Sunday, 3 September 2023

Day 8: The Long Way to Reykjavík

Day 8 Route (Hamarsvöllur to Reykjavík)

Snorrastofa museum in Rekholt

Day 8 was our final day in Iceland. We stayed the night at the Hamar Hotel in Hamarsvöllur just 79 km (1 hour 10 minutes) away from the Baron Fosshotel in Reykjavík. We began the day in Reykholt by visiting Snorrastofa and its surrounding grounds. It was an interesting place and a good start to the final day.  

Next up was the Hraunfossar (Lava Falls). Hraunfossar is a series of waterfalls formed by rivulets streaming out of the Hallmundarhraun lava field that flowed from an eruption of one of the volcanoes lying under the glacier Langjökull.

Hraunfossar Falls

Barnafoss on Hvítá River

Barnafoss is a rapid waterfall and a short walk from the Hraunfossar Falls. Barnafoss translates to the Children’s Falls and has an Icelandic folklore tale associated with it (Barnafoss Legend). The contrast between Barnafoss and Hraunfossar is striking; one is dramatic and angry, and the other one is serene and soothing.

The next stop was Deildartunguhver, the highest-flowing hot spring in Europe, located in Reykholtsdalur. It has a flow rate of 180 litres (380 pints) per second. The water at Deildartunguhver hot spring is a constant 97 degrees Celsius (207 degrees Fahrenheit). Much of the water at Deildartunguhver is used for heating Icelandic homes in the surrounding area. 


Deildartunguhver Hot Springs

Due to unscheduled delays while exploring the Snæfellsnes Peninsula the previous day, we returned for another afternoon of exploring. One stop was the Bjarnarfoss Waterfall (Bear Waterfall), a 262-foot (80-meter) waterfall, easily visible from Route 54. As with most Icelandic sites, there are locale legends associated with this beautiful cascading waterfall (Bjarnarfoss Legend). 

Bjarnarfoss waterfall

Other stops on the Snæfellsnes Peninsula included the Lóndrangar basalt cliffs (nicknamed the Rocky Castle), an abandoned farmhouse at Dagverðará, various craters and of course another view of Snæfellsjökull.  The two pillars at Lóndrangar are all that remains of a volcanic crater due to erosion.  The abandoned farmhouse is great stop for photographers so we weren't the only visitors that day.  After one last stop for a final view of Snæfellsjökull, we headed into Reykjavík.

Lóndrangar basalt cliffs (aka The Rocky Castle)
  
Abandoned Farmhouse of Dagverðará at Snæfellsnes

Crater on Snaefellsnes Peninsula (near Bjarnarfoss Waterfall)

Final View of Snæfellsjökull

A Touch of Frost (near Barnafoss Falls)


Deildartunguhver Geothermal Energy Facility

Gamla Kirkjan, Rekholt (ca 1887)

Our arrival in Reykjavík was late afternoon, so we only had time for was a walk around the area.  At least one additional day was required to visit Reykjavík properly.  One reason to return in the future!  Our final photograph taken in Iceland was of a gyrfalcon (Iceland's national bird) on Laugavegur 70 Street. This beautiful work was done by Örn Tönsberg (better known as Selur One), one of Reykjavík’s most prolific street artists. 

Goodbye Iceland, Hello Faroe Islands!  

Gyrfalcon on Laugavegur 70 Street

Video Clip

Monday, 8 May 2023

Iceland Day 7: My Comeuppance!

Day 7 Route (unpaved section highlighted in red)

Kattarhyggur Bridge (Cat´s Arch)

The distance between our hotels on Day 7 was just 212 kilometres or 2.5 hours away, so we decided to explore the Snæfellsnes Peninsula that afternoon. I decided to trust my memory instead of writing down the intended route. That was to be my comeuppance; I made the mistake of saying to turn onto Route 55 (to get to Route 54) instead of Route 56. Route 55 was a gravel road, albeit in very good condition. At that time, I assumed that Route 54 was all paved, so it would not be a problem. Oops, it turned out that ~ 75 km of Route 54 was unpaved and we had to drive 40 kms on a rough section before returning to paved road. Two hours on gravel roads was unanticipated and unscheduled. All I have to say for myself is that it wasn't a gravel switch-back going up a mountain through the fog without guard rails. (https://sandrawhiteway.blogspot.com/2022/12/iceland-day-4-dramatic-skies-waterfalls.html). 

Our first stop since leaving Skagafjörður was at the Kattahryggur bridge, commonly known as the Cat´s Arch.  It was one of the first concrete bridges built in Iceland along the old Akureyri Road. This road was originally used for horse-drawn carriages and later motorized vehicles. The subsequent stops had beautiful views of the Baula and Litla-Baula Mountains; which are laccoliths, a type of intrusive rock with a domed top surface and a level base. These mountains are 3.4 million years old. 

Baula and Litla-Baula Mountains from Glanni Waterfall Trail.

Coming from a place where storytelling or "spinning a yarn" is so deeply woven into our cultural fabric tends to make people appreciate the stories of other cultures. I think Iceland could take the storytelling crown. Every location in Iceland, whether it's a waterfall, a mountain or a settlement, seems to have a story associated with it that somehow incorporates gods, elves, trolls and other mythical creatures. Our next stop was to visit Glanni Waterfall on the Nordura River.  Rumor has it that Glanni is home to elves and trolls, but you are more likely to encounter salmon since the Nordura River is known for great salmon fishing. 

Glanni Waterfalls on the Nordura River

Next up was our adventure around the Snæfellsnes Peninsula. The first stop was a quick view of Eldborg Crater (translated means Fortress of Fire or Fire City). This crater presents a regular oval shape with a diameter of 200 metres and a depth of 50 metres. The surrounding lava fields were created by eruptions 5,000 to 8,000 years ago. Eldborg Crater is a 5 kilometres (3 miles) round trip hike from Snorrastaðir farm.

Eldborg Crater (Fortress of Fire)

A couple of minutes past our stop at Eldborg Crater, we began our alternative route to the north shore of the Snæfellsnes Peninsula. We transversed the peninsula via gravel roads (Route 55 and part of Route 54). The views were lovely but realistically stopping and taking Route 56 immediately would have been the sensible decision due to time constraints. In addition, the rental vehicle was small, a Kia Ceed. We saw a lovely church in a field by itself. Google maps identified it as Breiðabólsstaðarkirkja, either there are two churches with the same name or this one is called something else. Approximately 8 kilometres further we stopped to photograph a boat wreck across the water on an island. 

Breiðabólsstaðarkirkja (maybe but google maps says it is)
 
Boat Wreck on an Island 

It was along the unpaved section of Route 54 that we stopped to photograph one of the many stone cairns that we had seen. These stone cairns are ancient route markers made from lava rocks. In Iceland, these cairns (steinvarða) were traditionally placed along single-track roads to mark trails and date back to the 9th and 10th centuries. Tourism necessitated Icelandic Authorities to institute rules and rule 4 was “never dislodge stones or build cairns”. This article explains the reason and necessity for rule 4.  (https://icelandmonitor.mbl.is/news/nature_and_travel/2019/07/05/tourists_warts_removed_by_park_rangers/)

Stone Cairns (Steinvarða)

Eureka we hit pavement again as Route 56 joined Route 54. One of our stops was Kirkjufell (also known as Arrowhead Mountain in Game of Thrones) and when we arrived it was crowded. We avoided the crowds the best we could, got the photograph and continued on our way.  Kirkjufell is very picturesque and while we would have also liked to have included Kirkjufellsfoss waterfall in a photo, crowds made that impossible.  Like many beautiful spots in Iceland, I suspect the optimum times to photograph them would be sunrise and sunset and not just for the ideal light conditions.

Arrowhead Mountain in Game of Thrones (AKA Kirkjufell)

Our next major stop was Hellissandur, a fishing village dating back to the 16th century located on the north-western point of the Snæfellsnes Peninsula. Our reason for stopping here was decidedly modern; street art. Street art transformed Hellissandur's closed and abandoned buildings due to the fishery downturn into beautiful and colourful works of art.  A few pieces are showcased below.  (https://vimeo.com/311365999). 

Arctic Tern on Bird House by Ban Pesk 2019

Fears Conversation by Ban Pesk 2018

Terrors of Fróðá by Natalia Moguel, 2018

Bardur Protector of the Snaefellsnes by Camilo Arias, 2018


Crazy Birds by Ban Pesk , 2018

Bárðar Saga (Half Human Half Troll) by Nikki 10, 2018

This was the point where our side trip along Route 56 caught up and the time crunch had arrived.  We headed to our hotel outside of Borgarnes to prepare for our last day in Iceland.  A few quick photo stops was all that time allowed.

View of Snæfellsjökull 

Video Clip

Sunday, 15 January 2023

Iceland Day 6: Reflections

 

Lake Ljósavatn, Lake of Light

Day 6 was a day of reflecting on our first 5 days in Iceland, enjoying the views as we travelled from Reykjahlíð to Sauðárkrókur. Day 5 had been an incredibly busy day, so we left later than normal and took our time as we headed towards Sauðárkrókur. The landscape along this section of the trip was not as dramatic (though still beautiful) as previous days and that provided a respite from landscape sensory overload.  The day started out as cloudy with sunny breaks and ended with rain showers, not unusual for our time in Iceland.  

Day 6 Route


Wooden Sculpture
Berjaya Mývatn Hotel
Goðafoss Waterfall and Lake Ljósavatn

Our first stop was a Lake Mývatn Viewpoint, only us enjoying a last goodbye to the Lake Mývatn area. Our second stop was a quick return to the magnificent Goðafoss Waterfall in the Bárðardalur Valley, mid morning just prior to the arrival of tour groups.  

Next up was Ljósavatn, a lake in Ljósavatnsskarð Pass near the mouth of Bárðardalur Valley. The light and weather conditions were perfect for taking pictures of lake reflections of the surrounding mountains. This was such a beautiful place, our stop was longer than normal, pure relaxation. Lake Ljósavatn was formed because of volcanic eruptions and the resulting lava blocking a depression or valley.   

Lake Mývatn Viewpoint


Goðafoss Waterfall in the Bárðardalur Valley


Eyjafjörður Fjord

From Lake Ljósavatn we traveled to Akureyri, bypassing the Vaðlaheiðargöng Toll Tunnel. We took Route 83 and 84 crossing the mountains over the Víkurskarð pass. As we were traveling in early September and had mild weather, this route was safe from snow at this time while offering a scenic view of the Eyjafjörður Fjord. Akureyri is located on the Eyjafjörður Fjord in North Iceland, known as ‘The Capital of the North’ is a mere 100 kilometres (62 miles) from the Arctic Circle.

View of Akureyri from Across the Eyjafjörður Fjord


Öxnadalur Valley

After leaving Akureyi and heading west, route 1 passes through the 30 km Öxnadalur Valley. The most prominent feature of Öxnadalur Valley is the Hraundrangi Spire in the Drangafjall ridge that has an elevation of 1075 meters (3,527 ft), 80 meters (260 ft) higher than other points in the ridge. The Hraundrangi Spire and the Drangafjall ridge are what remains of Háafjall Mountain after it collapsed in a massive rockslide near the end of the Ice Age. 

The Hraundrangi Spire in the Drangafjall Ridge

Views of the Öxnadalur Valley


Glaumbær Turf Houses

Our next stop was Glaumbær Turf Houses. In the past, everyone in Iceland would have lived in a turf house, regardless of social standing. The Glaumbær turf house was occupied until 1947, when it was declared a protected site and a farm has been located on the site since the settlement of Iceland in approximately 874. The style of the buildings at Glaumbær date back to the 18th and 19th centuries with the oldest dating back to ~1750 and the most recent from 1876-79. The Turf Houses were built out of stone, wood, and of course, turf. Turf construction evolved in Iceland owing to acute shortage of large trees (acute is an apt describe of its tree status). The buildings at Glaumbær are a thin wooden shell (the wood would have been imported), separated from each other and insulated by thick walls of turf, and roofed with a thick layer of sod. The design of the turf houses had to take into practical considerations of wet and dry periods on the turf and sod. The Glaumbær Turf Houses are well worth a stop, a step back into Iceland's history. This site has useful information of the turf house construction as well as the farm's history (https://nat.is/glaumbaer-skagafjordur-folk-museum/ ).

Glaumbær Turf Houses

Glaumbær Turf Houses

Glaumbær Turf Houses

Glaumbær Turf Houses

Glaumbær Turf Houses

From Glaumber we headed to the Snæfellsnes Peninsula.

The following websites provide additional information on various topics concerning Iceland:

Tuesday, 3 January 2023

Iceland Day 5: Variety is the Spice of Life

Day 5 Route or Variety is the Spice of Life 

Canyon Moira
Day 5 was a beautiful day from start to finish with varying vistas coupled with great weather. Waterfalls, volcanic desert, geothermal landscapes, lakes, canyons, and craters were on tap for the day. Driving between Egilsstaðir and Goðafoss, you pass through a landscape change around every corner making this one of the most beautiful parts of our Iceland Journey.

Canyon Moira

Our first stop after leaving Egilsstaðir was the Canyon Moira, a beautiful canyon just off highway 1, that has little or no signage. It is a short hike to the canyon bridge, through a gated trail that is accessible but lifting the latch on the red gate. Now I had seen beautiful pictures of blue-green water in Canyon Moira but as the Jökulsá á Dal, is a glacial river, mud and silt are a normal occurrence as well. In fact, Jökulsá á Dal was the muddiest of Icelandic rivers, carrying approximately 112 tons of clay and sand to the ocean daily. While the Kárahnjúkar Hydroelectric Power plant has reduced the amount sediment and silt entering the river, my visit shows that significant amounts are still transported via the river to the ocean, depending I suspect, upon the amount of water released from Kárahnjúkar dam on any day.

The pedestrian Bridge over the Jökulsá á Dal River at Canyon Moira

Rjúkandafoss

Next up was another series of waterfalls collectively know as Rjúkandafoss. It is one of the tallest waterfalls in Iceland with an overall height of 139 meters (456 feet) when including all in the series of the waterfalls, thus making it easily visible from the road.

Rjúkandafoss along Highway 1

Alternate View of Rjúkandafoss 

Volcanic Desert

View from Parking de la Chaise Blanche, North East Highlands

Our rental vehicle was a car so travel along Iceland's infamous F roads was forbidden and a car would have been unsuitable to that environment. While the Ring Road technically does not traverse the Highlands of Iceland, driving from Egilsstaðir to Reykjahlíð you pass through a small offshoot of Iceland's Highlands (Northeast Highlands). The main portion of Iceland's Highlands are located on a sparsely inhabited plateau, an area that is barren, devoid of life and is a volcanic desert. Do not get me wrong there are Highland areas I would love to see, next time with the aid of a high clearance 4x4 and more time.

Our first stop was at the "Parking de la Chaise Blanche". It is probable that the large white chair has "bite the dust", having succumb to the harsh environment in which it was placed. The surrounding area was so devoid of life it is easily understandable why NASA conducted moon training missions in Iceland. Water infiltrates the ground so quickly in this type of environment that it is unavailable for plant growth resulting in a surface of grey, black, or brown earth, lava, and volcanic ashes. While the landscape may at first seem sparse, it is an incredibly diverse landscape that includes glaciers, geothermal hot springs, spectacular ice caves, stunning waterfalls and is an active volcanic landscape. Its this incredibly diverse, fascinating, and unique landscapes that so intrigues visitors to Iceland.  

Volcanic Desert Landscape of the North East Highland

A mere 5.6 kms (3.5 miles) down the road is the Beitarhúsið cafe. The building was what caught our interest, but the warning sign was the revelation. In the parking lot, a large government sign warning about continuing down the road as it was a F road and 4x4's were required. Additional insurance was strongly recommended such as gravel protection and a Super Collision Damage waiver. Also, it noted that most rental cars do not have an insurance for the undercarriage damage and undercarriage damage can occur on the F roads. We carried full insurance and are very thankful we did as two weeks later, many cars were damaged from high winds that pummeled northeast Iceland. In one of the photos in the linked article, most of the signs I mentioned above are missing and cars are severely damaged (https://www.ruv.is/frett/2022/09/26/worst-storm-in-living-memory).

Beitarhúsið

 Dettifoss and Selfoss

Dettifoss, Selfoss, and Hafragilsfoss are located on the Jökulsá á Fjöllum River which flows from the Vatnajökull glacier and is in the Vatnajökull National Park in northeast Iceland. We did not visit Hafragilsfoss. Dettifoss is one of Europe’s most powerful waterfalls, second actually in terms of water flow. While you can visit both sides of the river, the west side road is paved. We attempted the east side but decided it was a not safe to drive for the vehicle we had rented. The east side was in rough shape and turned out to be the roughest unpaved road we tried in Iceland. The west side road (Dettifoss Road) is paved and as such will have more tourists. We still got great photos and were not subjected to hoards of tourists. 

Returning to Route 1 along Dettifoss Road, you could see the steam coming out of the vents at Hverir Geothermal Area, our next stop.

Dettifoss from West Side

Selfoss from West Side

Hverir Geothermal Area

The Hverir Geothermal Area is at the foot of Námafjall mountain, part of the Krafla volcano fissure zone. Hverir is one of the most active geothermal areas in all of Iceland, so expect, smoking fumaroles and boiling mud pots all surrounded by sulphur crystals of differing colours. And of course, the overwhelming smell of rotten eggs. Hverir is atop of the Mid-Atlantic Ridge; the boundary where the North American and Eurasian tectonic plates meet and separate. 

The gas and heat observed at Hverir is generated approximately 1,000 meters (~3200 feet) below the surface, where cold groundwater seeps down to the magma layer and is superheated to above 200 °C (390 °F). Obviously sticking to marked trails is essential for safety reasons. There is a hiking trail up the Námafjall mountain. Due to timing constraints, we were unable to hike it, but I suspect it will provide some interesting views of Hverir. 

Námafjall Mountain and the Hverir Geothermal Area

Bubbling Mud Pools
Smoking fumaroles (no not manmade)

Hverfjall

Hverfjall volcanic crater is a tephra explosion crater or tuff ring volcano, a kilometer (3280 ft) in diameter and about 396 metres (1300 ft) high. The volcano which erupted in 2500 BP is part of the Krafla fissure swarm. Hverfjall is a popular hiking destination and based on our experience timing is critical if you wish to hike it. When we arrived at the parking lot, it was full of both cars and tour buses. The hiking trail around the crater was crowded. We decided to head onto our next destination a little further down the road. 

Hverfjall Volcanic Crater


The Skútustaðagígar Pseudo Craters 

The Skútustaðagígar pseudo craters are a natural phenomenon that occurs because of hot lava flowing over cool, wet grounds resulting in the pressurization of the earth from flowing lava, rather than being caused by the volcanic eruptions. Steam becomes trapped under the lava, producing extreme pressure. Steam explosions are triggered when pressures exceed a certain threshold, creating depressions in the ground known as pseudo craters. Pseudo craters are a rare phenomenon found only in Iceland, Hawaii, and the Azores islands. The biggest pseudo craters in Iceland are the Skútustaðagígar pseudo craters in the Mývatn area in North Iceland and were formed during the eruption of Lúdentaborgir and Þrengslaborgir around 2,300 years ago.

Skútustaðagígar Pseudo Craters

Mývatn Lake and a View of Several Pseudo Craters

Goðafoss and Geitafoss


As the day 5 ended we visited the beautiful Goðafoss (Waterfall of the Gods) located on the Skjálfandafljót River, the fourth-largest river in Iceland. It is one of the most spectacular waterfalls in the country, falling from a height of 12 meters (39 feet) over a width of 30 meters (98 feet). Of course, like many sites in Iceland there is a related legend (https://glacialexperience.is/the-historical-godafoss-waterfall-in-north-iceland-the-waterfall-of-the-gods/.). While Geitafoss is the smaller downstream sibling to Goðafoss, it is located on turbulent section of the river making it small but mighty. The name, Geitafoss or Goats' Fall stems from a farmer who herded his sheep and goats near this location. 

Goðafoss in the Early Evening

Geitafoss the smaller downstream waterfall from Goðafoss