107-412: Gutland can mean: Gotland , the largest island and a province of Sweden Gutland (Luxembourg) , a region of southern Luxembourg Gutland (film) , a 2017 film Topics referred to by the same term [REDACTED] This disambiguation page lists articles associated with the title Gutland . If an internal link led you here, you may wish to change
214-455: A Mohs hardness of 2 to 4, dense limestone can have a crushing strength of up to 180 MPa . For comparison, concrete typically has a crushing strength of about 40 MPa. Although limestones show little variability in mineral composition, they show great diversity in texture. However, most limestone consists of sand-sized grains in a carbonate mud matrix. Because limestones are often of biological origin and are usually composed of sediment that
321-463: A bloom of cyanobacteria or microalgae . However, stable isotope ratios in modern carbonate mud appear to be inconsistent with either of these mechanisms, and abrasion of carbonate grains in high-energy environments has been put forward as a third possibility. Formation of limestone has likely been dominated by biological processes throughout the Phanerozoic , the last 540 million years of
428-589: A marine climate ( Cfb ). This results in larger seasonal differences than typical of marine climates in spite of it being surrounded by the Baltic Sea for large distances in all directions. This is due to strong continental winds travelling over the sea from surrounding great landmasses. Seasonal temperature variation is smaller in more isolated places on the island such as Hoburgen or Östergarnsholm, having warmer autumn and winter, but are cooler during spring and summer days. Seasonal lag being exceptionally strong in
535-434: A carbonate rock outcrop can be estimated in the field by etching the surface with dilute hydrochloric acid. This etches away the calcite and aragonite, leaving behind any silica or dolomite grains. The latter can be identified by their rhombohedral shape. Crystals of calcite, quartz , dolomite or barite may line small cavities ( vugs ) in the rock. Vugs are a form of secondary porosity, formed in existing limestone by
642-616: A central quartz grain or carbonate mineral fragment. These likely form by direct precipitation of calcium carbonate onto the ooid. Pisoliths are similar to ooids, but they are larger than 2 mm in diameter and tend to be more irregular in shape. Limestone composed mostly of ooids is called an oolite or sometimes an oolitic limestone . Ooids form in high-energy environments, such as the Bahama platform, and oolites typically show crossbedding and other features associated with deposition in strong currents. Oncoliths resemble ooids but show
749-449: A change in environment that increases the solubility of calcite. Dense, massive limestone is sometimes described as "marble". For example, the famous Portoro "marble" of Italy is actually a dense black limestone. True marble is produced by recrystallization of limestone during regional metamorphism that accompanies the mountain building process ( orogeny ). It is distinguished from dense limestone by its coarse crystalline texture and
856-949: A composition reflecting the organisms that produced them and the environment in which they were produced. Low-magnesium calcite skeletal grains are typical of articulate brachiopods , planktonic (free-floating) foraminifera, and coccoliths . High-magnesium calcite skeletal grains are typical of benthic (bottom-dwelling) foraminifera, echinoderms , and coralline algae . Aragonite skeletal grains are typical of molluscs , calcareous green algae , stromatoporoids , corals , and tube worms . The skeletal grains also reflect specific geological periods and environments. For example, coral grains are more common in high-energy environments (characterized by strong currents and turbulence) while bryozoan grains are more common in low-energy environments (characterized by quiet water). Ooids (sometimes called ooliths) are sand-sized grains (less than 2mm in diameter) consisting of one or more layers of calcite or aragonite around
963-412: A considerable fraction of the limestone bed. At depths greater than 1 km (0.62 miles), burial cementation completes the lithification process. Burial cementation does not produce stylolites. When overlying beds are eroded, bringing limestone closer to the surface, the final stage of diagenesis takes place. This produces secondary porosity as some of the cement is dissolved by rainwater infiltrating
1070-483: A drop of dilute hydrochloric acid is dropped on it. Dolomite is also soft but reacts only feebly with dilute hydrochloric acid, and it usually weathers to a characteristic dull yellow-brown color due to the presence of ferrous iron. This is released and oxidized as the dolomite weathers. Impurities (such as clay , sand, organic remains, iron oxide , and other materials) will cause limestones to exhibit different colors, especially with weathered surfaces. The makeup of
1177-553: A farmer from Gökhem parish in Västergötland on the mainland was found to be more closely related to modern-day Mediterraneans. This is consistent with the spread of agricultural peoples from the Middle East at about that time. Gutasaga contains legends of how the island was settled by Þieluar and populated by his descendants. It also tells that a third of the population had to emigrate and settle in southern Europe,
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#17327723529441284-637: A few million years, as this is the most stable form of calcium carbonate. Ancient carbonate formations of the Precambrian and Paleozoic contain abundant dolomite, but limestone dominates the carbonate beds of the Mesozoic and Cenozoic . Modern dolomite is quite rare. There is evidence that, while the modern ocean favors precipitation of aragonite, the oceans of the Paleozoic and middle to late Cenozoic favored precipitation of calcite. This may indicate
1391-455: A few thousand years. As rainwater mixes with groundwater, aragonite and high-magnesium calcite are converted to low-calcium calcite. Cementing of thick carbonate deposits by rainwater may commence even before the retreat of the sea, as rainwater can infiltrate over 100 km (60 miles) into sediments beneath the continental shelf. As carbonate sediments are increasingly deeply buried under younger sediments, chemical and mechanical compaction of
1498-490: A high percentage of the mineral dolomite , CaMg(CO 3 ) 2 . Magnesian limestone is an obsolete and poorly-defined term used variously for dolomite, for limestone containing significant dolomite ( dolomitic limestone ), or for any other limestone containing a significant percentage of magnesium . Most limestone was formed in shallow marine environments, such as continental shelves or platforms , though smaller amounts were formed in many other environments. Much dolomite
1605-435: A limestone sample except in thin section and are less common in ancient limestones, possibly because compaction of carbonate sediments disrupts them. Limeclasts are fragments of existing limestone or partially lithified carbonate sediments. Intraclasts are limeclasts that originate close to where they are deposited in limestone, while extraclasts come from outside the depositional area. Intraclasts include grapestone , which
1712-628: A lot more attention military-wise and has seen a much larger spending on the military. As of 2018, the Gotland Regiment has been re-raised and is the first time since World War II that a new regiment has been established in Sweden. The first modern day tourists came to Gotland during the 19th century and were known as "bathers". Gotland became very popular with socialites at the time through Princess Eugenie who lived in Västerhejde , in
1819-471: A lower Mg/Ca ratio in the ocean water of those times. This magnesium depletion may be a consequence of more rapid sea floor spreading , which removes magnesium from ocean water. The modern ocean and the ocean of the Mesozoic have been described as "aragonite seas". Most limestone was formed in shallow marine environments, such as continental shelves or platforms . Such environments form only about 5% of
1926-525: A lower diversity of organisms and a greater fraction of silica and clay minerals characteristic of marls . The Green River Formation is an example of a prominent freshwater sedimentary formation containing numerous limestone beds. Freshwater limestone is typically micritic. Fossils of charophyte (stonewort), a form of freshwater green algae, are characteristic of these environments, where the charophytes produce and trap carbonates. Limestones may also form in evaporite depositional environments . Calcite
2033-523: A mechanism for dolomitization, with one 2004 review paper describing it bluntly as "a myth". Ordinary seawater is capable of converting calcite to dolomite, if the seawater is regularly flushed through the rock, as by the ebb and flow of tides (tidal pumping). Once dolomitization begins, it proceeds rapidly, so that there is very little carbonate rock containing mixed calcite and dolomite. Carbonate rock tends to be either almost all calcite/aragonite or almost all dolomite. About 20% to 25% of sedimentary rock
2140-703: A military standpoint, it occupies a strategic location at the center of the Baltic Sea . The name of Gotland is closely related to that of the Geats and Goths . The island was the home of the Gutes , and sites such as the Ajvide Settlement show that it has been occupied since prehistory . A DNA study conducted on the 5,000-year-old skeletal remains of three Middle Neolithic seal hunters from Gotland showed that they were related to modern-day Finns , while
2247-531: A naval base in the past, as of 2004 , there are no naval units based on Gotland. The Tofta firing range itself (also known as the Tofta Tank firing range), is a military training ground which is located 8 km (5.0 mi) south of Visby. Another less common name for the range is the Toftasjön firing range. Tracing its origins back to 1898, as of 2008 the range extended over 2,700 acres (11 km ). It
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#17327723529442354-536: A number of these grinding grooves to the Stone Age, from c. 3300 BC to c. 2000 BC , based on astronomical alignments, although his methodology has been heavily criticized. The Medieval town of Visby has been entered as a site of the UNESCO World heritage programme. An impressive feature of Visby is the fortress wall that surrounds the old city, dating from the 13th century. Many of
2461-465: A permanent fixed link to the main island. Residents are depending on an around the clock, free of charge, car ferry for transportation over a strait roughly 1.3 km (0.81 mi) wide, taking about eight minutes. Fårö may get connected to the main island with a bridge in the future, but the project has had plenty of delays related to funding. At the closest point, the two islands are separated by less than 500 metres (1,600 ft), although that
2568-448: A plausible source of mud. Another possibility is direct precipitation from the water. A phenomenon known as whitings occurs in shallow waters, in which white streaks containing dispersed micrite appear on the surface of the water. It is uncertain whether this is freshly precipitated aragonite or simply material stirred up from the bottom, but there is some evidence that whitings are caused by biological precipitation of aragonite as part of
2675-449: A radial rather than layered internal structure, indicating that they were formed by algae in a normal marine environment. Peloids are structureless grains of microcrystalline carbonate likely produced by a variety of processes. Many are thought to be fecal pellets produced by marine organisms. Others may be produced by endolithic (boring) algae or other microorganisms or through breakdown of mollusc shells. They are difficult to see in
2782-540: A ram statant Argent armed Or holding on a cross-staff of the same a banner Gules bordered and with five tails of the third." The county was granted the same coat of arms in 1936. The municipality, created in 1971, uses the same picture, but with other tinctures . Gotland is Sweden's largest island, and it is the largest island fully encompassed by the Baltic Sea (with Denmark's Zealand at the Baltic's edge). With its total area of 3,183.7 km (1,229.2 sq mi)
2889-582: A reserve component of the Swedish Amphibious Corps . Among the residual war reserve stocks reported to be still in storage on Gotland in March 2015, were 14 tanks ( Stridsvagn 122s ) at the Tofta skjutfält (the Tofta firing range), but without any crews or dedicated maintenance personnel assigned to them. Gotland currently has no local air defence capability. Despite its importance as
2996-517: A rich heritage of folklore, including myths about the bysen , Di sma undar jordi , Hoburgsgubben and the Martebo lights . Gotland gives its name to the traditional farmhouse ale Gotlandsdricka , a turbid beer with much in common with Finnish sahti , and related beers from the Baltic states . There are a number of notable people born or living on Gotland, or in other major ways associated with
3103-576: A tradition associated with the migration of the Goths , whose name has the same origin as Gutes , the native name of the people of the island. It later tells that the Gutes voluntarily submitted to the king of Sweden and asserts that the submission was based on mutual agreement, and notes the duties and obligations of the Swedish King and Bishop in relationship to Gotland. According to some historians, it
3210-477: A year. In 2007, the number of passengers exceeded 1.5 million. In 2012, the ferries had 1,590,271 passengers and the airlines 327,255 passengers. Even during the COVID-19 pandemic tourism did not change much as Swedes chose to visit the island instead of travelling abroad. The main port of call on Gotland is Visby. The city is visited by a number of cruise ships every year. About 40 cruise lines frequent
3317-442: Is Lojsta Hed which stands 82 m (269 ft) above sea level. The average height of the island is 29 meters. Settlements besides Visby include: Of these, Hemse is the largest settlement in southern Gotland and along with Roma the two largest inland villages. Burgsvik is the southernmost locality and Fårösund the northernmost. The island of Fårö is permanently settled, but with only a few hundred year-round residents and lacks
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3424-556: Is Sweden's largest island. It is also a province / county (Swedish län), municipality , and diocese . The province includes the islands of Fårö and Gotska Sandön to the north, as well as the Karlsö Islands ( Lilla and Stora ) to the west. The population is 61,023 (2024) of which about 23,600 live in Visby , the main town. Outside Visby, there are minor settlements and a mainly rural population. The island of Gotland and
3531-560: Is also favored on the seaward margin of shelves and platforms, where there is upwelling deep ocean water rich in nutrients that increase organic productivity. Reefs are common here, but when lacking, ooid shoals are found instead. Finer sediments are deposited close to shore. The lack of deep sea limestones is due in part to rapid subduction of oceanic crust, but is more a result of dissolution of calcium carbonate at depth. The solubility of calcium carbonate increases with pressure and even more with higher concentrations of carbon dioxide, which
3638-482: Is an uncommon mineral in limestone, and siderite or other carbonate minerals are rare. However, the calcite in limestone often contains a few percent of magnesium . Calcite in limestone is divided into low-magnesium and high-magnesium calcite, with the dividing line placed at a composition of 4% magnesium. High-magnesium calcite retains the calcite mineral structure, which is distinct from dolomite. Aragonite does not usually contain significant magnesium. Most limestone
3745-402: Is at a distance from road connections. Slite is the largest settlement on Gotland's sparsely populated east coast. The eastern coast of Gotland, including the adjacent marine waters and islets, has been designated an 150,000 ha Important Bird Area (IBA) by BirdLife International because it supports a suite of waterfowl , waders and terns . Gotland has a semi-continental variety of
3852-402: Is carbonate rock, and most of this is limestone. Limestone is found in sedimentary sequences as old as 2.7 billion years. However, the compositions of carbonate rocks show an uneven distribution in time in the geologic record. About 95% of modern carbonates are composed of high-magnesium calcite and aragonite. The aragonite needles in carbonate mud are converted to low-magnesium calcite within
3959-474: Is clusters of peloids cemented together by organic material or mineral cement. Extraclasts are uncommon, are usually accompanied by other clastic sediments, and indicate deposition in a tectonically active area or as part of a turbidity current . The grains of most limestones are embedded in a matrix of carbonate mud. This is typically the largest fraction of an ancient carbonate rock. Mud consisting of individual crystals less than 5 μm (0.20 mils) in length
4066-416: Is commonly white to gray in color. Limestone that is unusually rich in organic matter can be almost black in color, while traces of iron or manganese can give limestone an off-white to yellow to red color. The density of limestone depends on its porosity, which varies from 0.1% for the densest limestone to 40% for chalk. The density correspondingly ranges from 1.5 to 2.7 g/cm . Although relatively soft, with
4173-420: Is controlled largely by the amount of dissolved carbon dioxide ( CO 2 ) in the water. This is summarized in the reaction: Increases in temperature or decreases in pressure tend to reduce the amount of dissolved CO 2 and precipitate CaCO 3 . Reduction in salinity also reduces the solubility of CaCO 3 , by several orders of magnitude for fresh water versus seawater. Near-surface water of
4280-545: Is converted to low-magnesium calcite. Diagenesis is the likely origin of pisoliths , concentrically layered particles ranging from 1 to 10 mm (0.039 to 0.394 inches) in diameter found in some limestones. Pisoliths superficially resemble ooids but have no nucleus of foreign matter, fit together tightly, and show other signs that they formed after the original deposition of the sediments. Silicification occurs early in diagenesis, at low pH and temperature, and contributes to fossil preservation. Silicification takes place through
4387-503: Is deposited close to where it formed, classification of limestone is usually based on its grain type and mud content. Most grains in limestone are skeletal fragments of marine organisms such as coral or foraminifera . These organisms secrete structures made of aragonite or calcite, and leave these structures behind when they die. Other carbonate grains composing limestones are ooids , peloids , and limeclasts ( intraclasts and extraclasts [ ca ] ). Skeletal grains have
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4494-460: Is described as coquinite . Chalk is a soft, earthy, fine-textured limestone composed of the tests of planktonic microorganisms such as foraminifera, while marl is an earthy mixture of carbonates and silicate sediments. Limestone forms when calcite or aragonite precipitate out of water containing dissolved calcium, which can take place through both biological and nonbiological processes. The solubility of calcium carbonate ( CaCO 3 )
4601-617: Is described as micrite . In fresh carbonate mud, micrite is mostly small aragonite needles, which may precipitate directly from seawater, be secreted by algae, or be produced by abrasion of carbonate grains in a high-energy environment. This is converted to calcite within a few million years of deposition. Further recrystallization of micrite produces microspar , with grains from 5 to 15 μm (0.20 to 0.59 mils) in diameter. Limestone often contains larger crystals of calcite, ranging in size from 0.02 to 0.1 mm (0.79 to 3.94 mils), that are described as sparry calcite or sparite . Sparite
4708-462: Is distinguished from micrite by a grain size of over 20 μm (0.79 mils) and because sparite stands out under a hand lens or in thin section as white or transparent crystals. Sparite is distinguished from carbonate grains by its lack of internal structure and its characteristic crystal shapes. Geologists are careful to distinguish between sparite deposited as cement and sparite formed by recrystallization of micrite or carbonate grains. Sparite cement
4815-560: Is one of the first minerals to precipitate in marine evaporites. Most limestone is formed by the activities of living organisms near reefs, but the organisms responsible for reef formation have changed over geologic time. For example, stromatolites are mound-shaped structures in ancient limestones, interpreted as colonies of cyanobacteria that accumulated carbonate sediments, but stromatolites are rare in younger limestones. Organisms precipitate limestone both directly as part of their skeletons, and indirectly by removing carbon dioxide from
4922-473: Is otherwise chemically fairly pure, with clastic sediments (mainly fine-grained quartz and clay minerals ) making up less than 5% to 10% of the composition. Organic matter typically makes up around 0.2% of a limestone and rarely exceeds 1%. Limestone often contains variable amounts of silica in the form of chert or siliceous skeletal fragments (such as sponge spicules, diatoms , or radiolarians ). Fossils are also common in limestone. Limestone
5029-472: Is produced by decaying organic matter settling into the deep ocean that is not removed by photosynthesis in the dark depths. As a result, there is a fairly sharp transition from water saturated with calcium carbonate to water unsaturated with calcium carbonate, the lysocline , which occurs at the calcite compensation depth of 4,000 to 7,000 m (13,000 to 23,000 feet). Below this depth, foraminifera tests and other skeletal particles rapidly dissolve, and
5136-518: Is secondary dolomite, formed by chemical alteration of limestone. Limestone is exposed over large regions of the Earth's surface, and because limestone is slightly soluble in rainwater, these exposures often are eroded to become karst landscapes. Most cave systems are found in limestone bedrock. Limestone has numerous uses: as a chemical feedstock for the production of lime used for cement (an essential component of concrete ), as aggregate for
5243-471: Is therefore an effort not only to write down the history of Gotland, but also to assert Gotland's independence from Sweden. It gives Awair Strabain as the name of the man who arranged the mutually beneficial agreement with the king of Sweden; the event would have taken place before the end of the ninth century, when Wulfstan of Hedeby reported that the island was subject to the Swedes: Then, after
5350-643: The Carolingian Empire , as major commercial centers for the next several centuries. The Berezan' Runestone , discovered in 1905 in Ukraine, was made by a Varangian ( Viking ) trader named Grani in memory of his business partner Karl. It is assumed that they were from Gotland. The Mästermyr chest , an important artefact from the Viking Age , was found in Gotland. On 16 July 1999,
5457-459: The Finnish War between Sweden and Russia, a Russian army landed on the southeastern shores of Gotland near Grötlingbo . Under command of Nikolai Andreevich Bodisko 1,800 Russians took the city of Visby without any combat or engagement, and occupied the island. A Swedish naval force rescue expedition was sent from Karlskrona under the command of admiral Rudolf Cederström with 2,000 men;
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#17327723529445564-667: The Teutonic Knights , awarded to them on the condition that they expel the piratical Victual Brothers from their fortified sanctuary . An invading army of Teutonic Knights conquered the island in 1398, destroying Visby and driving the Victual Brothers from Gotland. In 1409, Grand Master Ulrich von Jungingen of the Teutonic Knights guaranteed peace with the Kalmar Union of Scandinavia by selling
5671-525: The land of the Burgundians , we had on our left the lands that have been called from the earliest times Blekingey , and Meore , and Eowland , and Gotland, all which territory is subject to the Sweons ; and Weonodland was all the way on our right, as far as Weissel -mouth. The number of Arab dirhams discovered on the island of Gotland alone is astoundingly high. In the various hoards located around
5778-624: The sunny climate and the extensive shoreline bordering mild waters. During summer, Visby hosts the political event Almedalen Week , followed by the Medieval Week , further boosting visitor numbers. In winter, Gotland usually remains surrounded by ice-free water and has mild weather. Gotland has been inhabited since approximately 7200 BC. The island's main sources of income are agriculture, food processing, tourism, information technology services, design, and some heavy industry such as concrete production from locally mined limestone . From
5885-442: The Baltic sea with Visby as one of their destinations. In 2005, 147 ships docked at Visby, in 2010 the number was 69. In 2014, 62 ships are scheduled to visit Visby. The decrease in visiting ships is due to the fact that the modern cruise ships are too large to enter Visby harbor. Ships must anchor a fair distance from shore whereupon passengers are shuttled to shore in small boats, which is not possible during bad weather. In 2007,
5992-496: The Earth's history. Limestone may have been deposited by microorganisms in the Precambrian , prior to 540 million years ago, but inorganic processes were probably more important and likely took place in an ocean more highly oversaturated in calcium carbonate than the modern ocean. Diagenesis is the process in which sediments are compacted and turned into solid rock . During diagenesis of carbonate sediments, significant chemical and textural changes take place. For example, aragonite
6099-660: The Midsummer's Eve celebration on the island, but also throughout the summer months. The games have widespread renown; some of them are played by people as far away as in the United States. The knotwork design subsequently named the " Valknut " has the most attested historic instances on picture stones in Gotland, which include being on both the Stora Hammars I and the Tängelgårda stones . Gotland also has
6206-543: The Romanesque style from 1150 to 1250. The newer churches were constructed in the Gothic architectural style that prevailed from about 1250–1400. The oldest painting inside one of the churches on Gotland stretches as far back in time as the 12th century. Traditional games of skill like Kubb , Pärk , and Varpa are played on Gotland. They are part of what has become called "Gutniska Lekar", and are performed preferably on
6313-430: The accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite , a closely related rock, which contains
6420-434: The base of roads, as white pigment or filler in products such as toothpaste or paint, as a soil conditioner , and as a popular decorative addition to rock gardens . Limestone formations contain about 30% of the world's petroleum reservoirs . Limestone is composed mostly of the minerals calcite and aragonite , which are different crystal forms of calcium carbonate ( CaCO 3 ). Dolomite , CaMg(CO 3 ) 2 ,
6527-657: The beds. This may include the formation of vugs , which are crystal-lined cavities within the limestone. Diagenesis may include conversion of limestone to dolomite by magnesium-rich fluids. There is considerable evidence of replacement of limestone by dolomite, including sharp replacement boundaries that cut across bedding. The process of dolomitization remains an area of active research, but possible mechanisms include exposure to concentrated brines in hot environments ( evaporative reflux ) or exposure to diluted seawater in delta or estuary environments ( Dorag dolomitization ). However, Dorag dolomitization has fallen into disfavor as
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#17327723529446634-515: The buildings on the range, the former tank repair shop , is currently owned by a private company ( Peab ), with the military renting back the top floor for its own use. When not used by the military, a number of cultural and sports events have been held at the range, one of the most notable being the Gotland Grand National [ sv ] , the world's largest enduro race, from 1984 to 2023. As of 2018, Gotland has received
6741-410: The bulk of this initial garrison will make up a new motorised rifle battalion, alternatively referred to in other reports as a "modular-structured rapid response Army battalion". A later report claimed that plans were at an advanced stage for a support helicopter squadron and an Air Force "fast response Gripen jet squadron" to also be based on the island to support the new garrison and further reinforce
6848-556: The countryside had to be put down by King Magnus III of Sweden in 1288. In 1361, Valdemar Atterdag of Denmark invaded the island. About 1,500 Gotlandic farmers were killed by the Danish invaders after massing for the Battle of Mästerby . The Victual Brothers occupied the island in 1394 to set up a stronghold as a headquarters of their own in Visby. At last, Gotland became a fief of
6955-572: The defences. Prior to the disbandment of the original garrison, there had been a continuous Swedish military presence on Gotland in one form or another, for nearly 200 years. After the standing down of the original garrison, a battalion of the Swedish Home Guard is based on Gotland for emergencies as part of the Eastern Military Region ( MR E ). The unit, 32:a Gotlandsbataljonen (the 32nd Gotland battalion), acts as
7062-466: The depositional fabric of carbonate rocks. Dunham divides the rocks into four main groups based on relative proportions of coarser clastic particles, based on criteria such as whether the grains were originally in mutual contact, and therefore self-supporting, or whether the rock is characterized by the presence of frame builders and algal mats. Unlike the Folk scheme, Dunham deals with the original porosity of
7169-469: The deposits are highly porous, so that they have a spongelike texture, they are typically described as tufa . Secondary calcite deposited by supersaturated meteoric waters ( groundwater ) in caves is also sometimes described as travertine. This produces speleothems , such as stalagmites and stalactites . Coquina is a poorly consolidated limestone composed of abraded pieces of coral , shells , or other fossil debris. When better consolidated, it
7276-406: The earth's oceans are oversaturated with CaCO 3 by a factor of more than six. The failure of CaCO 3 to rapidly precipitate out of these waters is likely due to interference by dissolved magnesium ions with nucleation of calcite crystals, the necessary first step in precipitation. Precipitation of aragonite may be suppressed by the presence of naturally occurring organic phosphates in
7383-453: The first proposition for building a new pier at Visby harbor, large enough to serve the modern cruise ships, was made. In 2011, the matter of the new pier was discussed in the Riksdag and in 2012 research and planning for the pier began. In January 2014, a letter of intent for building a new cruise pier in Visby harbor was signed by Region Gotland and Copenhagen Malmö Port (CMP). The pier
7490-399: The first refers to the grains and the second to the cement. For example, a limestone consisting mainly of ooids, with a crystalline matrix, would be termed an oosparite. It is helpful to have a petrographic microscope when using the Folk scheme, because it is easier to determine the components present in each sample. Robert J. Dunham published his system for limestone in 1962. It focuses on
7597-572: The formation of distinctive minerals from the silica and clay present in the original limestone. Two major classification schemes, the Folk and Dunham, are used for identifying the types of carbonate rocks collectively known as limestone. Robert L. Folk developed a classification system that places primary emphasis on the detailed composition of grains and interstitial material in carbonate rocks . Based on composition, there are three main components: allochems (grains), matrix (mostly micrite), and cement (sparite). The Folk system uses two-part names;
7704-429: The geologic record are called bioherms . Many are rich in fossils, but most lack any connected organic framework like that seen in modern reefs. The fossil remains are present as separate fragments embedded in ample mud matrix. Much of the sedimentation shows indications of occurring in the intertidal or supratidal zones, suggesting sediments rapidly fill available accommodation space in the shelf or platform. Deposition
7811-465: The island had twenty district courts ( tings ), each represented by its elected judge at the island-ting, called landsting . New laws were decided at the landsting, which also took other decisions regarding the island as a whole. The city of Visby and rest of the island were governed separately, and a civil war caused by conflicts between the German merchants in Visby and the peasants they traded with in
7918-691: The island has remained under Swedish rule. On 19 September 1806, Gustav IV Adolf offered the sovereignty of Gotland to the Order of St. John of Jerusalem , who had been expelled from Malta in 1798, but the Order rejected the offer since it would have meant renouncing their claim to Malta. The Order never regained its territory, and eventually it reestablished itself in Rome as the Sovereign Military Order of Malta . On 22 April 1808, during
8025-480: The island of Gotland and the other areas of the province of Gotland make up 0.8% of Sweden's total land area. The province includes the small islands of Fårö and Gotska Sandön to the north, as well as the Karlsö Islands, (Lilla and Stora) to the west, which are even smaller. The island of Gotland has an area of 2,994 km (1,156 sq mi), whereas the province has 3,183.7 km (1,229.2 sq mi) [3,151 km (1,217 sq mi) of land excluding
8132-532: The island of Gotland to Queen Margaret of Denmark, Norway and Sweden . The authority of the landsting was successively eroded after the island was occupied by the Teutonic Order, then sold to Eric of Pomerania and after 1449 ruled by Danish governors. In late medieval times, the ting consisted of twelve representatives for the farmers, free-holders or tenants. Since the Treaty of Brömsebro in 1645,
8239-473: The island was liberated and the Russians capitulated. Russian forces left the island on 18 May 1808. The traditional provinces of Sweden serve no administrative or political purposes today, but are historical and cultural entities. In the case of Gotland, however, due to its insular position, the administrative county ( län ), Gotland County , and the municipality ( kommun ), Region Gotland , both cover
8346-614: The island, there are more of these silver coins than at any other site in Western Eurasia. The total sum is almost as great as the number that has been unearthed in the entire Muslim world. These coins moved north through trade between Rus merchants and the Abbasid Caliphate , along the Silver-Fur Road , and the money made by Scandinavian merchants would help northern Europe, especially Viking Scandinavia and
8453-568: The island. In 2012, there were 171 registered sports organizations on Gotland. Limestone Limestone ( calcium carbonate CaCO 3 ) is a type of carbonate sedimentary rock which is the main source of the material lime . It is composed mostly of the minerals calcite and aragonite , which are different crystal forms of CaCO 3 . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as
8560-436: The island; palæo- sea-stacks are preserved in places. The island's main sources of income are agriculture along with food processing, tourism, IT solutions, design and some heavy industry such as concrete production from locally mined limestone . Most of Gotland's economy is based on small scale production. In 2012, there were over 7,500 registered companies on Gotland. 1,500 of these had more than one employee. Gotland has
8667-456: The lakes and rivers]. The population is 61,001 as of December 2021. As of 2016, approximately 23,600 people (about 40% of residents) lived in Visby, which is the seat of the municipality and the capital of the county. Gotland is located about 90 km (56 mi) east of the Swedish mainland and about 130 km (81 mi) from the Baltic states , Latvia being the nearest. Gotland is
8774-655: The link to point directly to the intended article. Retrieved from " https://en.wikipedia.org/w/index.php?title=Gutland&oldid=1258836054 " Categories : Disambiguation pages Place name disambiguation pages Hidden categories: Short description is different from Wikidata All article disambiguation pages All disambiguation pages Gotland Gotland ( / ˈ ɡ ɒ t l ə n d / , Swedish: [ˈɡɔ̌tːland] ; Gutland in Gutnish ), also historically spelled Gottland or Gothland ( / ˈ ɡ ɒ θ l ə n d / ),
8881-456: The name of the main island, but the adjacent islands are generally considered part of Gotland and the Gotlandic culture: There are several shallow lakes located near the shores of the island. The biggest is Lake Bästeträsk , located near Fleringe in the northern part of Gotland. The Hoburg Shoal bird reserve is situated on the southern tip of the island. The highest point of the island
8988-410: The ocean basins, but limestone is rarely preserved in continental slope and deep sea environments. The best environments for deposition are warm waters, which have both a high organic productivity and increased saturation of calcium carbonate due to lower concentrations of dissolved carbon dioxide. Modern limestone deposits are almost always in areas with very little silica-rich sedimentation, reflected in
9095-582: The other areas of the province of Gotland make up less than one percent of Sweden's total land area. The county formed by the archipelago is the second smallest by area and is the least populated in Sweden. In spite of the small size due to its narrow width, the driving distance between the furthermost points of the populated islands is about 170 kilometres (110 mi). Gotland is a fully integrated part of Sweden with no particular autonomy, unlike several other offshore island groups in Europe. Historically, there
9202-426: The reaction: Fossils are often preserved in exquisite detail as chert. Cementing takes place rapidly in carbonate sediments, typically within less than a million years of deposition. Some cementing occurs while the sediments are still under water, forming hardgrounds . Cementing accelerates after the retreat of the sea from the depositional environment, as rainwater infiltrates the sediment beds, often within just
9309-482: The relative purity of most limestones. Reef organisms are destroyed by muddy, brackish river water, and carbonate grains are ground down by much harder silicate grains. Unlike clastic sedimentary rock, limestone is produced almost entirely from sediments originating at or near the place of deposition. Limestone formations tend to show abrupt changes in thickness. Large moundlike features in a limestone formation are interpreted as ancient reefs , which when they appear in
9416-696: The residents still speak Gutnish (Gutamål), the autochthonous language on the islands. But most of them now speak Gotlandic ( Swedish : gotländska ), a Gutnish-influenced Swedish dialect. In the 13th century, a work containing the laws of the island, called "the Gotlandic law" (Gutalagen), was published in Old Gutnish , as well as the Gutasaga . Gotland is noted for its 94 Medieval churches , most of which are restored and in active use. These churches exhibit two major styles of architecture: Romanesque and Gothic . The older churches were constructed in
9523-460: The rock. The Dunham scheme is more useful for hand samples because it is based on texture, not the grains in the sample. A revised classification was proposed by Wright (1992). It adds some diagenetic patterns to the classification scheme. Travertine is a term applied to calcium carbonate deposits formed in freshwater environments, particularly waterfalls , cascades and hot springs . Such deposits are typically massive, dense, and banded. When
9630-421: The same territory as the province. Furthermore, the diocese of Visby is also congruent with the province. Gotland is traditionally divided into 92 sockens . On 1 January 2016, they were all reconstituted into Districts , administrative areas with the same borders as the former sockens. Gotland was granted its arms in about 1560. The coat of arms is represented with a ducal coronet. Blazon: "Azure
9737-451: The sea was 50 to 100 m (160 to 330 ft), and reefs continued to dominate the sedimentary record. Some sandstones are present in the youngest rocks towards the south of the island, which represent sand bars deposited very close to the shoreline. The lime rocks have been weathered into characteristic karstic rock formations known as rauks . Fossils, mainly of crinoids , rugose corals and brachiopods , are abundant throughout
9844-479: The sediments increases. Chemical compaction takes place by pressure solution of the sediments. This process dissolves minerals from points of contact between grains and redeposits it in pore space, reducing the porosity of the limestone from an initial high value of 40% to 80% to less than 10%. Pressure solution produces distinctive stylolites , irregular surfaces within the limestone at which silica-rich sediments accumulate. These may reflect dissolution and loss of
9951-662: The sediments of the ocean floor abruptly transition from carbonate ooze rich in foraminifera and coccolith remains ( Globigerina ooze) to silicic mud lacking carbonates. In rare cases, turbidites or other silica-rich sediments bury and preserve benthic (deep ocean) carbonate deposits. Ancient benthic limestones are microcrystalline and are identified by their tectonic setting. Fossils typically are foraminifera and coccoliths. No pre-Jurassic benthic limestones are known, probably because carbonate-shelled plankton had not yet evolved. Limestones also form in freshwater environments. These limestones are not unlike marine limestone, but have
10058-473: The south, and overlies a 75 to 125 m (246 to 410 ft) thick Ordovician sequence. It was deposited in a shallow, hot, and salty sea on the edge of an equatorial continent. The water depth never exceeded 175 to 200 m (574 to 656 ft), and became shallower over time as bioherm detritus and terrestrial sediments filled the basin. Reef growth started in the Llandovery Epoch , when
10165-533: The water by photosynthesis and thereby decreasing the solubility of calcium carbonate. Limestone shows the same range of sedimentary structures found in other sedimentary rocks. However, finer structures, such as lamination , are often destroyed by the burrowing activities of organisms ( bioturbation ). Fine lamination is characteristic of limestone formed in playa lakes , which lack the burrowing organisms. Limestones also show distinctive features such as geopetal structures , which form when curved shells settle to
10272-553: The water. Although ooids likely form through purely inorganic processes, the bulk of CaCO 3 precipitation in the oceans is the result of biological activity. Much of this takes place on carbonate platforms . The origin of carbonate mud, and the processes by which it is converted to micrite, continue to be a subject of research. Modern carbonate mud is composed mostly of aragonite needles around 5 μm (0.20 mils) in length. Needles of this shape and composition are produced by calcareous algae such as Penicillus , making this
10379-484: The weather station Östergarnsholm. As an example, December is warmer than March with temperature lows being similar to April. August is typically the warmest month, an unusual occurrence in Swedish sites. In capital Visby, July and August temperatures tend to be quite even. Since winters usually remain just above freezing and brackish water remaining liquid longer than freshwater, the sea remains ice-free all year round, except during rare extreme cold waves . The last time
10486-499: The west part of the island from the 1860s. When a new law ensuring two weeks vacation for all employees in Sweden was passed in 1938, camping became a popular pastime among the Swedes, and in 1955, Gotland was visited by 80,000 people. In the 1970s mostly young people were attracted to Gotland. Since 2010 the island has become a more versatile vacation spot visited by people from all over the world, in all manner of ways. In 2001, it
10593-490: The whole passage from the mainland to Gotland froze was in 1987 when icebreakers were used to maintain passenger and goods traffic to the island. Gotland is made up of a sequence of sedimentary rocks of a Silurian age, dipping to the south-east. The main Silurian succession of limestones and shales comprises thirteen units spanning 200 to 500 m (660 to 1,640 ft) of stratigraphic thickness, being thickest in
10700-616: The world's largest Viking silver treasure, the Spillings Hoard , was found in a field at Spillings farm northwest of Slite . The silver treasure was divided into two parts weighing a total of 67 kg (148 lb) (27 kg (60 lb) and 40 kg (88 lb)) and consisted mostly of coins, about 14,000, from foreign countries, mostly Islamic. It also contained about 20 kg (44 lb) of bronze objects along with numerous everyday objects such as nails, glass beads, parts of tools, pottery, iron bands and clasps. The treasure
10807-525: The world's northernmost established vineyard and winery, located in Hablingbo . Gotland occupies a strategic location in the Baltic sea from a defence viewpoint. In March 2015, the Swedish government decided to begin reestablishing a permanent military presence on Gotland, starting with an initial 150 troop garrison, consisting primarily of elements from the Swedish Army . It has been reported that
10914-406: Was a linguistic difference between the archipelago and the mainland with Gutnish being the native language. In recent centuries, Swedish took over almost entirely and the island is virtually monolingually Swedish in modern times. The archipelago is a very popular domestic tourist destination for mainland Swedes, with the population rising to very high numbers during summers. Some of the reasons are
11021-573: Was a major training and storage facility for the Gotland garrison during its existence, and was still occasionally used for training by various elements of the Armed Forces since the garrison was shut down in 2005. However, from the second half of 2014 onwards, there has been a marked increase in the use of the range, especially by armored units (mostly company sized), as tensions in Northeastern Europe have escalated. At least one of
11128-804: Was finished in 2018. The estimated cost is 250 million crowns (about US$ 38.52 million). A number of stones with grooves exist on Gotland. Archaeologists interpret these grooves as traces of an unknown industrial process in the High Middle Ages . There are approximately 3,700 grinding grooves, of which about 750 occur in the solid limestone outcrop and the rest in other rock formations. The latter often consist of hard rocks such as granite or gneiss, but also soft rocks such as sandstone occur. Grinding grooves are also found in Skåne, in southern Sweden and in Finland. Astronomer Göran Henriksson dates
11235-426: Was found by using a metal detector, and the finders fee, given to the farmer who owned the land, was over 2 million kronor (about US$ 308,000). The treasure was found almost by accident while filming a news report for TV4 about illegal treasure hunting on Gotland. Early on, Gotland became a commercial center, with the town of Visby the most important Hanseatic city in the Baltic Sea . In late medieval times,
11342-416: Was likely deposited in pore space between grains, suggesting a high-energy depositional environment that removed carbonate mud. Recrystallized sparite is not diagnostic of depositional environment. Limestone outcrops are recognized in the field by their softness (calcite and aragonite both have a Mohs hardness of less than 4, well below common silicate minerals) and because limestone bubbles vigorously when
11449-439: Was the fifth largest tourist destination in Sweden based on the total number of guest nights. Gotland is usually the part of Sweden which receives the most hours of sunlight during a year with Visby statistically the location with the most sunshine in Sweden. In 2007 approximately 750,000 people visited Gotland. In 1996, for the first time, ferries between Gotland and mainland Sweden carried more than 1 million passengers in
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