***  SWEDEN  2016   -  WEEKS 7~8  ***

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CAMPING IN SWEDEN 2016 - across the Arctic Circle to Jokkmokk, Kvikkjokk, WW2 Lancaster Easy Elsie crash site, Porjus and Lulea River HEP dams, iron ore town of Kiruna, Sweden's northernmost village Karesuando, border with Finland along Tornedalen valley, Pajala, re-cross Arctic Circle south at Överkalix, Älvsbyn, Piteälven valley and Storforsen rapids:

North across the Arctic Circle (again):  after leaving Moskosel northwards, E45 Inlandsvägen crossed the wide, fast-flowing Piteälven river, a white-water torrent even in the dry season; we did not stop today since we should see the Piteälven later in the trip at Storforsen rapids. The road meandered generally northwards through magnificent spruce forested terrain, with even more spectacular distant views to northern fell-land hills (click here for detailed map of route). The sheer scale of this forested fell-scape offset the apparent monotony of the endless sea of trees (see left). The Inlandsbanan railway had strayed away from the road, its route determined by the practical difficulties of overcoming natural obstacles of marshland and rivers, but re-crossed the E45 at the villages of Kåbdalis and Tarrajaur.

Click on 7 highlighted areas of map
for details of Arctic Sweden

Some 6kms south of Jokkmokk, we pulled into the lay-by which marked the notional line of 66º-33' N, the Arctic Circle (Polcirceln in Swedish, Napapiiri in Finnish) (Photo 1 - Crossing Arctic Circle), our second northward crossing of the Line this trip (see left). An information panel described how the earth's angle of tilt causes the Arctic Circle's movement. Defined as the southernmost latitude in the Northern Hemisphere at which the Midnight Sun can be seen on the night of the Summer Solstice, the Arctic Circle moves north and southwards across an area of 180 kms over a period of 40,000 years; it will reach its northernmost position in the year 12,000, returning to its current position in AD 22,000 and reaching its southernmost line in 32,000 and continuing to cycle north and south thereafter if you care to hang around to witness this curious phenomenon. After a pause for lunch sandwiches and photos, we continued into Jokkmokk.

Jokkmokk Fjällträdgård Botanic Gardens:  Jokkmokk takes its name in the Sámi language from its position on a bend in the Luleälven river. The surrounding municipality through which the river runs covers an area the size of Wales but with a population of just 3,000. On his expedition through Lapland in 1732, Carl von Linné, the Swedish botanist, likened it to an earthly paradise were it not for the midges. Along Jokkmokk's main street of Storgatan, we turned down to the Botanic Gardens which display the wild flora of Norbotten province's fells and mountains. Set along sheltered embankments each side of a brook which tumbles from a small lake, the gardens are divided into sections representing the different types of terrain, with the flora of each growing in semi-wild conditions. We began at the high fell-land plants which had to survive winter snows: they were an exact reproduction of the berry plants we had seen yesterday: Lingonberry, Bilberry, Bog Bilberry, Crowberry and Cloudberry. None of course were in flower at this time of year, and the berries had not yet formed. The next section was devoted to plants of the Taiga coniferous forest belt, and included the 3 types of lichen which in winter the reindeer forage for under snow covering (see left). When we had last visited the Botanic Gardens, we had been impressed with their content and layout, but this year being later in the season, plants were past flowering and the beds devoted to meadow birch forests and cold springs were totally overgrown. Parts on the rocky slopes across the brook were in process of reconstruction, but fortunately the higher south-facing slopes of Lingonberries remained intact and were covered with ripening berries (Photo 2 - Ripening Lingonberries). The upper sections with mountain heath-land plants seemed better cared for and well labelled with both common names and Latin binomials, which enabled our identification of White Arctic Mountain Heather (Cassiope tetragona), previously unknown to us and resembling club moss with tiny white flowers now past. There were masses of Mountain Avens, the flowers also now past but with wispy seed heads (see right), and beautiful specimens of Northern Wolfsbane (Photo 3 - Northern Wolfsbane) This year had been a rather disappointing visit, partly due to the late time of the season but also the rather neglected state of parts of the Gardens.

Skabram Camping at Jokkmokk and frustrating weather change:  we camped that night at Skabram Camping, a small and hospitable site just west of Jokkmokk kept by an ex-pat Dutch couple; it is clustered around the yard of a cheese farm whose products are on sale at reception, with chickens clucking around the camping area. The campsite at this time of year filled up with mainly Dutch and German holiday-makers, but our pitch was carefully chosen to give us a secluded corner to avoid the inevitable noise. The sun remained bright for our barbecue supper, and we sat out late into the evening with Moon Tigers burning on the table to deter mossies, looking out into a clearing in the surrounding pine forest towards the setting sun (see below right).

After overnight rain, the following day the sky was heavily overcast; it looked as if the forecast change in the weather had begun. A morning in camp ended with an hour-long thunderstorm with constantly rumbling thunder and pouring rain, delaying our afternoon in Jokkmokk. Shopping for provisions in the town's poorly stocked ICA and Coop-Konsum was a depressing experience; it needed both supermarkets to secure 3 day's stock of supplies. Round to the Tourist Information in another downpour, the bright and fluent Americanese-speaking young lass reassured us on the state of the road out to Kvikkjokk, but on checking the weather using their wi-fi internet, the forecast for the week ahead showed a depressingly gloomy period of rain covering the north as far as Karesuando. Down at Jokkmokk railway station, we found the monument to the royal opening in 1937 of the final stretch of the Inlandsbanan up to Gällivare (see left), but with the rain still pouring there was nothing for it but to return to camp at Skabram after a frustrating afternoon of weather. The cloud just about managed to break to give a wanly hazy evening sun which declined into a gap in the pine trees. This looked like being the last chance of a barbecue for a while with the worsening weather

The road's-end settlement of Kvikkjokk in the mountainous interior:  before continuing north, our plan was to make a foray out to Kvikkjokk, an isolated settlement 120kms into the interior towards the mountainous Sarek National Park. Encouraging advice from the TIC and a neighbouring German camper was that the lane leading out to Kvikkjokk, although in poor state, was asphalt all the way, with a small campsite at Årrenjarke 17kms from road's-end at Kvikkjokk; this was a staging point on the Kungsleden long distance wilderness trekking route part-way between Jäkkvik where we had camped last week and Abisko in the north. With drizzly rain falling, we finally headed north from Jokkmokk, and just across the Akkats dam, turned off onto Route 805, the minor road which followed the scattered course of the Lille Luleälven water system network (click here for detailed map of route) out to its end at remote Kvikkjokk. The rain was by now increasing, sky sullenly grey, and the distant mountains lost in low, misty rain cloud. Although tarmaced, the road was bumpy and uneven, meandering every-which-way westwards through deserted forests and passing only the occasional Sámi farmstead, and one lone and bedraggled reindeer. The entire length of the valley was a network of lakes which formed the Lille Luleälven water system, with intervening marshland, forests and extensive boulder-fields, an uninhabited landscape virtually unchanged since the retreat of the Ice Age glaciers, and looking even more desolate in such dreary weather. It was text book post-glacial terrain, if only we could have seen it in the misty, murky rain. With the bumpy, broken road surface, the 120km drive our to Kvikkjokk took us almost 2 hours, mile after endless, misty mile alongside lakes and marshes, through forests and boulder-fields.

After some 80kms the road surface improved, and we were able to make better progress eventually to reach the hut settlement and camping of Årrenjarke, tucked in a forested bay at the innermost large lake of Saggat. We investigated the tiny campsite which was nestled on a hillock-peninsula by an inlet looking south-eastwards along the entire length of the lake. Despite the still gloomy weather, the rain had now virtually stopped, and we reserved the prime pitch on the crest of the hillock at this magnificent setting with its outlook along the length of the lake and view of the distinctive ridge-end peak of Kasssavare (957m) with its sheer-sided summit cliffs reflected in the lake's still waters (see above right) (Photo 4 - Reflections in Saggat lake). The main valley road crossed a high shoulder of forested land to run along a well-engineered shelf immediately above the Saggat lake's waterline and along to the outskirts of Kvikkjokk. Other than the settlement being at road's-end and a staging point on the Kungsleden long-distance wilderness path, we had no idea what to expect of Kvikkjokk. On entering the settlement, a faded sign pointed down towards the lake, ending at a rough parking area, with a superb distant view of another distinctive sheer-sided peak, Tarrekaize (1824m) (see above left) (Photo 5 - Approaching Kvikkjokk). A little further and we reached the Kvikkjokk Turist-service building, closed and semi-derelict, with a notice on the locked door Stängd till nästa Fredag (Closed till next Friday); this seemed to summarize Kvikkjokk. Despite its isolation, a regular bus service still served the village, and several back-packers were waiting at the bus stop by the church. Lanes led up to a rough camping area and the Kvikkjokk Mountain Station hostel, both serving Kungsleden back-packers. The scattering of houses around the small shingled wooden church seemed partially occupied, but it would be a tough existence up here in the depths of winter. The car park literally at road's-end was quite full, presumably belonging to walkers out in these remote fells. Two major rivers flowed down from the westward desolate high mountains of Sarek National Park, the Kamajokk and Tarraätno, merging to form a delta as they flowed into Saggat lake, the source of the Lille Luleälven chain of lakes which finally flowed into the Stora Luleälven at Vuollerin. But for all its isolated setting, Kvikkjokk was something of a bleak and cheerless place, and its tourist service doubtless would remain stängd for many a nästa Fredag to come. Unless you were walking the Kungsleden and making a staging camp here, Kvikkjokk had little in itself to commend it other than its isolated setting amid such glorious mountainous solitude.

Årrenjarke Fjällby-Camping near to Kvikkjokk:  the weather increasingly brightened as we drove back alongside Saggat lake; after this morning's gloomy rain and solid, misty cloud, the forecast for brighter weather and even for clear sun later in the afternoon scarcely seemed credible. But in fact the cloud was now breaking and sun beginning to shine through. Back at Årrenjarke Fjällby-Camping, we called in at reception to book in; as expected, the price for camping was as expensive as the setting was attractive: 265kr, when at other northern campsites we had been used to paying 200kr at most. Our questioning such expensive prices was greeted with just a take-it-or-leave-it shrug. We acquiesced, and with some difficulty level-pitched George on the sloping, rocky, tree-root ridden ridge crest, and settled in (Photo 6 - Årrenjarke Fjällby-Camping), with Lingonberries growing in profusion around our pitch (see above left). By now the sun had fully broken through with a clear sun shining down through the pines, exactly as forecast. This was as gloriously located and peaceful a camping spot as you could ask for, looking down the length of Saggat lake from the pine-covered hillock (see above left); we sat revelling in the magnificent setting with mountains and trees reflected in the lake. We woke the following morning to a cloud-dappled sky, all reflected and sparking amid the pine woods in the lake's still waters (see left) (Photo 7 - Morning sun sparkling in Saggat lake). The beautiful morning light reinforced the magnificence of our camp spot setting (see above left and right). Although expensive, Årrenjarke Fjällby-Camping would probably be one of the trip's most memorable camping locations; it had been worth the long drive out to this isolated spot.

Return along Lille Luleälven valley to Inlandsvägen we set off on the 90km return drive on the single-track lane along the Lille Luleälven valley. Despite the rough road surface, the morning sun and clear blue sky made this drive a sheer delight compared with the gloomily wet drive out yesterday. The sun lit the road-side spruces and forest-covered hills, and the series of lakes reflected the clear sky and blotchy cloud-scape (see right) (Photo 8 - Lille Luleälven cloud-scape). We passed a lone buck reindeer grazing in the road-side forest, with the indignity of a collar and bell (Photo 9 - Grazing reindeer) (see left). It was a glorious drive, taking 1½ hours to reach the E45 Inlandsvägen. We now expected a rapid run for the 35kms up to Porjus (click here for detailed map of route), but on approaching the Ligga dam (see right), serious road-works began. Dropping down the steeply winding approach to cross the dam, entire sections of road were totally stripped of tarmac, leaving just rough, gravelled surface. Crossing the Ligga dam, the down-stream view into the bed of the Stora Luleälven showed the lower rocky gorge to be entirely dry and barren, the river's natural course below the reservoir diverted into the underground Ligga generating station for hydro-electric power (HEP) production, with the tail-race emerging several kms downstream. Across the dam, the E45 Inlandsvägen began the climb towards Harsprånget, the long haul today made more difficult by intermittent sections of road being entirely stripped of asphalt. This continued for the next 20kms, and we bumped along the rough, gravelled unsurfaced road all the way up to Porjus. For the country's main northern highway to be left for several months in this state by the National Road Agency with no remedial surfacing work taking place was an utter disgrace which certainly would not be tolerated in the south of Sweden.

Crash-site of WW2 RAF Lancaster bomber Easy Elsie:  thankful to regain normally tarmaced road on reaching Porjus Old PowerStation, we turned off across the Porjus New Dam onto Route 819 (click here for detailed map of route). The narrow single-track lane wound past the dam's rock-fill foundations leading to the Sámi hamlet of Ålloluokta, and 7kms along the shores of Lake Stora Lulevatten we reached the parking area at the start of the board-walk out to the marsh-land crash site of the WW2 RAF Lancaster Easy Elsie. RAF Lancaster FC-E was assigned to 617 Squadron in August 1944 and re-christened Easy Elsie by its crew. On its first operational mission against the German battleship Tirpitz at the northern Norwegian anchorage at Kåfjord, Lancaster Easy Elsie had been damaged by flak but repaired and made airworthy again. Tirpitz was moved south to Kvaløya in Tromsø Fjord, and was attacked again on 29 October 1944 by Lancasters of 617 and 9 Squadrons including Easy Elsie, each stripped of armaments, modified with extra fuel tanks and carrying one 6 ton Tallboy bomb. During the attack, Easy Elsie was severely damaged by flak: the right outer engine was lost, she was losing fuel and hydraulic fluid, and the radio was hit. Further damaged by flak knocking out the left inner engine and losing more fuel, and with bomb doors unable to be raised through loss of hydraulics, the resultant drag made the aircraft difficult to fly. With 2 engines lost and losing fuel, there was no way the Australian pilot, Flying Officer David Carey could get the Lancaster back to Scotland. He and the navigator Pilot Officer Alex McKie decided to try to get over to neutral Sweden. With maximum power on the 2 remaining engines, Carey managed to gain sufficient height to clear the Norwegian mountains and turned the severely damaged Lancaster south into Sweden. Between the cloud, all they could see was empty wilderness and forest, but with fuel almost exhausted they saw a boggy clearing in the forest near to Porjus. The crew jettisoned all weapons, ammunition and equipment to lighten the aircraft and took up crash-landing positions for Carey to put the aircraft down in an open space. The undercarriage cut into bog and the plane shuddered to a halt standing on its nose and falling back into the bog. It was 11-50am. The pilot injured his knee on the instrument panel with the impact of crash-landing, but the rest of the crew was unhurt. They destroyed all maps and operational orders, tried to set fire to the wreckage, and carried Carey into the nearby forest. Swedish soldiers who had seen the Lancaster's crash-landing, found the crew who were taken to Stockholm for interrogation and later repatriated to England in November 1944. Tirpitz was finally sunk in Tromsø Fjord in November 1944 by a further 617 and 9 Squadron Lancaster attack, Operation Catechism.

We had first visited the crash site on our 2013 Sweden trip; see our log for the full history of Easy Elsie's last mission and crash-landing in marshland near Porjus.

Kitting up in expectation of midges, we again set out to walk the 2 kms along the forest board-walk to the marsh-land clearing to pay our respects at the aircraft remains  (Photo 10 - Board-walk to crash-site). We feared that, in the 3 years since our first visit, the board-walk might be suffering for lack of maintenance, but it was as sturdy as ever thanks to the efforts of the Porjus Archive Committee; and at the driest time of a dry year, the surrounding marshland was firm apart from the very wet areas of bog around the aircraft remains. The 2 kms route out through the spruce forest was itself a delightful prelude, with the forest floor covered with the usual northern berry plants (Photo 11 - Ripe Cloudberry) and Labrador Tea (see above left). This lovely walk, meandering through the forest of tall candle-spruces, brought us out to the edge of a boggy clearing. The topography of this generally forest covered region showed the skill and good judgement on Carey and McKie's part in locating the clearing amid almost continuous forest, and managing to 'pancake' the severely damaged aircraft in the boggy ground with no serious injuries or death to the crew. It was one brilliant piece of flying and navigation. And over in the centre of the clearing, we could see ahead the Lancaster's remains lying forlornly where she had crash-landed 72 years ago (see above right) (Photo 12 - Forest clearing crash-site). We moved forward along the board-walk to the centre of the clearing and the remains of the crashed aircraft (see above left and right).

First impressions were that the wreckage was more scattered and randomly heaped, and in a more dilapidated state than in 2013. Certainly the rear fuselage was toppled over onto its side and the tail-plane and fins less orderly placed. But it was more likely that, with the passage of time, decay and dereliction had further taken its toll, together with souvenir hunters removing further portions of the aircraft's remains. The sun just about managed to shine for us to take our photos from the board-walk surrounding the wreckage, which still lay in the soggy marsh-land that had saved it from total destruction on crash-landing 72 years ago (see left) (Photo 13 - Remains of Lancaster Easy Elsie). With no functioning undercarriage due to total loss of hydraulics from flak damage, it was Flying Officer Carey's skill in putting the badly damaged aircraft down in this bog that had saved the crew's lives. We walked around the crashed Lancaster trying to identify its decayed components. There was little remaining of the cockpit and forward section of the fuselage which were badly damaged when the crew had attempted to destroy the plane after the crash-landing (see above right). Part of a yellow RAF roundel was recognisable on one section of the fuselage (see right) (Photo 14 - Fuselage with RAF roundel), and the surviving wings and other sections showed flak damage. It was a poignantly moving moment again to pay our respects to the skill and courage of Easy Elsie's flying crew at the site of the crash-landing (Photo 15 - Easy Elsie crash site). We do however make this plea to others who may visit the Lancaster's remains, which have survived here at the marshland crash-site for 72 years: please do NOT remove further fragments as souvenirs or further disturb the aircraft; leave the remains of the Lancaster in peace out of respect for her crew. See our Crashed RAF Lancaster Photo Gallery.

Wild-camp at the abandoned village of Harsprånget:  we returned across the Porjus dam to Porjus (click here for detailed map of route) (see left), and shopped for provisions at the local village ICA stores before tackling the return drive down the scoured, surface-less E45 to wild-camp at the site of the now abandoned village of Harsprånget. This had originally been built in 1946 to provide accommodation for building workers close to the construction site of the new Harsprånget dam and power plant. Sweden's 20th century programme of hydro-electric power production had begun in 1910 at Olidan on the Gotä River rapids near Trollhätten (See log of our visit to Olidan HEP plant). This was followed by the pioneering construction 5 years later of the dam and underground generating plant at Porjus, primarily to supply power for electric traction on the Malmbanan railway transporting iron ore from the mines at Gällivare and Kiruna down to the ports of Narvik and Luleå. Plans were drawn up in 1919 to follow this with an even bigger dam and HEP generating station further downstream on the steeply falling Luleälven river at Harsprånget. But with post-WW1 depression and decreased demand for electricity, construction of the Harsprånget dam was postponed. Work finally began in 1946 of what would be Sweden's largest rock-fill dam and hydro-electric generating plant at Harsprånget, with a power production capacity of 977Mw. Because of Harsprånget dam's isolated location in the then remote Lapland wilderness, a new village was built nearby for construction workers and their families. At its height, the village housed over 2,000 residents, a well-established community with shops, leisure facilities, hospital and school. The dam and generating plant at Harsprånget were commissioned in 1952,and production capacity increased with additional power plants during the 1970s. The nearby village of Harsprånget remained occupied until 1985, when the last occupants moved away and the wooden houses were transported elsewhere.

From the E45, we turned up the gravel lane that led to the site of the long abandoned village of Harsprånget. Nature had reclaimed the former settlement's site, and a tangle of wilderness vegetation and birch trees had reasserted itself where once there had been streets and houses. The Porjus Archive Association keep alive the village's memory, preserving the approach lane of Storgatan (Main Street), with a few of the street name boards still in place (see right). An information panel gave an outline map showing the extent of the former village's streets, but beyond Torget these were all now totally overgrown with an impenetrable re-growth of trees and vegetation. With midges swarming around our heads, we set up camp by the former village's square of Torget (see above right) (Photo 16 - Harsprånget wild-camp), and later that evening cooked an appropriate Swedish supper of köttbular (meatballs) and lingonberry sauce.

We woke to a bright morning for breakfast looking out onto the overgrown Torget of Harsprånget (see above left). Earlier we had walked along the remaining length of Storgatan where the forest was increasingly re-claiming the land. Harsprånget abandoned village had been a hugely memorable if eerily uncanny camping spot among the thickets of this ghost village, and the only disturbance during the night was the sound of an animal munching among the vegetation! For a brief overnight and morning, our presence had brought life back to what had once been a lively community, but now nature was once more re-asserting its hold over the site.

Harsprånget rock-fill dam and dry gorge:  back down the lane, we now faced the dreadful state of the E45. The State Highways Authority had stripped the entire asphalt surface from a 20km section of the road at the beginning of summer, and local people travelling between Porjus and Jokkmokk had been forced to endure the damaging impact on their vehicles for all this time; it was not expected to be re-surfaced for another couple of months. For a major European highway, and the principal route up through Northern Sweden, to be left in such a disgraceful condition for 5 months was nothing short of scandalous. We returned downhill with the road's steep gradient showing how much the Luleälven river must drop in the 10kms distance from the Porjus dam outflow. Rounding a bend, there was the massive curvature of the Harsprånget rock-fill dam winding across the head of the gorge (see left) (Photo 17 - Harsprånget rock-fill dam). We bumped our way a further km down the steep slope past the Harsprånget HEP generating station (kraftverk in Swedish) to the parking area signposted for the memorial to the 10 men killed during the Harsprånget dam's construction, and the look-out point viewing platform overlooking what once would have been the torrent of Harsprånget waterfalls. A gate through the fence displayed a menacing sign with the warning: Dam gates may open without prior warning, and an image showing the dam sluices open and water flooding down the normally dry gorge in pursuit of a figure fleeing in terror! (see right) We followed the sturdy board-walk which enabled a safe descent down over the smoothly eroded granite slabs into the steep and in places almost sheer rocky slope of the ravine (Photo 18 - Harsprånget Gorge board-walk). The Harsprånget gorge is now almost totally dry (see left): the dam's construction across the head of the gorge now holds back the waters of the Luleälven river which once cascaded in raging torrents, particularly after Spring melts, down the steep length of the canyon creating what was then the Harsprånget-fallet.

We edged down with the sun illuminating the length of the upper gorge. Vattenfall's construction of the Harsprånget dam may have closed off the rapids and falls which once glorified this magnificent gorge, but depriving the world of that spectacle had opened up another equally impressive sight: the precipitous rocky sides of the now dry gorge, lit by the morning sun, glowed in multiple shades of ruddy-brown. From the wooden viewing-platform high above the sheer drop of the canyon, the view up the gorge was staggeringly beautiful with its rock walls glowing in the sunlight; and the rock-fill dam, which from 1952 has held back the natural flow of the once mighty Luleälven torrent, reared high above across the distant head of the gorge, now revealing these magnificent rock walls (Photo 19 - Harsprånget Gorge rock walls) (see right). We clambered up the rocks at the look-out point marvelling at the bare rocky spectacle of this magnificent canyon now revealed before us in all its glory thanks to the Harsprånget dam. Looking downstream from the view-point, the walls of the totally dry canyon bed rose precipitously on the far side (see below left). But the sun had now disappeared behind gathering storm clouds, and we hurried back up the board-walk before the inevitable downpour hit.

The environmental impact of hydro-power:  the sight of the now dry Harsprånget brought home the controversial issue of the impact of supposedly environmentally friendly hydro-electric power. Vattenfall's web site naturally makes much of hydro-electric power as a totally renewable energy source with minimal environmental impact and zero pollution. Opponents however point out the vast changes that the damming of natural water courses causes, and the impact on both flora and fauna: salmon can no longer follow their powerful instinct to migrate upstream to spawn, and part of the cost of hydro-power is the necessary annual fish re-stocking of rivers. The enlargement of lakes caused by damming has damaging impact on grazing lands and makes reindeer migrating routes more difficult. We had ourselves witnessed the contrast in topographical impact of the now totally controlled Umeälven river compared with the natural state of the unexploited Vindelälven valley. Of the major rivers of Northern Sweden, only 4 now remain in their natural state unexploited by HEP, the Torne, Kalix, Pite and Vindel Rivers. Here at Harsprånget, we could see the issue in stark terms before our very eyes: before the dam's construction, this would have been a wild torrent flowing down the falls of the narrow canyon and subject to the natural seasonal variations in water flow from the wild spring melt-water floods to the ice-bound white-out of winter; the very name Harsprånget meaning 'hare's run' was derived from the sharp turns in the rapids, similar to a hare fleeing. Now however the gorge was entirely dry, and high above us at the head of the canyon we could see the stark desert-like stone field of the rock-fill dam's embankment. Having said that however, with the canyon now dry and deprived of water by the dam, the stark natural beauty of its varied multi-coloured rock walls were revealed in their full glory. Modern society demands ever-increasing supplies of electricity, and compared with the pollutant impact and short-term finiteness of expendable fossil fuels or long-term inheritance of nuclear waste, the impact of hydro-power seemed minimalist. Clearly there is no such thing as a free light switch and the price to pay for hydro-power, in terrain where this is feasible, seems the least damaging compared with alternative sources of energy.

The Luleälven dams and hydro-electric generating plants:  we bumped our way back up the 10kms of unsurfaced E45 to the huge complex of the Porjus dam and hydro-electric generating station at Porjus village, and turned off to the Gamle Kraftverk (Old Power Station). The power generating and distribution company Vattenfall is still a state-owned enterprise although now partly deregulated to compete for business across the EU. It now manages all of Sweden's power industry, hydro, nuclear and wind-power, with stakes in power generation in Germany, Poland and Holland. 46% of Sweden's electrical supply is generated by HEP, 44% by its 3 nuclear power stations, and just 1% by wind power. The 15 HEP stations on the Luleälven, which drops 1000m from its source in the Norwegian mountains down its 450km length to the Bothnian Gulf at Luleä, supply 15% of the country's power. The Luleälven's 15 dams are now of the rock-fill type construction, which rely on steady filtering of water through the semi-permeable core and broadly spread compacted rock to control the reservoir's water volume. All 15 of the Luleälven generating stations (kraft verks) are now remotely controlled from a central control station at Vuollerim part-way down the river.

The first dam at Porjus, built between 1910~15, was a vast construction undertaking in remote wilderness terrain through the darkness and freezing temperatures of the Arctic winter. The original Porjus generating station was constructed 60m underground, blasted out of the bedrock to achieve the necessary head-drop of water from the nearby dam. The tail-race ran in an underground tunnel over 1km downstream for the out-flow of used water back into the river. The imposing red-brick neo-Gothic switchgear building, visible at ground level above the underground generating hall, was designed in monumental style by Erik Josephson (1864~1929), a leading Swedish architect of public buildings, who had also been responsible for the fortress-like design of Olidan power station. Being a public undertaking, Vattenfall's predecessor company, Kungliga Vattenfallsstyrelsen (Royal State Power Board), intended the monumental Porjus Power Station to reflect its royal standing. No expense was spared in the design, which was not only extravagant in scale but also incorporated imposing art nouveau decorative features such as shapely windows, grandiose main doors, belfry-like tower with golden royal crown, and in the control room, grand light fittings and marble-faced control panel. King Gustav V was due to perform the opening in 1915, but WW1 made his monarchic venture to the Arctic too dangerous, and the dam's inauguration was performed by telephone from Stockholm. The old Porjus dam and power station continued in operation until 1975 when the original solid-core dam was replaced by the present rock-fill dam with its new underground kraft verk. The imposing Neo-Gothic building of the now redundant former power station has been retained as a heritage site, and during the summer months Vattenfall offer free-of-charge hourly guided tours of the original station and its underground generating hall.

Our visit to the Porjus Old Power Station:  black storm clouds filled the sky as we reached the Porjus Old Power Station (see above right) (Photo 20 - Porjus Old Power Station), and it was unnerving looking out across the towering complex of switchgear, transformers and distribution network with lightning flashing overhead and thunder rumbling around the surrounding fells. In pouring rain we heaved open the building's grandiose door in time for the 1-30pm tour, to be faced with depressing news: because of the thunderstorm and risk of power failure affecting the lift and lighting in the underground generating hall, the visit would be restricted to a brief commentary in the station's control room. Showing our extreme disappointment and frustration, we tried every form of persuasion: the storm was visibly passing, we were happy to use the stairs, let us speak to someone with more senior authority. But the young guide would not succumb; safety rules must prevail. So while we waited for the next tour in an hour, when the storm certainly would be past, we viewed the grandiose control room (see above left). Here was a total irony: Vattenfall, which is responsible for electricity generation covering the whole of Sweden and parts of wider Europe, could not even guarentee lighting for its own power station! At 2-30pm with the weather now clear, we returned with renewed determination; another of the guides, having checked the lighting after the thunderstorm fiasco, declared all was well and issued us with hard-hats for the tour. We emerged from the lift into the vast and beautifully tiled underground machine hall, and spent the next hour examining the turbines, generators and control equipment, in detailed discussion about their working with the guide, Eino. The Vattenfall displays were first class, with key parts of the original turbines and generators opened up to reveal their working components. An artificial opening gave a clear view inside the normally enclosed inner turbine chamber (see above left), showing the pressured water entry conduit which dropped 60m from the reservoir supply way above down onto the turbine blades, and the shaft rotated by water pressure on the turbine. Below this, the waste water conduit, now blocked off, would in operation have dropped down to the underground tail-race; see diagram of HEP power station working. Maintenance staff would have had to crawl into this chamber via a small entry port, and hang above the chasm of the exit conduit to repair cavitation damage to turbine blades.

Eino showed us the enormous steel drive shaft which connected turbine to generator on the far side of the hall via self-regulating apparatus which maintained rotation at the optimum rate of 2,500 rpm for generation of 50hz AC current (Photo 21 - Underground generating hall) (see above right). This governing device operated hydraulic pistons which automatically adjusted the turbine blades angle to maintain consistent revolutions of the drive shaft. The drive shaft itself was a hugely impressive piece of equipment with massive roller-bearings at key points along its length, and at the far end further bearings connected it to the 4m high generator, which was partially exposed to show its workings (Photo 22 - Porjus generator) (see above right). Driven by the turbine, the inner disk of electro-magnetic armatures rotated within the outer ring of stator-coils to generate AC electricity. Eino very competently and in fluent English explained the turbine and generator's workings. We discussed how the technology of both turbines and generators had improved in generating capacity: when all 9 turbine~generator sets of the original 1915 Porjus plant were operating, together they produced a maximum of 145Mw of electricity; in contrast, just one of the 2 new generation generators of the 1970s New Porjus Station can produce 240Mw. We were also shown the new Powerformer generators, set up in experimental form in place of the original units 8 and 9 at Porjus and installed operationally at Parsi HEP Station further down the Luleälven. They generate high voltage current supplied directly to the distribution grid without the losses incurred by step-up transformers. One item of historic interest was the logo of Allmänna Svenska Elektriska A-B (now ABB) electrical engineering company from Västerås which had supplied the Porjus generators. The company's original logo had incorporated the ancient Indo-European swastika symbol; this was changed in 1933 for political correctness reasons, but a plaque with a sole example of the original logo survives on a piece of machinery at Porjus (see above left). There was noticeable contrast in standards of finish between the original wing of the machine hall and the later extension: with royal status, the original company had lavished funding on the scale and finish of the tiled generator hall; in contrast, 1940s austerity meant reduced standards with plainer floor tiles and even exposed bed-rock showing through on the walls.

After the initial set-back from the storm, we had been most fortunate in achieving the Porjus Power Station visit with Eino as our guide: his knowledge, competence and fluent English contributed much to our understanding of the workings of HEP generation. His family lived in Porjus and his father was an electrical engineer at the New Porjus Power Station; we assumed Eino was also an engineer, but in fact he was due to go up to Skellefteå University to read computer science. Through our web site we extend our profuse gratitude for his thoroughly educative commentary and wish him well in his future studies and career.

North on E45 Inlandsvägen to Gällivare:  the storm clouds and rain had passed and sky brightening by the time we emerged from the Porjus underground generating hall to resume our northward journey. The final section of the Inlandsbanan railway curved away towards the Porjus new dam just beyond the Old Power Station (see above right) (Photo 23 - Porjus dam and New Power Station), following the line of the original trackway built in 1912 to supply materials for the old Porjus dam and deliver machine parts for the generator house. Part of this original narrow gauge siding trackway still survived outside the Old Power Station, running alongside the standard gauge Inlandsbanan, and disappearing through lofty doors into the switchgear house. Earlier we had seen huge gantry cranes which had off-loaded machine parts from railway wagons inside the station and lowered them for assembly down in the underground turbine~generator hall. We passed through Porjus village, now a community of 400 residents from its origins as a settlement for construction workers on the 1910 old dam and power station; the Stockholm government had assigned 100 immigrants to live here in a former barracks hut. The E45 turned north-west heading towards Gällivare (click here for detailed map of route) with the magnificent spruce forested rolling fell-scape lit by now bright afternoon sun against a blue sky; higher rounded hills covered with spruce forests graced the northern horizon.

Wild-camp on banks of Kalixälven river at  Lappeasuando:  crossing the river at Gällivare, we drove past the modern apartment blocks of the lower town to find the ICA Kvantum hypermarket. Ahead we could see the Malmberget iron mines scarring the hillside; we recalled our underground visit to the Malmberget mines in 2013 (See log of our 2013 visit to Malmberget iron mines) and this raised the question of how far the residents of Gällivare had progressed with relocation of the original settlement which was now so threatened with mining subsidence. The Gällivare ICA Kvantum was a large and well-stocked stores, built on reclaimed industrial land in the newer part of town, and we stocked up with 2 days' provisions. Leaving Gällivare, E45 merged with E10 coming up from Luleå and headed north across increasingly hilly, forested fell-land (see above right). After some 40kms we reached the Kalixälven river-crossing at  Lappeasuando, the tiny settlement which spans the 2 municipalities of Gällivare and Kiruna, divided by the river. Here the former 1930s elegantly arched bridge, which replaced a former ferry crossing the Kalixälven, still stands alongside the more functional modern bridge carrying the E45 across the wide river. Alongside, a large picnic area stood by a café; we pulled in, and below the tarmaced car park, found a lower grassy area screened by trees and directly overlooking the river and old bridge. Here was the perfect wild-camp spot, and we tucked George into a sheltered corner by the river by the old bridge (see left) (Photo 24 - Kalixälven wild-camp).

The afternoon sun was bright, and the old bridge gave a perfect view of our peaceful riverside camping spot (see left and above right). In contrast the stark parking area was crammed full of camping-cars lined up in rows; thankfully we were well sheltered from these hoards. Exploration showed not only that the café also had a small campsite, but the parking area was equipped with water-supplied WCs; it was indeed not only a beautifully located wild-camp spot but well equipped, and later the sun declined across the Kalixälven to give magnificent reflections in the wide river's still waters (Photo 25- Kalixälven reflections) (see right).

Yet more neglect of northern principal roads:  the following morning we continued north on E45 to the road junction at Svappavaara, where the Inlandsvägen turned north towards its ultimate northerly destination at Karesuando on the Finnish border. We turned NW on E10 towards Kiruna (click here for detailed map of route). The open-cast iron mines at Svappavaara seemed more widespread than ever as LKAB, the state-owned mining company takes over more of the Sámi reindeer grazing lands. But at least, we thought, two years on from when we last passed this way, when we had crawled along for more than 20kms of rough, unsurfaced road with the tarmac totally stripped away, by now all the road-widening works should have been completed with an entirely new, re-engineered highway. For the first 5kms this was so, but then the dreaded road works signs loomed. The next 15kms had been widened but were still in process of being re-tarmaced. Worse still however, where the road crossed drainage culverts every 500m, the surface was still stripped, meaning slowing to cross these rough 30m sections. This appallingly slow progress with reinstating a major highway simply would not be tolerated in the south of Sweden particularly around Stockholm; but up here in the north, seemly anything goes. This was not simply northern prejudice feeling the victim of public services neglect compared with the south; we had experienced direct evidence of such neglect twice now. LKAB's mining, which is taking over more and more land in Norrland, raises untold revenues for the State, yet the north of the country enjoys second rate public services compared with the south.

The iron mining town of Kiruna, threatened by mining subsidence:  we had visited Kiruna in both 2013 and 2014, when we had learned much about the town's economic reliance on iron ore mining, undertaken by the State-mining company LKAB, which takes its name, Luossovaara-Kiirunavaara Aktiebolag, from the Kiruna's 2 hills of Luossovaara and Kiirunavaara where open-cast iron ore mining at Kiruna first began in 1898 (see right). Mining is progressively undermining the city centre, making necessary its relocation due to the impact of mining subsidence. Our main reason for returning to Kiruna this year was to see how much tangible progress had been made in the last 2 years with the town's relocation. In 2004 LKAB's Managing Director had submitted an arrogantly brief letter to Kiruna Municipal Authority, which we had seen displayed in Kiruna City Hall. The gist of the letter was: We are going on mining deeper; you'd better move your town. LKAB's deep mining method called sub-level caving leaves cavities in the bed-rock when the ore is extracted. When these cavities collapse re-filling the surrounding bed-rock, over time this results in subsidence at the surface (see log of 2013 visit to Kiruna). Because the ore body, into which LKAB are deep mining, slopes down at a 60º angle beneath the city, the area of subsidence is moving ever closer towards Kiruna centre at the rate of 40m a year (see diagram left). This damaging impact on the city's environment has already reached close to the E10 and the present City Hall. The speed of approach of the area of surface deformation depends on the rate of LKAB's deep mining, at present at the 1,365m level. Levels and progress of deformation are being monitored by ground measuring instruments, giving forecasts of future rate of subsidence on which the Municipality is basing its relocation plans. Forecasts however predict that 33% of Kiruna's 20,000 residents must be re-housed; within the zone of surface deformation, there are 3,200 homes, several hotels, the entire city centre commercial district, and the majority of public institutions including City Hall, secondary and elementary schools, hospital, library, parish church and public baths. This all affects 1,000 jobs and over 6,000 people.

Our 2016 re-visit to Kiruna:  turning off E10 into Kiruna, we passed the construction site for the new city centre, but the only visible progress was a large rotunda-shaped building in the early stages of construction. The rest of the area was still untouched former industrial land. Was this all the progress that the last 2 years had produced, and were the discussions, consultation and glitzy plans still the only thing happening in Kiruna? One thing was certain however: LKAB was still driving the underground mining into the ore body ever deeper and deeper, lining the State's coffers accordingly, and of course further undermining the city centre with ever threatening subsidence. We continued ahead into the city, passing the mammoth gash of the original open-cast mine scarred across Kiirunavaara hill. There was the City Hall just beyond the corner of Gruvavägen (Mine Street), and the attractive wooden houses of the original 1910 township. All still looked the same; nothing had yet fallen into the mine! On a Saturday afternoon, we parked without difficulty in the central square; in the community centre LKAB's model illustrating the potential impact of mining subsidence was still there (See left), but today no one from LKAB's PR department was present to answer our questions. There was nothing new to be learned here.

We drove through Kiruna's western suburbs to the lane which circled up around the western side of Luossovaara hill. Leaving George towards the top of the steep gravelled trackway, we walked up the final section to the ski station at the summit, past the gashes of the original open-cast mines which still scar the eastern face of the hill. Our reason for struggling up to this high view-point was for the panoramic vista over the township spread out below with the overwhelming presence of LKAB modern mining operations, at least that which can be seen on the surface. Here dominating the landscape was the original reason for Kiruna's foundation as a town, its current source of wealth and employment, and soon its potential cause of destruction and need for relocation (see above right) (Photo 26 - LKAB iron ore mine). In the hazy afternoon sunshine we took our photos looking over the town and mine. Lines of empty hopper wagons awaiting re-filling with processed iron ore pellets for rail shipment down to Narvik stood in the sidings (see left) (Photo 27 - Sidings of hopper wagons); it seemed that LKAB had in the last 2 years re-routed the railway line safely away from the area of subsidence to the far side of the lake, and the new relocated Kiruna railway station had now opened. But all else remained the same, with the evident line of surface deformation creeping ever closer towards the city centre.

From the summit area we peered over the fencing into the gash of the former open-cast mine which spread across the eastern face of Luossovaara hill (see right), and returned down to George to sit at a barbecue hearth to eat our sandwiches. From this viewpoint high on the western side of Luossovaara hill, we had a 270º continuous panorama of empty wilderness; not even a trace of roads or any human presence, just empty fell-scape and the distant sweep of horizon looking out towards Abisko with the line of snow-capped Norwegian mountains (Photo 28 - Fell-scape panorama); so close to the industrial landscape of Kiruna's mines on the far side of the hill, but here an outlook of empty and uncontaminated natural beauty. This was another of the trip's most memorable lunch spots.

Back down the hill into the town, we parked by the City Hall for photographs (Photo 29 - Kiruna City Hall) (see left); who knows, next time we come to Kiruna, this inelegant cuboid building with its skeletal bell-tower may have been demolished and the city bureaucrats relocated, or will it have collapsed into the mine! As we stood examining the city relocation displays in the City Hall's lofty inner hall (see below right), a Municipal official joined us, opening with an unfortunate question: what did we think about what had been achieved with the city's relocation? Summoning utmost tact, the gist of our response was: well, not very much! You've had since 2004 and, from our 3 visits since 2013, all that seems to have happened is much discussion and paper plans, but precious little by way of tangible action, (well she did ask!) and the hole in the ground goes on getting bigger by the year. In fact, without her trying to push some indefensible local authority party line, we had a helpful and informative discussion with her about what was happening at Kiruna. The decision had been taken for the new city centre as the town's focus to move to a now agreed site 3kms eastwards along Malmvägen, and the rotunda building we had seen in construction was the new City Hall called Kristallen. In discussion about public attitudes towards the necessity for relocation, she added that, while there was general acceptance, public concerns now focussed on 2 issues which she summarised as money and outlook: LKAB were now committed to contributing huge sums of money as compensation for city infrastructure, and to fund new housing over the next 3 years to replace that in the threatened areas. While this suited property owners, those who rented houses, largely from LKAB at currently reasonable rents, faced a doubling of rental prices for new replacement housing. This issue remained unresolved. The other major concern was over visual outlook: those parts of the town affected by subsidence currently enjoyed a westward vista towards open fell-land, which we had seen from Luossovaara; eastward relocation however would deprive residents of that magnificent open fell and mountainous outlook. Another issue was that, due to cost restrictions, Kiruna's attractive original wooden houses, part of its key heritage, would be demolished and not relocated; a proposal had been put forward for the owners to relocate the demolished wooden houses at their own expense. This issue also remained unresolved.

In spite of all of this, the fact remained that, were it not for LKAB's mining, Kiruna would not exist as a township; its entire economic future depend totally on LKAB as the city's main employer along with mining support industries. Unemployment in Kiruna, with its population of 20,000 is just 2%. This prompted us to raise the issue of immigration and its impact on Kiruna. The Swedish government had forcibly assigned immigrants to northern townships to house, and Kiruna had accepted 1,000. Some had even been allocated to the empty skiing hotels up in the Arctic wilderness at Riksgränsen during the summer season! Despite this having been a thoroughly informative discussion from which we had learnt much, we were still however left with the feeling that the pace of progress with Kiruna's relocation was failing to match the rate at which LKAB's ever deeper and deeper mining was hastening the growth of subsidence. Time will tell.

Before leaving Kiruna, we re-visited 2 of its other features. Just up Gruvavägen, the town's wooden church (also due for relocation) had itself been a gift from LKAB and its the all-powerful managing director Hjalmar Lundbohm, regarded as Kiruna's founding father (Photo 30- Kiruna's wooden church) (see above left). The church was open, but the interior with its elaborate wooden structure was almost too dark for photos (see right). Further up into the town, but still within the threatened zone of deformation, we paused at the Swedish Sámi Parliament, the Sámetinget (Photo 31 - Swedish Sámi Parliament) (see left).

Jukkasjärvi wooden church:  at 4-30pm we finally left Kiruna today. Our discussion at City Hall was partly reassuring about the city's relocation, but with typical local authority handling, it seemed a frustratingly slow process; what should we find if we ever return? Back out along E10, we turned off across the wide Torneälven river to Jukkasjärvi to find Sweden's oldest wooden church from 1608 (see right). A wedding was about to take place, but as the guests assembled we just managed to gain entry for photos of the organ screen with Sámi drum symbol intertwined with Christian cross and modernistic altar paintings showing Laestadius denying sustaining liquor to the Sámis (Photo 32 - Jukkasjärvi wooden church).

Trollsparvens Camping at Vittangi:  we returned along the E10 for the 40kms to Svappavaara, braving the 3 hazards of this road: everlasting road works, slowly lumbering Norwegian camping-cars, and an equally tedious procession of speed cameras. Here we turned off northwards onto the E45 Inlandsvägen again, across the flat, forested lands of the Torneälven valley to Vittangi on the southern side of the river. The village has given its name to Vittangi Syndrome, congenital analgesia or the inability to feel pain, because of a cluster of cases of this rare condition reported in 2006 at Vittangi. On the far side of the wide river-crossing, we found tonight's campsite, Trollsparvens Camping on the banks of the Torneälven, a place we had passed twice before. An earlier phone call had brought no response, and on arrival the reception hut was locked. But as we stood there an Estonian migrant worker staying at one of the huts came over, saying he was looking after the place while the owner was in Luleå. The camping area was deserted and we settled in, but here on the banks of the Torneälven the midges were horrendous, some of the worst of the trip. After the mountainous landscapes of the last few days, the flat fells of the Torneälven valley seemed tediously monotonous, particularly in the now dull light (see left). The charge was reasonable at 180kr/night and facilities basic, but after 2 nights of wild-camping, it was a relief to soak in a hot shower.

Final stretch of E45 Inlandsvägen to Karesuando:  after a relaxing morning, it was noon before we were away, to drive the final 100kms of E45 Inlandsvägen, the road we had followed much of the way from Göteborg in the south, to Karesuando, Sweden's northernmost village on the border with NW Finland (click here for detailed map of route). When we had driven this section of Inlandsvägen south in 2014, it had been a glorious day with bright sun picking out all the details of the candle-spruces lining the road and enlivening the fell-scape. Today in total contrast, the dull, flat light rendered the trees and fells and equally dull and lifeless grey-green monotone (see right). We continued northwards through the Sámi settlements of Nedre and Övre Soppero, which spanned the Lainioälven, one of Sweden's finest fishing rivers and a tributary of the Torneälven. At present rate we should reach Karesuando early afternoon, but a thought now occurred: having secured our pitch at Sandlövs Camping, why not cross the border-bridge into Finland, and drive up to Kilpisjärvi this afternoon for a nostalgic re-visit and shop for shop for Finnish items from the K-Market there? So that was decided on, and we hastened on to Karesuando. As we drove northwards, the flat, empty fell-scape gave way to distant, higher and more rounded hills, but misty and featureless in the gloomy light.

A brief re-visit to Kilpisjärvi in NW Finland:  we reached the outskirts of Karesuando at 2-00pm and through the village past the familiar shops and reindeer meat-hall, turned off into Sandlövs Camping, where we had stayed many times before. Having reserved our place opposite the bridge and church, we crossed the bridge to Kaaresuvanto on the Finnish bank and turned NW-wards onto Route 21 to cross the Lätäseno which drains the empty fells of Finland's north-western arm of territory, and headed for Kilpisjärvi (click here for detailed map of route). Today the gloriously empty fell-scape and boulder-fields of the Könkämaälven valley were a boundless and featureless grey monotone in this dull light, such a pity without sunlight to enliven all the details of this magnificent empty wilderness landscape (see above left). Despite the less than even road surface, we made good progress, passing frequent camping-cars and caravans lumbering their way back to Norway. The distinctive feature of this lovely road are the long, straight stretches which undulate across the landscape, disappearing into the horizon-bound distance (see above right). Following the river and line of lakes which marks the Finnish~Swedish border, and passing through the occasional Sámi settlement, we moved NW-wards towards Kilpisjärvi, road signs ticking off the kms. The higher fells grew closer, and eventually we gained height towards the watershed with the first views of Kilpisjärvi lake filling the upper valley. In the now even gloomier light, the distant mountains of Norway were almost invisible in dark rain cloud, and as we passed along the shore of Kilpisjärvi lake, Saana (Finland's highest fell) and the lower Malla Fell were half-lost in a heavy covering of cloud. Passing the National Park centre, we finally reached the central area of Kilpisjärvi, with the K-Market and filling station as its focus, and by now the dark, gloomy cloud had turned to driving rain. The car park was full of Norwegian cross-border shoppers, but at least the supermarket was open. Inside we shopped for favourite Finnish items, and to our relief found a whole shelf full of the Laitilan Finnish beer which we had driven 100km from Karesuando to buy! We loaded our trolley and the €s bill tolled upwards; but no matter, we had secured our Laitilan. With a grateful kiitos paljon to the fluently English-speaking girl on the till, we loaded our supplies into George, and in winter-cold wind and rain, drove along to Kilpisjärvi Retkeilykeskus for a brief nostalgic re-visit. Across the lake, where last year we had crossed to the Treriksröset monument marking the fell-land meeting of the 3 borders, today the fells and distant mountainous skyline were totally lost in gloomy rain cloud. We turned and headed back the way we had driven along the shore of Kilpisjärvi lake in poor light and driving rain. From the head of the pass, the long, straight road stretched away for seemingly many kms into the murky distance, with the fell-scape and lakes a featureless, grey blur (see above left). It took over an hour to drive the 100km back to Kaaresuvanto on the Finnish side of the border-bridge, and as we returned south-eastwards the sky became brighter. George had a fill of cheaper Finnish diesel before we re-crossed the river into Ruotsi, as the Finns call Sweden (see right).

Sandlövs Camping at Karesuando:  Sandlövs Camping was still almost deserted as we settled George into his place looking across to Laestadius' church. The Finnish beer we had driven a wearying 200kms for this afternoon tasted even better than usual! It had also been a wonderfully nostalgic foray into NW Finland despite the regrettable weather conditions. The inevitable Norwegian caravans drifted in along with a ludicrously monstrous mega-bus, less an intrusion than a source of much ridicule and contempt for such gross materialism on wheels. Karesuando and Sandlövs Camping in particular will always be one of our Very Special Places, and it was wonderful to be back despite the misty cloud and rain which persisted all evening. Karesuando at the northern limit of Sweden represented the trip's half-way point, having driven almost 3,500 miles since crossing the Öresund; tomorrow we should begin the long homeward drive along the Finnish borderlands of the Tornedalen valley to Pajala, and the forecast was awful for chill Arctic rain. The forecast was right and we woke to miserably chill temperatures and wind-driven rain. It was no fun this morning washing up at the outdoor sink, wearing waterproofs against the chill rain. It was simply too wet this morning for photos of this lovely straightforward campsite, and we recalled the pleasant sun when we stayed here last year from Finland (Photo 33 - Sandlövs Camping at Karesuando) (see left). With farewells to Sandlövs for another year, we drove into the village for our shopping. In pouring rain, our first stop was Eliasson Kötthallen (Meat-hall) for frozen packs of reindeer and elk meat (see right), then the minimarkets for general foodstuffs.

A wet drive along the Tornedalen valley Finnish borderlands to Pajala:  finally leaving Karesuando with the rain still pouring on a very gloomy morning, we turned south-eastwards just before the border-bridge onto the lonely Route 99 for the 180km drive down Tornedalen. On a sunny day, this would have been a supremely beautiful road, with a bright sun picking out the detail of pines and spruces, occasional glimpses of the Torneälven, and the distant forested hills of Finland across the river-border. Today however, in such filthy wet weather, the forests had a sad and drearily grey air (see left), and we bumped along the poorly surfaced road, splashing through puddles and scarcely seeing any other vehicles. This was indeed a very lonely road (click here for detailed map of route). The road ran parallel with the Muonionjoki border-river (Photo 34 - Muonionjoki border-river), passing the occasional Sámi settlement. Finally we reached the larger village of Muodoslompolo where we had discovered a small campsite set right on the river-border and run by the Tornedalen-Finnish Malmström family for 30 years. We ventured off the main road and 6 kms along a single-track lane at the tiny border village of Muonionalusta, set on a river-island formed between the main Muonionjoki and a tributary, we finally reached Rajamaa Camping. Although it was off our route today, this was certainly worthwhile for a future stay either from Northern Finland or Swedish Lapland, particularly since Route 404 crossed the river to Muonio close to the Pallas-Yllästunturi National Park. We continued south on Route 99 which turned inland through sandy-heath forests rich with reindeer lichen before returning to the river at the tiny settlement of Parkajoki. All the settlements along this stretch had Finnish-sounding names, ending in -joki and -järvi.

The Kaalama memorial:  a short distance further near the village of Kaalama, we reached the memorial to a 1942 wartime atrocity which we had first discovered when passing this way on our 2013 trip. Set in a forest clearing a short distance from the road, the monument, headed Kolmin Proletär Internationalism and mounted on a communist red-star plinth, incorporated a pictorial plaque showing helmeted soldiers executing kneeling figures (see right). The lengthily worded inscription included the date of 22 December 1942, but we had been unable to discover from any source more details about the commemorated massacre. Careful analysis and translation of the monument's semi legible Swedish inscription has now thrown some light on the incident: the monument was erected in 1978 by the Pajala branch of the VPK, formerly the Swedish Communist Party; in 1942 a group of Finnish communist guerrilla fighters, referred to as Forest Guards because of their hideout in the forests, had been pursued across the border by Finnish military; their alleged crime was their 'anti fascist' resistance to what the text calls the 'fascist onslaught', in other words a continuation of the bitter left- and right-wing enmity that still existed in Finland from the time of the 1918~20 Civil War, even after the 1939~40 Winter War had brought a degree of national unity. The guerrillas had been sheltered by left-wing sympathisers from nearby Swedish villages, but some had been shot by Swedish military and police (the massacre portrayed on the pictorial plaque), others were imprisoned or deported back to internment camps in Finland. We now had a clearer understanding of the background to this now forgotten memorial half-buried in the forest, which recalled one brutal episode involving left-wing guerrillas and the White-dominated Finnish military along the porous Tornedalen border, in the long history of internecine political extreme violence in Finland during the first half of the 20th century.

Pajala Camping and the village of Pajala:  Route 99 now moved away from the river (click here for detailed map of route), with apparently a clear run past the Struve geodetic memorial at Jupukka, but then we had to face yet more road works and a 10 kms stretch of totally stripped, unsurfaced gravel or newly asphalted road, lasting until the river crossing to join Route 395 coming in from Vittangi down to Pajala. Through Pajala, we finally reached the campsite down on the banks of the wide Torneälven river. When we had stayed here in 2013, prices were a reasonable 210kr/night; 3 years on, they risen to 260kr, a very unreasonable 25% increase price. Reluctantly we booked in, and settled into the forested corner (Photo 35 - Pajala Camping), preferring the company of Bilberries and Lingonberries on the river bank to all the caravans and camping-cars corralled into the tarmaced area by reception. Today had been a depressingly chill, wet and cheerless day for our drive along the Tornedalen valley, but we hoped for better weather for our day in camp tomorrow at Pajala. A warmer morning brought even a hint of hazy sun, but by early afternoon the rain returned; even so we managed to pick breakfast bilberries from the forest floor near our pitch, and that evening we cooked a Lapland supper of reindeer and lingonberry stew. But the rain began again, and for the first time this trip, the sky was really dusky; the year was moving on and we tomorrow we should cross the Arctic Circle south.

Crossing the Arctic Circle south near to Överkalix:  before leaving Pajala, we called in at the village centre to shop at the Coop-Konsum and re-visit the Pajala Sun Square, claimed as the world's largest sun dial fully 38m in diameter and filling the village's central square. The Midnight Sun's 24 hours' light casts the shadow of the tall gnomon, angled like the Earth's axis, against the 360° cicle of hour posts. And this morning, the sun actually obligingly shone enabling us to check the sun dial's accuracy (Photo 36 - Pajala sun dial) (see right). Route 392 took us across the lonely and deserted wilderness terrain between the Torneälven and Kalixälven valleys (click here for detailed map of route), but 30km south from Pajala we reached Korpilombolo and yet another 20kms of road entirely stripped of asphalt which the owner of Pajala Camping had warned us of. We passed no reindeer this year along this road, but this was scarcely surprising; these gentle creatures have more sense than to try walking along such rough gravelled, unsurfaced road which we had to travel. As we journeyed on, the hugely dramatic cloud-scape filling the southern sky emphasised the emptiness of this lonely fell-land and forest (see left); we made the most of it, since we should shortly be leaving the Arctic, and exchanging wild country for forests maintained for timber cutting. Driving on, we reached the road junction at the Kalixälven valley, and as we turned south the terrain became more pastoral with farms spread along the banks of the wide river. A short distance further an we reached the line of the Arctic Circle, our 4th crossing this year (see right) (Photo 37 - Crossing Arctic Circle south).

South to Älvsbyn:  by the time we reached the junction with Route 98 and near to Överkalix to join Route E10 coming in from Gällivare, the lower Kalixälven valley was continuous farmland (click here for detailed map of route), reinforcing the feeling we had now left the Arctic. We followed this faster road alongside the lakes of the lower Kalixälven valley to turn off at the junction with Route 356 at Marjärv. This road wound its way through forested lands, with the parallel Haparanda railway line following an even more winding course. But these were not now the wild forests of the Arctic, but clearly maintained for timber. The sky had darkened and rain was falling as we reached the unremarkable garrison town of Boden, to cross the Luleälven again, here flowing far more gently in its lower valley than when we had last seen this mighty river much abused for HEP production up at Porjus and Harsprånget. The final stage of today's journey on Route 356 was through more open terrain with distant views over forested hills, bringing us finally down to join Route 94 along the lower Piteälven valley and across the river to Älvsbyn.

Selholmens Camping at Älvsbyn:  after shopping for provisions at the well-stocked ICA supermarket in the centre of Älvsbyn, we booked in at Selholmens Camping, a small local campsite pleasantly terraced up the banks of the Piteälven river. The campsite is owned by Älvsbyn municipality and managed by a local sports association. On our last stay in July 2013, the site was popular with Swedish holiday-makers from the coastal cities, and today we had telephoned to be assured of a place. On arrival, we were surprised to find the site almost empty, the only occupants being the clusters of caravans used by migrant railway civil engineering workers. We settled on the upper terrace to enjoy the peace of the early evening overlooking the river. The following morning we woke to mist drifting along the river valley, which soon lifted to give a clear sky and bright sun; it was a truly beautiful early autumn morning (see left) (Photo 38 - Selholmens Camping at Älvsbyn). To begin with we were able to sit out at a picnic table to enjoy a peaceful breakfast. But the railway navvies returned from their night shift; their undue noise and offensive behaviour put paid to the peaceful morning. This may be a ready source of income for municipal campsites to host migrant workers (an increasing feature seen a elsewhere), but the noise and unacceptable behaviour of such folk will certainly deter regular visitors; we made it abundantly clear to the warden that we were not prepared to tolerate such disturbance. It remains for campsite owners to choose their priorities between a quick buck or lasting business.

Storforsen rapids on the Piteälven river:  the forecast suggested that the fine weather would not last through the afternoon, and we therefore set off early to ensure clear sun for our re-visit to Storforsen rapids. Before departing, we reserved a pitch lower down away from the noise and loutish behaviour of the railway workers. Route 274 followed the Piteälven for 30kms westwards along the farming valley (click here for detailed map of route) to the lake where the river turns through a sharp 90º after descending the steep rapids of Storforsen, to continue its more gentle course along the lower valley. A side lane ended at the large car park, almost full of tourist cars even mid-week.

The Piteälven along with Torneälven, Kalixälven and Vindelälven are Sweden's 4 remaining rivers whose natural environment is protected by law from intrusive exploitation for hydro-electric generation. The natural flow of water in the Piteälven varies enormously between seasons, highest during Spring melts reaching 1000m3/second, and lowest in mid-winter when the flow rate is as low as 24m3. The rapids at Storforsen (meaning Great Rapids) are the largest natural white-water rapids in the Nordic countries and among Europe's largest with a total drop of 82m over their 5km course at the point where the river over aeons has gouged out a channel in the hard granite bed rock. Along the final and most spectacular 600m, the rapids drop some 50m before the river resumes its normally placid onward flow. The Piteälven was used for timber-floating from 1858 until 1982, and in sections of rapids such as Storforsen, the river's course was straightened and deepened by blocking off its side channels with box-booms to allow logs to be floated down-river to sawmills.

We threaded a way across to the now semi-dry rocks of the Döda Fallet (Dead Falls) area, where the river was diverted from its natural, wide-spreading course to be channelled into a deeper float-way at the time of log-floating. The flat rocks now serve as a sunbathing terrace for tourists, though how such folk can lie there apparently indifferent to the thunderous roar of the rapids hurtling past nearby remains one of life's mysteries! The nature reserve includes sturdy wooden walk-ways immediately alongside this final 800m section of the falls enabling bird's eye viewing of this spectacular natural phenomenon. The sun drifted in and out of increasing cloud, and we stood at the walk-way's top viewing platform, looking directly across to the point at which the mighty river tumbled over the brink of the rapids, surging and boiling in foaming fury down its white-water passage with the sun lighting the rapids' sparkling waters (Photo 39 - Storforsen Rapids). We followed the board-walk down, and even in a dry year mid-summer when the river's flow was supposedly at its lowest, the churning waters of the rapids was still mesmerising, the patterns of water for ever changing and throwing up clouds of spray. Part-way down the rapids, and across an intervening area of rocky pathway under trees between sections of board-walk, the river's surging passage hurtled over one of the bed-rock thresholds more resistant to erosion, creating a series of spectacular falls (Photo 40 - Lower Storforsen). The board -walk, running the length of the rapids (see above left), can easily be taken for granted, but is in itself a remarkable work of construction which gives such an intimate view immediately above and alongside the rapids (Photo 41 - View from Storforsen board-walk) (see right). Pounded by the rapids' turbulence, especially in Spring, the structure must need constant maintenance.

We followed the board-walk down to the lower area where below the rapids the river turns to resume a more placid course along the lower valley. Here among the riverside vegetation we found Stone Bramble berries in fruit (Photo 42 - Stoneberry ripe fruits). Back up the board-walk, the sun's angle had now moved round so that its light just caught the clouds of spray welling up from where the rapids thundered over the rocky thresholds, to create a rainbow effect (Photo 43 - Rainbow over Storforsen). Looking down the length of the rapids from the top viewing platform, we were rewarded with spectacular lighting, the afternoon sun's light again catching the spray to produce further rainbow effect (Photo 44 - Storforsen rainbow). After such a memorable afternoon at Storforsen with its admirable board-walk giving such close views of the rapids, we returned along the Piteälven for a final night's camp at Älvsbyn.

Coming soon:  we shall now continue our southward journey following a series of zigzags routes inland and out to the east coast along the valleys of Sweden's major rivers, the Skellefteälven, Vindelälven, Ångermanälven and Indalsälven: firstly inland to Arvidsjaur, then back to the Bothnian coast at Skellefteå, on the way visiting the restored section of the former Linbanan mining cable-way that once transported ore to coastal smelters. We then travel down the lower Vindelälven river valley before looping inland again and finishing back at the coast at Örnsköldsvik, for at day out on Trysunda, one of the High Coast off-shore Baltic islands. Inland again, we shall visit the spectacular Döda Fallet dry falls created by a disastrous accident in the late 18th century on the Indalsävlen river. We shall visit the town of Sundsvall before moving on to Hudiksvall to stay for a couple of days with an old friend and her family. But that's a story for the next episode, coming soon.

Next edition to be published shortly

Sheila and Paul

Published:  26 November 2016

 

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