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Damestenen
The Damestenen ("Stone of the Ladies" in English), also referred as ''Hesselagerstenen'' ("Large stone of Hesselager"), is a glacial erratic located near Svendborg, in the south-east of Fionia, Denmark. Geography The boulder is the biggest glacial erratic in Denmark, followed by the Tirslund Rock. It stands close to the village of Hesselager, some 20 km northeast of Svendborg; located in a field, it can be reached by a country lane named ''Damestenensvej''. Features The Damestenen consists of a block of light grey granite dating back to the last Last Glacial Period. Its height is 12 m, the circumference is 46 m, and its weight is 1000 tons. History The boulder is mentioned by the Danish theologian Erik Pontoppidan in his work titled ''Den Danske Atlas'' (1763–1781). In 1840, during Christian VIII's kingdom, the boulder was analysed by the geologist Johan Georg Forchhammer, who suggested to excavate around it in order to determine its size and to c ...
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Svindinge
Svindinge is a village in central Denmark ) , song = ( en, "King Christian stood by the lofty mast") , song_type = National and royal anthem , image_map = EU-Denmark.svg , map_caption = , subdivision_type = Sovereign state , subdivision_name = Danish Realm, Kingdom of Denmark ..., located in Nyborg municipality on the island of Funen in Region of Southern Denmark. History Svindinge is first mentioned in 1376 as Swinninge, but likely originates from the Iron Age. Svindinge Church Svindinge Church was built in the period 1571–78. The construction was ordered by Christoffer Valckendorf, the owner of Glorup manor at the time. A local story tells of a jötunn from Langeland, who was upset with Svindinge Church's tall steeple and threw a giant rock at the church. She failed to hit, and instead the stone landed near Hesselager, where Damestenen, it is located today. The church has three bells. The largest is known as "Saint Peter's Rooster" (Danish: ''Skt. Peders Hane'' ...
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Hesselager
Hesselager is a small town located on the island of Funen in south-central Denmark, in Svendborg Municipality. It is located 19 km south of Nyborg, 7 km northwest of Lundeborg and 18 km northeast of Svendborg. Close to the village stands the Damestenen The Damestenen ("Stone of the Ladies" in English), also referred as ''Hesselagerstenen'' ("Large stone of Hesselager"), is a glacial erratic located near Svendborg, in the south-east of Fionia, Denmark. Geography The boulder is the biggest ... (or ''Hesselagerstenen''), the biggest glacial erratic of Denmark., Valdemar Johan Heinrich Nordmann, Victor Christian Madsen (Danmarks geologiske undersøgelse), ''Compte rendu de la Réunion géologique internationale à Copenhague, 1928'', C. A. Reitzel, 1930, . References Cities and towns in the Region of Southern Denmark Svendborg Municipality {{SouthernDK-stub ...
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Tirslund Rock
Tirslund Rock or Tirslundstenen is a glacial erratic in Denmark. Deposited during the Ice Age it lies 4 km west of Brørup. It is Jutland's largest granite boulder and the second largest in Denmark after the Damestenen. Its height is 3.5 metres above the ground and it is 16 metres in circumference. The weight is about 340 tons. The rock was put under protection in 1832. History According to the legend, King Harald Bluetooth Harald "Bluetooth" Gormsson ( non, Haraldr Blátǫnn Gormsson; da, Harald Blåtand Gormsen, died c. 985/86) was a king of Denmark and Norway. He was the son of King Gorm the Old and of Thyra Dannebod. Harald ruled as king of Denmark from c. 95 ... wanted to use the Tirslund Rock as a memorial stone on his parents Gorm the Old and Thyra's burial mounds in Jelling. It was supposed to be transported on a great iron sled, but as the legend says, enemies forced King Harrold to abandon this enterprise. So the stone was left where it stands and the i ...
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Glacial Erratic
A glacial erratic is glacially deposited rock differing from the type of rock native to the area in which it rests. Erratics, which take their name from the Latin word ' ("to wander"), are carried by glacial ice, often over distances of hundreds of kilometres. Erratics can range in size from pebbles to large boulders such as Big Rock () in Alberta. Geologists identify erratics by studying the rocks surrounding the position of the erratic and the composition of the erratic itself. Erratics are significant because: *They can be transported by glaciers, and they are thereby one of a series of indicators which mark the path of prehistoric glacier movement. Their lithographic origin can be traced to the parent bedrock, allowing for confirmation of the ice flow route. *They can be transported by ice rafting. This allows quantification of the extent of glacial flooding resulting from ice dam failure which release the waters stored in proglacial lakes such as Lake Missoula. Erratics ...
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Svendborg
Svendborg () is a town on the island of Funen in south-central Denmark, and the seat of Svendborg Municipality. With a population of 27,300 (1 January 2022), Svendborg is Funen's second largest city.BY3: Population 1st January by urban areas, area and population density
The Mobile Statbank from Statistics Denmark
In 2000 Svendborg was declared "Town of the year" in Denmark, and in 2003 it celebrated its 750th anniversary as a . By road, Svendborg is located southwest of



Funen
Funen ( da, Fyn, ), with an area of , is the third-largest island of Denmark, after Zealand and Vendsyssel-Thy. It is the 165th-largest island in the world. It is located in the central part of the country and has a population of 469,947 as of 2020. Funen's main city is Odense, which is connected to the sea by a seldom-used canal. The city's shipyard, Odense Steel Shipyard, has been relocated outside Odense proper. Funen belongs administratively to the Region of Southern Denmark. From 1970 to 2006 the island formed the biggest part of Funen County, which also included the islands of Langeland, Ærø, Tåsinge, and a number of smaller islands. Funen is linked to Zealand, Denmark's largest island, by the Great Belt Bridge, which carries both trains and cars. The bridge is in reality three bridges; low road and rail bridges connect Funen to the small island of Sprogø in the middle of the Great Belt, and a long road suspension bridge (the second longest in the world at the time ...
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Granite
Granite () is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is nearly alway ...
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Erik Pontoppidan
Erik Ludvigsen Pontoppidan (24 August 1698 – 20 December 1764) was a Danish author, a Lutheran bishop of the Church of Norway, an historian, and an antiquarian. His Catechism of the Church of Denmark heavily influenced Danish and Norwegian religious thought and practice for roughly the next 200 years after its 1737 publication. Biography Pontoppidan was educated in Fredericia (1716–1718), after which he was a private tutor in Norway, and then studied in Holland, and in London and Oxford, England. In 1721 he became ''informator'' of Frederick Carl of Carlstein (later duke of Plön), and two years later morning preacher in the castle and afternoon preacher in Nordborg. From 1726 to 1734 he was pastor at Hagenberg, where he so protected the pietists as to find it advisable to defend his course against the Lutherans with ''Dialogus; oder Unterredung Severi, Sinceri, und Simplicis von der Religion and Reinheit der Lehre'' (1726) and ''Heller Glaubensspiegel'' (1727). During this ...
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