laggan, Islay *Laggan Dam on the River Spean south west of Loch Laggan *Kinloch Laggan, hamlet at the north end of Loch Laggan *Loch Laggan, Highland *River Laggan, Islay and outwith Scotland: *Laggan, New South Wales, Australia * Laggan, County Donegal, Ireland, see Porthall and also: See also *Lagan (other) Lagan may refer to: Entertainment * ''Lagan'' (1941 film), Indian Bollywood film * Lagan (1955 film), a Bollywood film *''Lagan'' (1971 film), Bollywood film * ''Lagaan'', 2001 Indian epic sports-drama film * "Lagan", a song by the Afro Celt So ...
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Blackrock Formation
BlackRock, Inc. is an American multi-national investment company based in New York City. Founded in 1988, initially as a risk management and fixed income institutional asset manager, BlackRock is the world's largest asset manager, with trillion in assets under management as of January 2022. BlackRock operates globally with 70 offices in 30 countries, and clients in 100 countries. Along with Vanguard and State Street, BlackRock is considered to be one of the Big Three index fund managers that dominate corporate America. BlackRock has sought to position itself as an industry leader in environmental, social and corporate governance (ESG). The company has faced criticism for worsening climate change, its close ties with the Federal Reserve System during the COVID-19 pandemic, anticompetitive behavior, and its unprecedented investments in China. History 1988–1997 BlackRock was founded in 1988 by Larry Fink, Robert S. Kapito, Susan Wagner, Barbara Novick, Ben Golub, Hugh F ...
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Islay Geology
Islay ( ; gd, Ìle, sco, Ila) is the southernmost island of the Inner Hebrides of Scotland. Known as "The Queen of the Hebrides", it lies in Argyll just south west of Jura and around north of the Northern Irish coast. The island's capital is Bowmore where the distinctive round Kilarrow Parish Church and a distillery are located. Port Ellen is the main port. Islay is the fifth-largest Scottish island and the eighth-largest island of the British Isles, with a total area of almost . There is ample evidence of the prehistoric settlement of Islay and the first written reference may have come in the first century AD. The island had become part of the Gaelic Kingdom of Dál Riata during the Early Middle Ages before being absorbed into the Norse Kingdom of the Isles. The later medieval period marked a "cultural high point" with the transfer of the Hebrides to the Kingdom of Scotland and the emergence of the Clan Donald Lordship of the Isles, originally centred at Finlaggan. Durin ...
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Metasediment
In geology, metasedimentary rock is a type of metamorphic rock. Such a rock was first formed through the deposition and solidification of sediment Sediment is a naturally occurring material that is broken down by processes of weathering and erosion, and is subsequently transported by the action of wind, water, or ice or by the force of gravity acting on the particles. For example, sa .... Then, the rock was buried underneath subsequent rock and was subjected to high pressures and temperatures, causing the rock to recrystallize. The overall composition of a metasedimentary rock can be used to identify the original sedimentary rock, even where they have been subject to high-grade metamorphism and intense deformation. Types of metasedimentary rocks See also * References Metamorphic petrology {{petrology-stub ...
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Islay
Islay ( ; gd, Ìle, sco, Ila) is the southernmost island of the Inner Hebrides of Scotland. Known as "The Queen of the Hebrides", it lies in Argyll just south west of Jura and around north of the Northern Irish coast. The island's capital is Bowmore where the distinctive round Kilarrow Parish Church and a distillery are located. Port Ellen is the main port. Islay is the fifth-largest Scottish island and the eighth-largest island of the British Isles, with a total area of almost . There is ample evidence of the prehistoric settlement of Islay and the first written reference may have come in the first century AD. The island had become part of the Gaelic Kingdom of Dál Riata during the Early Middle Ages before being absorbed into the Norse Kingdom of the Isles. The later medieval period marked a "cultural high point" with the transfer of the Hebrides to the Kingdom of Scotland and the emergence of the Clan Donald Lordship of the Isles, originally centred at Finlagg ...
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Fault (geology)
In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust result from the action of plate tectonic forces, with the largest forming the boundaries between the plates, such as the megathrust faults of subduction zones or transform faults. Energy release associated with rapid movement on active faults is the cause of most earthquakes. Faults may also displace slowly, by aseismic creep. A ''fault plane'' is the plane that represents the fracture surface of a fault. A '' fault trace'' or ''fault line'' is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geologic maps to represent a fault. A ''fault zone'' is a cluster of parallel faults. However, the term is also used for the zone of crushed rock along a single fault. Prolonged motion along closely spaced faults can bl ...
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Geology Of Scotland
The geology of Scotland is unusually varied for a country of its size, with a large number of differing geological features.Keay & Keay (1994) page 415. There are three main geographical sub-divisions: the Highlands and Islands is a diverse area which lies to the north and west of the Highland Boundary Fault; the Central Lowlands is a rift valley mainly comprising Palaeozoic formations; and the Southern Uplands, which lie south of the Southern Uplands Fault, are largely composed of Silurian deposits. The existing bedrock includes very ancient Archean gneiss, metamorphic beds interspersed with granite intrusions created during the Caledonian mountain building period (the Caledonian orogeny), commercially important coal, oil and iron bearing carboniferous deposits and the remains of substantial Palaeogene volcanoes. During their formation, tectonic movements created climatic conditions ranging from polar to desert to tropical and a resultant diversity of fossil remains. Scotla ...
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