Speilsalen
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Speilsalen
Speilsalen (The Hall of Mirrors) was a natural glacial formation caused by a river underneath a glacier in the Trollheimen mountains in the municipality of Oppdal in Trøndelag county, Norway. It was located at the northeast base of the mountain Blåhøa : ''For the mountain peak Blåhøi in Innlandet, Norway, see Blåhøi.'' : Blåhøa (or ''Blåhø'') is a mountain in the municipality of Oppdal in Trøndelag county, Norway. It is the highest mountain at the northeastern side of the Trollheimen m .... Under favourable conditions late summer, it was possible to walk the from one end to the other underneath the glacier. It was never considered safe to walk under a glacier. Speilsalen collapsed in August 2007. References External links Article with pictures from glaciers in Trollheimen Glaciers of Norway Oppdal Landforms of Trøndelag Former landforms Ice caves {{norway-glacier-stub ...
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Trollheimen
Trollheimen is a mountain range in Møre og Romsdal and Trøndelag counties in central Norway. The mountain range is part of the Scandinavian Mountains. Etymology The name ('the home of the trolls') was proposed by Håkon Løken and used by Trondhjems Turistforening in the 1880s, and is considered a "tourist name" (there was no single name for the entire area before). Trollheimen is now the common name in Norway for this mountain range. Topography and climate Trollheimen is often considered the most varied of all mountain ranges in Norway for several reasons. The mountains in the western part are alpine in form, with pointed peaks and typical river valleys. The mountains in the east are less steep with more rounded shapes predominating, and the valleys are wider and bear the mark of being created by glaciers. The climate differs from the more oceanic climate in the west to a considerably drier, continental climate in the eastern valleys, due to their being sheltered by mounta ...
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Oppdal
is a municipality in Trøndelag county, Norway. It is part of the Dovre region and the traditional district of Orkdalen. The administrative centre of the municipality is the village of Oppdal. Other villages in the municipality include Lønset, Vognillan, Fagerhaug, and Holan. The Oppdal Airport, Fagerhaug is located in the northeastern part of the municipality. The municipality is the 24th largest by area out of the 356 municipalities in Norway. Oppdal is the 139th most populous municipality in Norway with a population of 7,066. The municipality's population density is and its population has increased by 4.6% over the previous 10-year period. General information The prestegjeld of Oppdal was established as a municipality on 1 January 1838 (see formannskapsdistrikt law). The municipal boundaries have not changed since that time. On 1 January 2018, the municipality switched from the old Sør-Trøndelag county to the new Trøndelag county. Name The municipality (originally ...
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Blåhøa
: ''For the mountain peak Blåhøi in Innlandet, Norway, see Blåhøi.'' : Blåhøa (or ''Blåhø'') is a mountain in the municipality of Oppdal in Trøndelag county, Norway. It is the highest mountain at the northeastern side of the Trollheimen mountain range. The mountain is located in the northwestern part of the municipality of Oppdal, about north of the lake Gjevillvatnet, about west of Nerskogen (in Rennebu), and about northwest of Vognillan. The tall mountain has a topographic prominence of . The Speilsalen glacial tunnel was located about northeast of the peak. Name The first element is ''blå'' which means "blue Blue is one of the three primary colours in the RYB colour model (traditional colour theory), as well as in the RGB (additive) colour model. It lies between violet and cyan on the spectrum of visible light. The eye perceives blue when obs ...", and the last element is ''hø(a)'' which means a "large and round mountain". References Oppdal Mo ...
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Glacier
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its Ablation#Glaciology, ablation over many years, often Century, centuries. It acquires distinguishing features, such as Crevasse, crevasses and Serac, seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between lati ...
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Trøndelag
Trøndelag (; sma, Trööndelage) is a county in the central part of Norway. It was created in 1687, then named Trondhjem County ( no, Trondhjems Amt); in 1804 the county was split into Nord-Trøndelag and Sør-Trøndelag by the King of Denmark-Norway, and the counties were reunited in 2018 after a vote of the two counties in 2016. The largest city in Trøndelag is the city of Trondheim. The administrative centre is Steinkjer, while Trondheim functions as the office of the county mayor. Both cities serve the office of the county governor; however, Steinkjer houses the main functions. Trøndelag county and the neighbouring Møre og Romsdal county together form what is known as Central Norway. A person from Trøndelag is called a ''trønder''. The dialect spoken in the area, trøndersk, is characterized by dropping out most vowel endings; see apocope. Trøndelag is one of the most fertile regions of Norway, with large agricultural output. The majority of the production ends ...
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Norway
Norway, officially the Kingdom of Norway, is a Nordic country in Northern Europe, the mainland territory of which comprises the western and northernmost portion of the Scandinavian Peninsula. The remote Arctic island of Jan Mayen and the archipelago of Svalbard also form part of Norway. Bouvet Island, located in the Subantarctic, is a dependency of Norway; it also lays claims to the Antarctic territories of Peter I Island and Queen Maud Land. The capital and largest city in Norway is Oslo. Norway has a total area of and had a population of 5,425,270 in January 2022. The country shares a long eastern border with Sweden at a length of . It is bordered by Finland and Russia to the northeast and the Skagerrak strait to the south, on the other side of which are Denmark and the United Kingdom. Norway has an extensive coastline, facing the North Atlantic Ocean and the Barents Sea. The maritime influence dominates Norway's climate, with mild lowland temperatures on the se ...
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Glaciers Of Norway
These are the largest glaciers on mainland Norway.The largest glaciers in Norway
(page 51, Accessed on July 29, 2014)
However, the 18 largest glaciers in the Kingdom of Norway are on , including the second largest in Europe, on

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Landforms Of Trøndelag
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fo ...
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Former Landforms
A former is an object, such as a template, gauge or cutting die, which is used to form something such as a boat's hull. Typically, a former gives shape to a structure that may have complex curvature. A former may become an integral part of the finished structure, as in an aircraft fuselage, or it may be removable, being using in the construction process and then discarded or re-used. Aircraft formers Formers are used in the construction of aircraft fuselage, of which a typical fuselage has a series from the nose to the empennage, typically perpendicular to the longitudinal axis of the aircraft. The primary purpose of formers is to establish the shape of the fuselage and reduce the column length of stringers to prevent instability. Formers are typically attached to longerons, which support the skin of the aircraft. The "former-and-longeron" technique (also called stations and stringers) was adopted from boat construction, and was typical of light aircraft built until the ...
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