The Rore Roundtrip

By the tourist office, cross the road at the traffic lights. Turn left, and continue along Pharos Vei. At the very end of Hoyvardeveien is the first hilltop: Vardeheia, 41 m a.s.l. Stunning views, and within an easy 10 min. walk from town centre. Enter Vestregate and then follow Storgaten until you reach Frivoldveien. The next hilltop is Floyheia, 63.5 m a.s.l., with beautiful views to the sea, town and countryside. This trail has been created based on Knut Hamsun’s work, “On Overgrown Paths”, and you’ll find quotes from the book along the way. Some steep sections, but Hamsun was 88 years old when he did this walk. Mollerheia, 41.9 m a.s.l., is the hilltop prior to the descent down to Kirkegaten. Cross over to Kirkeheia, 27 m a.s.l., with its beautiful park and the wooden Grimstad Church - Norway’s second largest of its kind. Binabben, 58.5 m a.s.l. and the last of the hilltops, offers an excellent “forest walk on wellkept paths to the vantage point. Spectacular 360° view towards countryside, town, harbour, archipelago and sea. At the top is a panorama disc with distances and details on what’s what in every direction. Duration: approx. 1 ½ hours. Terrain: Varied, some hilly areas, exciting countryside. Sturdy shoes and a reasonable level of fitness are required. Level of difficulty: Medium Suitable for: Both Vardeheia and Kirkeheia are suitable for wheelchairs/prams.

What is a smooth rocky shore? Cliffs and sandy beaches are very common, but the polished rocky shores are unique to Norway – almost. They do exist in other places, but not many. Stretches of such rock formations can be found from the Swedish west coast and up to Stockholm’s archipelago, and also in Greenland, Scotland, Alaska and possibly New Zealand. The rest of the world, however, does not have anything resembling these beautiful shores we associate with Southern Norway and the Oslo Fjord. The reason is that not many areas fulfil the two conditions required for such polished, smooth rocks to be formed. High-grade metamorphic rock such as gneiss or granite is required, and this coarse-grained formation must have been scoured and rubbed smooth by a thick layer of ice. As old as time itself! The Norwegian rocky shores originated long before the ice arrived - maybe as much as a billion years. Formation started 1.8 billion years ago and ended 1200 million years later. The time-span is almost incomprehensible! When the ice retreated for the last time, the rocky shores were given a last finish and took their current shape. This is only 10 000 years ago. Since then, the land has risen as much as 200 metres in some areas. Hence, the rocky shorescurrently lining the water’s edge were far below sea level and a thousand metres or more under the ice when they were formed. As the ice moved, masses of sand, gravel and stone were pushed in front and below. These deposits were pressed down and rubbed against the bedrock with immense force. This was how Norway’s rocky shores were formed. Soft elements were scoured away, and the hard rock was left polished, smooth and rounded. In several areas, characteristic scour lines are still evident, and some cracks in the actual bedrock can also be seen.

From the tourist office, followSmith Petersens Gate towards Arendal. Continue past Grimstad Church and Grimstad Town Hall on the left, and follow the foot and cycle path across Biesletta. Cross the road by the Bieheia turn-off, and continue along the foot and cycle path on the right hand side until you reach Vikkilen. Follow the signs for Fevik. At the Vik junction, turn right and follow the foot and cycle path along route 420 towards Fevik. When you reach the 40 km/h zone, cross the road and continue along the foot and cycle path on the left hand side. After a few kilometres, where you have open views to the sea, you can see the idyllic Strand Hotel Fevik. At the very tip of the headland is Sandodden Fort. Cross over to the right hand side and follow the pavement to Fevik. Turn right at Feviktoppen, and then take the second right. Feviktoppen has a small shopping centre. Continue past Fevik Park on your left and Fevik Church Community Centre on your right. Follow the signs for Som/Haugenes. Somsveien towards Hasseltangen does not have a foot and cycle path. An alternative route is marked in blue. Please see recommended trip below. After the Haugenes junction, continue straight ahead until your reach Hasseltangen. To get to the outermost part of Hassel-tangen, follow the gravel road to the left at the very end of the car park. On your return, turn right towards Birketveit at the first junction. At the route 420 junction, turn left towards Fevik. When you have passed a riding school on your left, cross the road and follow the signs for Lunde. At the end of the road is a T-junction where you turn left towards Lia. Continue straight ahead until you reach the foot and cycle path, and follow this towards Vik/Grimstad. Just before the Vik junction, use the pedestrian crossing to get over to the right hand side and then follow the foot and cycle path underneath route 420. From here, follow the foot and cycle path back to Grimstad. Opt. 1: Turn right towards Storesand, and continue past Randvika. In the upper part of the car park, bear left and follow the main road until you reach Haugenes junction. Then turn right towards Hasseltangen. Comments: Mainly flat and gentle terrain, but parts of the trip do not follow foot and cycle paths. Some gravel roads.