Scandinavian Mountains in the context of "Carpathian Mountains"

Saana (Northern Sami: Sána) is a fell in Enontekiö, Finland. Saana's summit lies 1,029 metres (3,376 ft) above sea level and 556 m (1,824 ft) above the adjacent Kilpisjärvi lake. Geologically it is part of the Scandinavian Mountains, and is made of the same kinds of schist and gneiss rock. The peak is a popular destination for hikers and backpackers because of the sweeping views offered at the summit.

In December 2017, in celebration of the 100th anniversary of Finland's independence, Saana was lit with blue light. The area illuminated covered roughly 2.5 million square meters, making it the largest art illumination in the world.

Enontekiö (Finnish: [ˈenontekiø]; Northern Sami: Eanodat [ˈe̯anoðah(t)]; Swedish: Enontekis; Inari Sami: Iänudâh; Skolt Sami: Jeänõk) is a municipality in the Finnish part of Lapland with approximately 1,800 inhabitants. It is situated in the outermost northwest of the country and occupies a large and very sparsely populated area of about 8,400 square kilometres (3,200 sq mi) between the Swedish and Norwegian border. Finland's highest point, the Halti fell, with a height of 1,324 metres (4,344 ft) above the mean sea level, is situated in the north of Enontekiö. The municipality shares borders with regions of Sweden and Norway that encompass the Scandinavian Mountains. The administrative centre of Enontekiö is the village of Hetta. About one fifth of the community's population are Sami people. Enontekiö's main industries are tourism and reindeer husbandry.

U-shaped valleys, also called trough valleys or glacial troughs, are formed by the process of glaciation. They are characteristic of mountain glaciation in particular. They have a characteristic U shape in cross-section, with steep, straight sides and a flat or rounded bottom (by contrast, valleys carved by rivers tend to be V-shaped in cross-section). Glaciated valleys are formed when a glacier travels across and down a slope, carving the valley by the action of scouring. When the ice recedes or thaws, the valley remains, often littered with small boulders that were transported within the ice, called glacial till or glacial erratic.

Examples of U-shaped valleys are found in mountainous regions throughout the world including the Andes, Alps, Caucasus Mountains, Himalaya, Rocky Mountains, New Zealand and the Scandinavian Mountains. They are found also in other major European mountains including the Carpathian Mountains, the Pyrenees, the Rila and Pirin mountains in Bulgaria, and the Scottish Highlands. A classic glacial trough is in Glacier National Park in Montana, USA in which the St. Mary River runs. Another well-known U-shaped valley is the Nant Ffrancon valley in Snowdonia, Wales.

Kebnekaise (Swedish pronunciation: [kɛbnɛˈkâjsɛ]; from Sami Giebmegáisi or Giebnegáisi, "Cauldron Crest") is the highest mountain in Sweden. The Kebnekaise massif, which is part of the Scandinavian mountain range, has two main peaks. The glaciated southern peak used to be the highest at 2,120 metres (6,960 ft) above sea level, but has shrunk by 24 meters during the last 50 years, making the northern icefree peak at 2,096.8 metres (6,879 ft) the highest. Kebnekaise lies in Swedish Lapland, about 150 kilometres (93 mi) north of the Arctic Circle and west of Kiruna near the Kungsleden hiking trail between Abisko and Hemavan.

The Weichselian glaciation is the regional name for the Last Glacial Period in the northern parts of Europe. In the Alpine region it corresponds to the Würm glaciation. It was characterized by a large ice sheet (the Fennoscandian ice sheet) that spread out from the Scandinavian Mountains and extended as far as the east coast of Schleswig-Holstein, northern Poland and Northwest Russia. This glaciation is also known as the Weichselian ice age (German: Weichsel-Eiszeit), Vistulian glaciation, Weichsel or, less commonly, the Weichsel glaciation, Weichselian cold period (Weichsel-Kaltzeit), Weichselian glacial (Weichsel-Glazial), Weichselian Stage or, rarely, the Weichselian complex (Weichsel-Komplex).

In Northern Europe it was the youngest of the glacials of the Pleistocene ice age. The preceding warm period in this region was the Eemian interglacial. The last cold period began about 115,000 years ago and ended 11,700 years ago. Its end corresponds with the end of the Pleistocene epoch and the start of the Holocene. The German geologist Konrad Keilhack (de) (1858–1944) named it using the German name (Weichsel) of the Vistula (Polish: Wisła) in present-day Poland.

Jotunheimen (Norwegian pronunciation: [ˈjôːtʉnˌhæɪmn̩]; "the home of the Jötunn") is a mountainous area of roughly 3,500 square kilometres (1,400 sq mi) in southern Norway and is part of the long range known as the Scandinavian Mountains. The 29 highest mountains in Norway are all located in the Jotunheimen mountains, including the 2,469-metre (8,100 ft) tall mountain Galdhøpiggen (the highest point in Norway and Northern Europe). The Jotunheimen mountains straddle the border between Innlandet and Vestland counties (historically part of the old Oppland and Sogn og Fjordane counties).