|
Arbuthnott-Garvock Group
The Arbuthnott-Garvock Group (or Arbuthnot-Garvock Group) is a Devonian lithostratigraphic group (a sequence of rock strata) in central Scotland. The name is derived from the village of Arbuthnott in Aberdeenshire and the Hill of Garvock near Laurencekirk. The group comprises the previously separate overlying Garvock Group and the underlying Arbuthnott Group. Outcrops These rocks are exposed in the west in southern Kintyre between Campbeltown and Southend and in an arcuate belt between Machrie and Sannox on the Isle of Arran. They occur in a southwest–northeast trending belt parallel to and just south of the Highland Boundary Fault between Helensburgh and Blairgowrie via Aberfoyle and Callander and as far as the southern edge of Stonehaven on the Scottish east coast. An extensive area in the east between Stonehaven and Dundee is underlain by these rocks including the Brechin, Forfar and Arbroath areas. A further belt of country between Forfar and Dunblane through Perth and exten ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Strathmore Group
The Strathmore Group is a Devonian lithostratigraphic group (a sequence of rock strata) in central Scotland. Its sandstones are interbedded with siltstones which interfinger with conglomerates. It is encountered from Arran in the west across the Midland Valley to Stonehaven in the east. The name is derived from Strathmore, Angus where this sequence occupies the axis of the Strathmore Syncline which runs for many tens of miles parallel to and south of the Highland Boundary Fault The Highland Boundary Fault is a major fault zone that traverses Scotland from Arran and Helensburgh on the west coast to Stonehaven in the east. It separates two different geological terranes which give rise to two distinct physiographic ter .... The rocks of the Strathmore Group have also previously been referred to as the Strathmore Beds. References * {{Refend Devonian System of Europe Geology of Scotland Geological groups of the United Kingdom Geologic formations of the United Kingdom [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Blairgowrie And Rattray
Blairgowrie may refer to: * Blairgowrie, Perth and Kinross, a town in Scotland now part of the burgh of Blairgowrie and Rattray * Blairgowrie, Victoria, Australia * Blairgowrie, Gauteng, South Africa {{Geodis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Helensburgh
Helensburgh (; gd, Baile Eilidh) is an affluent coastal town on the north side of the Firth of Clyde in Scotland, situated at the mouth of the Gareloch. Historically in Dunbartonshire, it became part of Argyll and Bute following local government reorganisation in 1996. Geography and geology Helensburgh is northwest of Glasgow. The town faces south towards Greenock across the Firth of Clyde, which is approximately wide at this point. Ocean-going ships can call at Greenock, but the shore at Helensburgh is very shallow, although to the west of the town the Gareloch is deep. Helensburgh lies at the western mainland end of the Highland Boundary Fault. This means that the hills to the north of Helensburgh lie in the Highlands, whereas the land to the south of Helensburgh is in the Lowlands or Central Belt of Scotland. Consequently, there is a wide variety of landscape in the surrounding area – for example, Loch Lomond (part of Scotland's first National Park) is only over ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Isle Of Arran
The Isle of Arran (; sco, Isle o Arran; gd, Eilean Arainn) or simply Arran is an island off the west coast of Scotland. It is the largest island in the Firth of Clyde and the seventh-largest Scottish island, at . Historically part of Buteshire, it is in the unitary council area of North Ayrshire. In the 2011 census it had a resident population of 4,629. Though culturally and physically similar to the Hebrides, it is separated from them by the Kintyre peninsula. Often referred to as "Scotland in Miniature", the island is divided into highland and lowland areas by the Highland Boundary Fault and has been described as a "geologist's paradise".Haswell-Smith (2004) pp. 11–17. Arran has been continuously inhabited since the early Neolithic period. Numerous prehistoric remains have been found. From the 6th century onwards, Goidelic-speaking peoples from Ireland colonised it and it became a centre of religious activity. In the troubled Viking Age, Arran became the property of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sannox
Sannox ( gd, Sannaig) is a village on the Isle of Arran, Scotland. The village is within the parish of Kilbride. The name comes from the name the Vikings gave to the area, ''Sandvik'', meaning the Sandy Bay. History Within North Glen Sannox it is possible to find an Iron Age fort and the remains of a village, abandoned in 1829 as part of the process of the Highland clearances. Most of the inhabitants of this village emigrated to Canada where they built a replica of the church that was constructed in Sannox in 1822. The replica church in Inverness, Quebec, is no longer there (since the 1950s) and only the cemetery remains. Remains of the houses and runrigs - a type of farming common in western Scotland at the time - are visible throughout North Glen Sannox. Mining was a source of employment in the area, when in 1840 a mine was opened in Glen Sannox. However operations only lasted around two decades. Operations ended when in 1862 the 11th Duke of Hamilton closed the mine, claimin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Machrie
Machrie ( gd, Am Machaire) is a village on the Isle of Arran in the Firth of Clyde, Scotland. Machrie Bay can be found on the West Coast. The village is within the parish of Kilmory. It is most well known for its Standing Stones that are a local tourist attraction, along with the King's Cave which was believed to have been used by Robert the Bruce Robert I (11 July 1274 – 7 June 1329), popularly known as Robert the Bruce (Scottish Gaelic: ''Raibeart an Bruis''), was King of Scots from 1306 to his death in 1329. One of the most renowned warriors of his generation, Robert eventuall .... Machrie Moor Machrie Moor is the site of a number of neolithic structures dating back up to 4500 years ago. These include the six Machrie Moor Stone Circles, and Moss Farm Road Stone Circle. The standing stones were dated back to approximately 2500 years ago but excavations in the 1980s uncovered elaborate timber structures and stone circles which dated back even further in histor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Southend, Argyll And Bute
Southend (, ) is the main settlement at the southern end of the Kintyre peninsula in Argyll and Bute, Scotland. It lies south of Campbeltown, the main town in the area. The civil parish of Southend comprises the village and the surrounding land, used mainly for farming and forestry. The population of the parish is 497. History The village is located beside Dunaverty Bay, which at one end has a rocky promontory called ''Dunaverty Rock'', where Dunaverty Castle was located. Historically the local inhabitants may be first mentioned by Ptolemy as the Epidii (horse people), whose main town may have been named later in the Ravenna Cosmography as Rauatonium. During the early medieval period Dunaverty became the location where Saint Columba first set foot in Scotland. Above the cemetery at Keil are two carved human footprints ( Petrosomatoglyphs) similar to that seen at Dunadd, now called ''Columba's Footprints''. Here it is claimed Columba first preached on Scottish soil, after ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Campbeltown
Campbeltown (; gd, Ceann Loch Chille Chiarain or ) is a town and former royal burgh in Argyll and Bute, Scotland. It lies by Campbeltown Loch on the Kintyre peninsula. Campbeltown became an important centre for Scotch whisky, and a busy fishing port. The 2018 population estimate was 4,600 indicating a reduction since the 2011 census. History Originally known as Kinlochkilkerran (an anglicization of the Gaelic, which means 'head of the loch by the kirk of Ciarán'), Campbeltown was renamed in the 17th century as ''Campbell's Town'' after Archibald Campbell (Earl of Argyle) was granted the site in 1667. Campbeltown Town Hall was completed in 1760. Whisky Campbeltown is one of five areas in Scotland categorised as a distinct malt whisky producing region, and is home to the Campbeltown single malts. At one point it had over 30 distilleries and proclaimed itself "the whisky capital of the world". However, a focus on quantity rather than quality, and the combination of Proh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rock Strata
In geology and related fields, a stratum ( : strata) is a layer of rock or sediment characterized by certain lithologic properties or attributes that distinguish it from adjacent layers from which it is separated by visible surfaces known as either '' bedding surfaces'' or ''bedding planes''.Salvador, A. ed., 1994. ''International stratigraphic guide: a guide to stratigraphic classification, terminology, and procedure. 2nd ed.'' Boulder, Colorado, The Geological Society of America, Inc., 215 pp. . Prior to the publication of the International Stratigraphic Guide, older publications have defined a stratum as either being either equivalent to a single bed or composed of a number of beds; as a layer greater than 1 cm in thickness and constituting a part of a bed; or a general term that includes both ''bed'' and '' lamina''.Neuendorf, K.K.E., Mehl, Jr., J.P., and Jackson, J.A. , eds., 2005. ''Glossary of Geology'' 5th ed. Alexandria, Virginia, American Geological Institute. 779 pp. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lithostratigraphy
Lithostratigraphy is a sub-discipline of stratigraphy, the geological science associated with the study of strata or rock layers. Major focuses include geochronology, comparative geology, and petrology. In general, strata are primarily igneous or sedimentary relating to how the rock was formed. Sedimentary layers are laid down by deposition of sediment associated with weathering processes, decaying organic matter (biogenic) or through chemical precipitation. These layers are often distinguishable as having many fossils and are important for the study of biostratigraphy. Igneous layers occur as stacks of lava flows, layers of lava fragments (called tephra) both erupted onto the Earth's surface by volcanoes, and in layered intrusions formed deep underground. Igneous layers are generally devoid of fossils and represent magmatic or volcanic activity that occurred during the geologic history of an area. There are a number of principles that are used to explain the appear ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
%2C_Helensburgh.jpg "Click for more on -> Helensburgh")
.jpg "Click for more on -> Campbeltown")
