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49-544: The municipality is situated along the Sagfjorden in south central Troms county. The municipality is mostly coastal areas around the fjord as well as some inland valleys . Salangen is home to the world's northernmost bat population. The 458-square-kilometre (177 sq mi) municipality is the 217th largest by area out of the 357 municipalities in Norway. Salangen is the 278th most populous municipality in Norway with

98-609: A passive margin . Sedimentary rocks that were deposited on top of the basement complex were formed in a setting of quiet marine and river waters. The craton was covered by shallow, warm, tropical epicontinental or epicratonic sea (meaning literally "on the craton") that had maximum depths of only about 60 m (200 ft) at the shelf edge. The position of the equator during the Late Ordovician epoch ( c.  458  – c.   444 Ma) on Laurentia has been determined via extensive shell bed records. Flooding of

147-633: A network of early Proterozoic orogenic belts . Small microcontinents and oceanic islands collided with and sutured onto the ever-growing Laurentia, and together formed the stable Precambrian craton seen today. The craton is named after the Laurentian Shield , through the Laurentian Mountains , which received their name from the St. Lawrence River , named after Saint Lawrence of Rome. In eastern and central Canada, much of

196-453: A population of 2,069. The municipality's population density is 4.5 inhabitants per square kilometre (12/sq mi) and its population has decreased by 6.9% over the previous 10-year period. The municipality of Salangen was established on 1 January 1871 when it was separated from the large Ibestad Municipality . The initial population of Salangen Municipality was 1,384. During the 1960s, there were many municipal mergers across Norway due to

245-473: A separate municipality once again. After the split, the new, smaller Salangen Municipality had 2,611 residents. On 1 January 2020, the municipality became part of the newly formed Troms og Finnmark county. Previously, it had been part of the old Troms county. On 1 January 2024, the Troms og Finnmark county was divided and the municipality once again became part of Troms county. The municipality (originally

294-482: Is located mainly on quartzite (known as Sjøvegan quartzite locally and regionally as Bø quartzite). In the hills to the south, there is garnet -rich schist (known as Trollvannet schist). Across the nearby lake Nervatnet and towards the village of Strokkenes , granite within marble is present (Høglund marble and Strokkenes granite). This granite is Leucratic, an indicative sign of granite intruded within an orogenic mountain building event. Salangen Municipality

343-788: Is more common, not least because large parts of the structure extend outside Canada. In the United States, the craton bedrock is covered with sedimentary rocks on the broad interior platform in the Midwest and Great Plains regions and is exposed only in northern Minnesota, Wisconsin, the New York Adirondacks , and the Upper Peninsula of Michigan . The sequence of sedimentary rocks varies from about 1,000 m to in excess of 6,100 m (3,500–20,000 ft) in thickness. The cratonic rocks are metamorphic or igneous with

392-575: Is part of Laurentia. The island is separated from North America by the Nares Strait , but this is a Pleistocene erosional feature. The strait is floored with continental crust and shows no indications of a thermal event or seaway tectonism. Greenland is composed mostly of crust of Archean to Proterozoic age, with lower Paleocene shelf formations on its northern margin and Devonian to Paleogene formations on its western and eastern margins. The eastern and northern margins were heavily deformed during

441-654: Is part of the Indre Troms prosti ( deanery ) in the Diocese of Nord-Hålogaland . The municipality is located in the southern part of Troms county, at the northeastern end of the Astafjorden . Ibestad Municipality is located west of Salangen, connected by the Mjøsund Bridge ; Lavangen Municipality to the south; Bardu Municipality to the east; and Dyrøy Municipality and Sørreisa Municipality are to

490-409: Is responsible for primary education (through 10th grade), outpatient health services , senior citizen services, welfare and other social services , zoning , economic development , and municipal roads and utilities. The municipality is governed by a municipal council of directly elected representatives. The mayor is indirectly elected by a vote of the municipal council. The municipality

539-565: Is under the jurisdiction of the Midtre Hålogaland District Court and the Hålogaland Court of Appeal . The municipal council (Kommunestyre) of Salangen is made up of 19 representatives that are elected to four year terms. The tables below show the current and historical composition of the council by political party . The mayor ( Norwegian : ordfører ) of Salangen is the political leader of

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588-535: The Astafjorden and then turns to the southeast until it reaches the village of Sjøvegan at the head of the fjord. The innermost part of the fjord is also named the Sagfjorden. This article about a location in Troms is a stub . You can help Misplaced Pages by expanding it . This article about a fjord in Norway is a stub . You can help Misplaced Pages by expanding it . Laurentia Laurentia or

637-632: The Basin and Range Province has been stretched up to 100% of its original width. The area experienced numerous large volcanic eruptions . Baja California rifted away from North America during the Miocene . This block of crust consists of Proterozoic to early Paleozoic shelf and Mesozoic arc volcano formations. The Holocene being an interglacial , a warm spell between episodes of extensive glaciation. Several climate events occurred in Laurentia during

686-611: The Belt Supergroup , which is over 12 kilometers (7.5 mi) thick. By 750 Ma the breakup was mostly complete, and Gondwana (composed of most of today's southern continents) had rotated away from Laurentia, which was left isolated near the equator. The breakup of Rodinia may have triggered an episode of severe ice ages (the Snowball Earth hypothesis.) There is some evidence that the fragments of Rodinia gathered into another short-lived supercontinent, Pannotia , at

735-642: The Caledonian orogeny . The Isua Greenstone Belt of western Greenland preserves oceanic crust containing sheeted dike complexes . These provide evidence to geologists that mid-ocean ridges existed 3.8 Ga. The Abitibi gold belt in the Superior Province is the largest greenstone belt in the Canadian Shield. Laurentia first assembled from six or seven large fragments of Archean crust at around 2.0 to 1.8 Gya. The assembly began when

784-756: The Chattanooga Shale and the Antler Orogeny in the Western Cordillera. During the Carboniferous and Permian , Laurussia fused with Gondwana to form Pangaea . The resulting Alleghanian orogeny created the Central Pangean Mountains . The mountains were located close to the equator and produced a year-round zone of heavy precipitation that promoted the deposition of extensive coal beds, including

833-461: The Grenville orogeny at 1.30 to 0.95 Gya, which accreted the 1.30 to 1.00 Gya Llano-Grenville province to Laurentia. The Picuris orogeny , in particular, was characterized by the intrusion of great volumes of granitoid magma into the juvenile crust, which helped mature the crust and stitch it together. Slab rollback at 1.70 and 1.65 Gya deposited characteristic quartzite - rhyolite beds on

882-645: The North American Craton is a large continental craton that forms the ancient geological core of North America . Many times in its past, Laurentia has been a separate continent , as it is now in the form of North America, although originally it also included the cratonic areas of Greenland and the Hebridean Terrane in northwest Scotland . During other times in its past, Laurentia has been part of larger continents and supercontinents and consists of many smaller terranes assembled on

931-523: The Phanerozoic eon. During the late Cambrian through the Ordovician , sea level fluctuated with ice cap melt. Nine macro scale fluctuations of "global hyper warming", or high intensity greenhouse gas conditions, occurred. Due to sea level fluctuation, these intervals led to mudstone deposits on Laurentia that act as a record of events. The late Ordovician brought a cooling period, although

980-675: The Western Interior Seaway ran from the Gulf of Mexico to the Arctic Ocean , dividing North America into eastern and western land masses. From time to time, land masses or mountain chains rose up on the distant edges of the craton and then eroded down, shedding their sand across the landscape. Chalk beds of the Niobrara Formation were deposited at this time, and accretion of crustal fragments continued along

1029-628: The Wopmay orogen of northwest Canada. During the assembly of the core of Laurentia, banded iron formation was deposited in Michigan, Minnesota, and Labrador. The resulting nucleus of Laurentia was mostly reworked Archean crust but with some juvenile crust in the form of volcanic arc belts. Juvenile crust is crust formed from magma freshly extracted from the Earth's mantle rather than recycled from older crustal rock. The intense mountain building of

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1078-482: The charge is a seal . The seal has a tincture of argent which means it is commonly colored white, but if it is made out of metal, then silver is used. They are canting arms since the name of the municipality is derived from the old word "Sellanger", meaning "fjord of seals". The arms were designed by Arvid Sveen. The Church of Norway has one parish ( sokn ) within Salangen Municipality. It

1127-415: The parish ) is named after the local Salangen fjord ( Old Norse : Selangr ). The first element is selr which means " seal ". The last element is angr which means " fjord ". The coat of arms was granted on 2 December 1985. The official blazon is " Azure , a seal hauriant argent " ( Norwegian : I blått en skråstilt sølv sel ). This means the arms have a blue field (background) and

1176-687: The Appalachian coal beds in the U.S. Meanwhile, Gondwana had drifted onto the South Pole, and cycles of extensive glaciation produced a characteristic pattern of alternating marine and coal swamp beds called cyclothems . During the Pennsylvanian , the Ancestral Rocky Mountains were raised in the southwestern part of Laurentia. This has been attributed either to either the collision with Gondwana or subduction under

1225-700: The Slave craton collided with the Rae-Hearne craton, and the Rae-Hearne craton collided shortly after with the Superior Craton. These then merged with several smaller fragments of Archean crust, including the Wyoming, Medicine Hat, Sask, Marshfield, and Nain blocks. This series of collisions raised the mountains of the Trans-Hudson orogenic belt , which likely were similar to the modern Himalayas , and

1274-517: The Trans-Hudson orogeny formed thick, stable roots beneath the craton, possibly by a process of "kneading" that allowed low density material to move up and high density material to move down. Over the next 900 million years, Laurentia grew by the accretion of island arcs and other juvenile crust and occasional fragments of older crust (such as the Mojave block). This accretion occurred along

1323-598: The Western Cordillera. Northeast Mexico was added to the North American craton relatively recently in geological time. This block was formed from the Mesozoic to nearly the present day, with only small fragments of earlier basement rock . It moved as a coherent unit after the breakup of Pangaea. The Atlantic and Gulf Coasts experienced eight transgressions in the Cenozoic. The Laramide orogeny continued to raise

1372-650: The center of the craton nearly rifted apart along the Midcontinent Rift System . This produced the Keweenawan Supergroup , whose flood basalts are rich in copper ore. Laurentia was formed in a tectonically active world. The subduction under the southeast margin of the continent is thought to have contributed to the formation of Rodinia . According to the Southwest U.S. and East Antarctica or SWEAT hypothesis , Laurentia became

1421-491: The continent that occurred during the Ordovician provided the shallow warm waters for the success of sea life and therefore a spike in the carbonate shells of shellfish. Today the beds are composed of fossilized shells or massive-bedded Thalassinoides facies and loose shells or nonamalgamated brachiopod shell beds. These beds imply the presence of an equatorial climate belt that was hurricane free which lay inside 10° of

1470-561: The continental margin from the southwest. Two additional marine transgressions took place during the late Paleozoic: the Kaskaskia and Absaroka. The great continental mass of Pangaea strongly affected climate patterns. The Permian was relatively arid, and evaporites were deposited in the Permian Basin . Sedimentary beds deposited in the southwest in the early Triassic were fluvial in character, but gave way to eolian beds in

1519-911: The core of an independent continent with the opening of the North Atlantic in the Paleogene . Four orogenies occurred in the Mesozoic in the Western Cordillera: the Sonoma , Nevadan , Sevier , and Laramide . The Nevadan orogeny emplaced the extensive batholiths of the Sierra Nevada . The regression of the Sundance Sea in the late Jurassic was accompanied by deposition of the Morrison Formation , notable for its vertebrate fossils. During Cretaceous times,

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1568-515: The core of the supercontinent . It was rotated approximately 90 degrees clockwise compared with its modern orientation, with East Antarctica and Australia to the north (what is now the west), Siberia to the east (present north), Baltica and Amazonia to the south (present east), and Congo to the southwest (present southeast). The Grenville orogen extended along the entire southwest (present southeast) margin of Laurentia, where it had collided with Congo, Amazonia, and Baltica. Laurentia lay along

1617-668: The craton. These included the North Slope of Alaska, which merged during the Early Devonian . Several small crust fragments accreted from the late Devonian through the Mesozoic to form the Western Cordillera. The Western Cordillera became a convergent plate margin during the Ordovician, and the Transcontinental Arch became submerged, only to reappear in the Devonian. The Devonian also saw the deposition of

1666-520: The equator. Recent evidence suggests that South America and Africa never quite joined to Rodinia, though they were located very close to it. Newer reconstructions place Laurentia closer to its present-day orientation, with East Antarctica and Australia to the west, South China to the northwest, Baltica to the east, and Amazonia and Rio de la Plata to the south. The breakup of Rodinia began by 780 Ma, when numerous mafic dike swarms were emplaced in western Laurentia. Early stages of rifting produced

1715-617: The equator. This ecological conclusion matches the previous paleomagnetic findings which confirms this equatorial location. At the end of the Cambrian, about 490 Mya, Avalonia rifted away from Gondwana. By the end of the Ordovician, Avalonia had merged with Baltica, and the two fused to Laurentia at the end of the Silurian (about 420 Ma) in the Caledonian orogeny . This produced the continent of Laurussia. During this time, several small continental fragments merged with other margins of

1764-527: The late Triassic. Pangaea reached its height about 250 Ma, at the start of the Triassic . The breakup of Pangaea began in the Triassic, with rifting along what is now the east coast of the U.S. that produced red beds , arkosic sandstone , and lake shale deposits. The central Atlantic ocean basin began opening at about 180 Ma. Florida, which had been a part of Gondwana before the assembly of Pangaea,

1813-652: The middle Silurian . During the early to middle Ordovician , several volcanic arcs collided with Laurentia along what is now the Atlantic coast of North America. This caused an episode of mountain-building called the Taconic orogeny . As the mountains raised by the Taconic orogeny were subsequently eroded, they produced the immense Queenston Delta , recorded in the rocks of the Queenston Formation . There

1862-471: The municipality and the chairperson of the municipal council. Here is a list of people who have held this position: Salangen (fjord) Salangen   ( Norwegian ) or Siellakvuotna   ( Northern Sami ) is a fjord in Salangen Municipality and Ibestad Municipality in Troms county, Norway . The 18-kilometre (11 mi) fjord flows to the northeast from

1911-538: The north. The highest point in the municipality is the 1,378.52-metre (4,522.7 ft) tall mountain Hjerttinden. The area itself is part of the Caledonian Orogeny formed of part of a series of Nappes that run down the coast of Norway. These nappes were metamorphosed as a result of partial subduction beneath Laurentia during the early to middle Paleozoic . On a smaller scale, the municipality

1960-626: The overlying sedimentary layers composed mostly of limestones , sandstones , and shales . These sedimentary rocks were largely deposited 650–290 Ma. The oldest bedrock, assigned to the Archean Slave , Rae , Hearne , Wyoming , Superior , and Nain Provinces, is located in the northern two thirds of Laurentia. During the Early Proterozoic they were covered by sediments, most of which has now been eroded away. Greenland

2009-745: The present Rocky Mountains into the Paleocene. The Western Cordillera continued to suffer tectonic deformation, including the formation of the Basin and Range Province in the middle Cenozoic and the uplift of the Colorado Plateau . The Colorado Plateau was uplifted with remarkably little deformation. The flood basalts of the Columbia Plateau also erupted during the Cenozoic. The southwestern portion of Laurentia consists of Precambrian basement rocks deformed by continental collisions. This area has been subjected to considerable rifting as

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2058-624: The southeastern margin of Laurentia, where there was a long-lived convergent plate boundary . Major accretion episodes included the Yavapai orogeny at 1.71 to 1.68 Gya, which welded the 1.8 to 1.7 Gya Yavapai province to Laurentia; the Mazatzal orogeny at 1.65 to 1.60 Gya, accreting the 1.71 to 1.65 Gya Mazatzal province; the Picuris orogeny at 1.49 to 1.45 Gya, which may have welded the 1.50 to 1.30 Gya Granite-Rhyolite province to Laurentia; and

2107-476: The southern margin of the craton. This long episode of accretion doubled the size of Laurentia but produced craton underlain by relatively weak, hydrous, and fertile (ripe for extraction of magma) mantle lithosphere. The subduction under the southeast margin of the continent likely caused enrichment of the lithospheric mantle beneath the orogenic belts of the Grenville Province . Around 1.1 Gya,

2156-666: The stable craton is exposed at the surface as the Canadian Shield , an area of Precambrian rock covering over a million square miles. This includes some of the oldest rock on Earth, such as the Archean rock of the Acasta Gneiss , which is 4.04 billion years ( Ga ) old, and the Istaq Gneiss Complex of Greenland, which is 3.8 Ga. When subsurface extensions are considered, the wider term Laurentian Shield

2205-544: The very end of the Proterozoic. This continent broke up again almost at once, and Laurentia rifted away from South America at around 565 Ma to once again become an isolated continent near the equator, separated from Gondwana by the western Iapetus Ocean . Sometime in the early Cambrian , around 530 Ma, Argentina rifted away from Laurentia and accreted onto Gondwana. The breakup of Pannotia produced six major continents: Laurentia, Baltica, Kazakhstania, Siberia, China, and Gondwana. Laurentia remained an independent continent until

2254-428: The work of the Schei Committee . On 1 January 1964, Lavangen Municipality (population: 1,677) and Salangen Municipality (population: 2,611) were merged to form a new, larger Salangen Municipality with a new population of 4,288. This merger was not popular and on 1 January 1977, it was mostly undone. Most of the old Lavangen Municipality (except for the Lavangsnes area) was separated from Salangen Municipality to form

2303-429: Was also violent volcanic activity, including the eruption that produced the Millburg/Big Bentonite ash bed. About 1,140 cubic kilometers (270 cu mi) of ash erupted in this event. However, this does not seem to have triggered any mass extinction. Throughout the early Paleozoic, Laurentia was characterized by a tectonically stable interior flooded by the seas, with marginal orogenic belts . An important feature

2352-457: Was left with Laurentia during the opening of the central Atlantic. This former Gondwana fragment includes the Carolina Slate belt and parts of Alabama. The Gulf of Mexico opened during the Late Triassic and Jurassic. This was accompanied by deposition of evaporite beds that later gave rise to salt domes that are important petroleum reservoirs today. Europe rifted away from North America between 140 and 120 Ma, and Laurentia once again became

2401-400: Was the Transcontinental Arch, which ran southwest from the lowlands of the Canadian Shield. The shield and the arch were the only portions of the continent that were above water through much of the early Paleozoic. There were two major marine transgressions (episodes of continental flooding) during the early Paleozoic, the Sauk and the Tippecanoe. During this time, the Western Cordillera was

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