A country · 334 places · 23 regions
Norway, all of it.
334 curated places across 23 regions — photographed, mapped, and noted with the season each is best in.
The 4 biggest regions — Oslo Municipality, Nordland, Hordaland and Sogn og Fjordane — read below as chapters, with 19 more waiting past them.
Chapter I · Oslo Municipality · 37 places
Oslo Municipality
The capital and most populous city of Norway, situated at the head of the Oslofjord in the southeastern corner of the country. The city centre is compact and walkable, organised around a main axis connecting the Central Station to the Royal Palace through Karl Johans gate. Major cultural landmarks include the National Gallery, the Vigeland Sculpture Park, and the Akershus Fortress, while the waterfront redevelopment around Tjuvholmen and Aker Brygge has reshaped the harbour zone.
via Wikimedia CommonsChapter II · Nordland · 33 places
Nordland
Reine is the administrative centre of Moskenes Municipality in Nordland county, on the island of Moskenesøya near the outer end of the Lofoten archipelago, well above the Arctic Circle and about 300 kilometres south-west of Tromsø. The village covers barely 0.28 square kilometres and had a population of 297 in 2023. It occupies a low spit of land inside a sheltered bay, with the granite spires of Olstinden and Reinebringen rising almost vertically behind it out of shallow, unusually pale water. The colour is not a trick of processing: the beaches here are ground shell and quartz sand, and in flat light the bay turns turquoise even at five degrees Celsius. The fishing village it still is. Reine was granted trading rights in 1743 and grew on the winter cod fishery, when spawning skrei arrive off Lofoten between January and April. The red and ochre timber cabins standing on stilts over the water are rorbuer, seasonal quarters built for visiting fishermen; most now let to travellers, but the fishery has not stopped. Wooden drying racks, the hjell, still fill the flats around the village from February onwards, hung with split cod that air-dries into stockfish over several months. That trade is the oldest continuous export business in Norway and the reason places like Reine exist at all; a substantial share still goes to Italy and Nigeria. On screen, precisely. Lofoten is the Norway that appears in Alexander Payne's Downsizing from 2017, where the miniaturised colony is set in a fjord landscape. The Norwegian unit worked in the archipelago and in Bergen, and the fjord sequences were shot at Trollfjord, a narrow inlet off the Raftsundet strait some distance north-east of here, rather than at Reine itself. It is worth being exact about that, because Reine's image circulates constantly and is often captioned with productions that never came near it. What Reine genuinely is, on the visual side, is one of the most photographed villages in Europe, and a fixture of tourism campaigns, stills libraries and aerial reels rather than of feature drama. The climb everyone makes. Reinebringen, at 448 metres, gives the view that defines the place: the village, its bay and the surrounding peaks laid out below in a single frame. The old path up was a notorious mudslide that caused repeated injuries, and between 2015 and 2019 Nepalese Sherpa crews built a stone staircase of roughly 1,500 steps up the flank. It is still steep, still exposed near the top, and closed periodically for avalanche or rockfall risk in winter and spring. The round trip takes two to three hours. Lower and gentler alternatives exist: the walk to Bunes beach from Vindstad, reached by the small ferry across Kjerkfjorden, ends at a wide sand beach beneath a 700-metre rock wall. The water off the point. South-west of Moskenesøya lies the Moskstraumen, the tidal current between the island and Værøy that gave European literature its maelstrom. Olaus Magnus described it in the sixteenth century, and Edgar Allan Poe, Jules Verne and Herman Melville all built on the legend. The real phenomenon is a strong tidal race generated by water forced between shallow banks, spectacular in the right combination of tide and wind and unremarkable otherwise. Boat operators from Reine and Å run trips towards it in settled weather. What is actually there today. The village is small: a church, a school, a couple of cafés, a gallery in a converted fish factory, and the ferry quay for the Kjerkfjorden crossing. Neighbouring Sakrisøy, on the same road, has yellow-painted cabins and a fish market; Hamnøy has the bridge that provides the standard photograph of red cabins against the mountain. The E10, King Olav V's road, links them all and ends 12 kilometres further on at the village of Å, where the Norwegian Fishing Village Museum preserves a working cod-liver-oil plant. The road between these villages threads a chain of bridges and short tunnels built from the 1960s onward; before it existed, every one of these settlements was a boat community, which explains why they sit where they do rather than where a road engineer would have put them. Getting there and timing. Leknes and Svolvær have airports with connections through Bodø; a car ferry runs Bodø to Moskenes in three to four hours, and the E10 reaches Lofoten by road from Narvik. Midnight sun runs from late May to mid-July, when the light never fully leaves and photography continues all night. The polar night lasts from early December to early January, and the northern lights are realistically visible from late September to March. Winter driving is serious, with wind rather than snow depth the main problem, and accommodation prices in the rorbuer peak in both July and the aurora months. The islands have absorbed a steep rise in visitors over the past decade, and parking, waste and access to private land around the best-known viewpoints are live local issues, so pulling off the E10 at a marked passing place rather than on a verge is more than a courtesy.
✦ February to March for aurora; June to August for midnight sun · $$
Chapter III · Hordaland · 32 places
Hordaland
Trolltunga is a horizontal shelf of gneiss projecting from a mountainside in Ullensvang Municipality, Vestland, at 1,126 metres above sea level and roughly 700 metres above the surface of the lake Ringedalsvatnet. The slab is a few metres long and a couple of metres wide, with nothing beneath it, which is the entire reason for its fame. The name translates as the troll's tongue. It lies inland from the Sørfjord, an arm of the Hardangerfjord, above the industrial village of Tyssedal and the town of Odda, in a landscape shaped as much by hydroelectric engineering as by ice. How the rock got there. The shelf is a product of frost and ice rather than erosion by water. During glaciation, ice exploited horizontal joints in the bedrock and plucked away the material below the slab, leaving a resistant layer cantilevered over the void; freeze-thaw cycles since then have widened the fractures. The same geology explains why the surrounding plateau is a patchwork of bare rock, shallow tarns and scoured hollows. Ringedalsvatnet below is dammed: the Ringedalsdammen, built in the early twentieth century, was for a time the largest dry-stone dam in Europe, and it fed the Tyssedal power station that turned this remote valley into one of Norway's first heavy-industry sites. A modern phenomenon, not an old one. Trolltunga was barely visited until the smartphone era. Fewer than 800 people made the hike in a typical year before 2010. By 2016 the figure had passed 80,000, driven almost entirely by a single photographic composition circulating on social platforms. That growth arrived faster than the infrastructure: rescue callouts multiplied, and the municipality and Red Cross now run an active safety presence in season. It is one of the clearest cases anywhere of an image creating a destination. The rock itself has no film credit and no literary history worth the name; its fame is purely a function of how it photographs, which is an honest thing to say about it. What the hike involves. The standard route runs 27 kilometres round trip from Skjeggedal with roughly 800 metres of ascent from the upper car park, and takes most people between eight and twelve hours. There is no shelter, no water sold on the route and no mobile coverage in places. Two emergency cabins stand along the trail. Three car parks sit at different heights, with the highest, P3, cutting several kilometres and a stiff climb from the total; access to it is regulated and paid. The terrain is rock, bog and snow patch rather than groomed path, and the weather on the plateau changes faster than the valley suggests. What is actually there at the end. A queue, in high summer. The tongue accommodates one group at a time, and waits of an hour or more are normal in July and August; a marshal is often present to keep the line orderly. There is no railing and no barrier, and the exposure is absolute. Away from the slab itself, the plateau rewards a longer look: the view runs down the length of Ringedalsvatnet, the water an opaque glacial green, with the Folgefonna icecap visible to the west on a clear day. Many walkers camp on the plateau to reach the rock at dawn, which is both the quietest hour and the best light. Norway's right of public access permits wild camping on uncultivated land, and in high summer a scatter of tents appears along the last kilometres of the route. Season and conditions. The unguided season runs roughly from mid-June to mid-September, depending on snow. Outside it, a guide and winter equipment are strongly advised and in practice required by the local authorities' guidance, since the route crosses ground that holds cornices and hides the trail entirely under snow. Snow can linger on the plateau into July. Fog is the most common hazard, not cold: the marked route is easy to lose in cloud, and the drop is unforgiving. Sturdy boots, layers, headlamp, two litres of water and real food are the baseline, and turning back early is a normal outcome rather than a failure. Getting there and the wider valley. Odda is about three hours by road from Bergen and roughly six from Oslo, with bus connections in summer; from Odda a shuttle runs to the Skjeggedal trailhead in season. The valley repays a second day. Tyssedal's power station of 1906 to 1918 is preserved as the Norwegian Museum of Hydropower and Industry, and the Buerbreen arm of the Folgefonna glacier lies a short drive south. Låtefossen, a twin waterfall dropping beside the road north of Odda, is one of the most photographed roadside cascades in the country. Accommodation concentrates in Odda and Tyssedal and fills months ahead for July weekends. Odda has changed character quickly: it was a smelter town whose carbide and zinc works defined it for a century, and the transition from industry to hiking traffic has been abrupt enough to remain visible in the streetscape, with workers' housing and plant buildings sitting directly beside outdoor outfitters.
via Wikimedia CommonsChapter IV · Sogn og Fjordane · 29 places
Sogn og Fjordane
The Nærøyfjord runs about 17 kilometres through Aurland Municipality in Vestland county, a branch of the Aurlandsfjord which is in turn a branch of the Sognefjord, Norway's longest at over 200 kilometres. At its tightest the channel narrows to roughly 250 metres of navigable water, while the summits on either side stand around three kilometres apart and reach some 1,760 metres. That ratio, a fjord narrower than the height of the walls above it, is what makes the passage feel less like sailing and more like moving down a corridor. The village of Gudvangen sits at the inner end where the Nærøydalselvi river arrives from the Nærøydalen valley; the hamlets of Bakka, Dyrdal and Styvi cling to the shore further out. Why it is protected. In 2005 UNESCO inscribed the Nærøyfjord alongside the Geirangerfjord as the West Norwegian Fjords, citing them as among the most spectacular examples of the classic fjord landscape anywhere on earth. The listing covers not only the water but the terraces of small farms above it, several of them abandoned in the twentieth century, and the transport routes that served them. Styvi still holds a stretch of the old postal road, a footpath that carried mail along the shoreline in winter when the fjord froze or the boats could not run. Those farms explain the odd green shelves visible halfway up otherwise vertical rock: they were mown and grazed for centuries, and several are now maintained as heritage landscapes. On screen and off it. The Sognefjord system, and the Nærøyfjord in particular, is repeatedly named among the Norwegian landscapes that Disney's art team studied on its 2012 research trip before building the world of Frozen. As with the rest of that film, nothing was photographed here: Frozen is animation, and the trip produced reference material rather than footage. What the fjord does supply to filmmakers directly is aerial and second-unit work; its shape is unmistakable from the air, and it turns up in documentary and commercial photography far more often than in drama. The honest headline is that the Nærøyfjord is a landscape that has been drawn from more than it has been shot in. What is actually there today. The standard passage is the ferry between Flåm and Gudvangen, about two hours, and since 2018 it has been run in part by battery-electric vessels built specifically for the World Heritage water. From Gudvangen the reconstructed Viking settlement of Njardarheimr, opened in 2017, occupies the flat ground at the fjord head, staffed year-round rather than seasonally. Kayak operators run guided paddles from both ends, which is the only way to appreciate the scale honestly, since a 1,700-metre wall reads as merely large from a ferry deck and as absurd from a boat sitting 30 centimetres above the water. Undredal, on the Aurlandsfjord side, has a white timber church from 1147 seating about 40 people and a long tradition of brown goat cheese; until a road reached it in 1988 the village was accessible only by boat, and the goats still outnumber the residents. Bakka, halfway along the Nærøyfjord, holds a small white church of 1859 and a handful of houses on the only flat ground for kilometres, a reminder that this water was a road long before it was a view. The approach from above. The valley behind Gudvangen climbs to Stalheim, where the hotel terrace gives one of the most reproduced views in the country: the Nærøydalen valley falling away between two rock faces. The old Stalheimskleiva road, a chain of thirteen hairpins built in the nineteenth century with gradients around eighteen per cent, drops from the plateau to the valley floor and has been subject to closures in recent years because of rockfall risk, so its status is worth checking before planning to drive it. The alternative is the E16 with its tunnels, faster and far less interesting. Getting there and timing. Flåm is the practical base, reached by the Flåm Railway, a 20-kilometre branch line from Myrdal on the Bergen–Oslo route that climbs roughly 865 metres with a gradient of one in eighteen over much of its length. Bergen is about two and a half hours away by road, Oslo around five. High season runs from late May to early September, when the ferries are frequent and the valley floors are green; the shoulder weeks in May and late September are quieter and the waterfalls still run hard. Winter brings the strangest version of the fjord, with black water, snow to the shoreline and daylight that never rises far above the ridgeline; the Flåm–Gudvangen sailings run on a reduced timetable, and February and March often deliver the stillest water of the year. The combined rail, boat and bus circuit marketed as Norway in a Nutshell packages the whole sequence in a day from Bergen or Oslo, which is efficient but leaves no time on the water beyond the crossing itself.
✦ May to September · $$
Regions of Norway
Every place in Norway
