Kamperöd: Archaeological Traces and Nature
Accommodation in Kamperöd
If you want to consider archaeological traces in the landscape and connections with nature when choosing a destination, Kamperöd offers two clearly identifiable themes: burial mounds and finds on the one hand, and the Rotviksbäcken, with its historical and ecological connections, on the other. This makes the area interesting for planning a trip that takes account not only of an individual monument, but also of its surroundings. The different aspects also help you view the area’s history through its landscape and waterways.
Burial mounds and early traces in the landscape
The large burial mound Skredsvik 21 is located near Kamperöd, on a moraine terrace beside Granhogen farm. Granhogen is also home to one of Bohuslän’s largest burial mounds. In the Kamperöd–Granhogen area, finds point to the landscape having been used as early as the Stone Age. Most of the area’s prehistoric finds are concentrated on the southern slope toward the farms of Hogane and Granhogen.
The findspots highlight different spatial scales: Skredsvik 21 is identified as an individual mound beside Granhogen, while the concentration of finds on the southern slope provides a broader point of reference. The Kamperöd–Granhogen cultural landscape also includes part of Kamperöd in Skredsvik. For your selection, this means you can focus on a named monument, the wider distribution of finds, or the cultural landscape, without conflating these different levels.
The dates also highlight different periods. The finds point to the landscape having been used as early as the Stone Age; the remains of the old Skvaltkvarnen mill date from the 1520s. The early finds and the mill remains therefore belong to different historical periods. This time gap helps you place Kamperöd’s various traces in context.
Rotviksbäcken: Nature and milling history
The Rotviksbäcken offers a different perspective. The stream begins in Kamperöd and flows into the Havstensfjorden–Svältekile Natura 2000 site and nature reserve. Sea trout swim up the Rotviksbäcken to spawn. This connects the stream’s course with a protected area and the fish’s spawning migration.
Rövargrottan lies below the rock formation Kamperöds Horn. Remains of the old Skvaltkvarnen mill, dating from the 1520s, can be seen at the small waterfall in the lower reaches of the Rotviksbäcken. Three millstones and a small stone wall can also be seen west of the Rotviksbäcken. The cave, stream and mill remains offer a different focus from the burial mounds: here, rock, flowing water and historical use take centre stage.
The stream thus has two distinct connections: the sea trout’s spawning migration draws attention to its ecological aspect, while the mill remains point to the historical use of the water. Together with Rövargrottan, they offer different themes related to the stream and rock, while the burial mounds form a distinct archaeological focus.
Route information for planning
Västtrafik bus route 841 runs between Lysekil, Torp and Göteborg. Route details may change, so check the current timetable before travelling.
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Go to the main travel overview: Uddevalla.