• ที่มีอยู่: เดื. - สิง.
• ระยะเวลา: 13 วัน
• กิจกรรม: ปีนเขา, ชมวิว, ทัวร์ถ่ายรูป, เวิร์คช็อปถ่ายรูป
• ความยากลำบาก: ง่าย
• อายุต่ำสุด: 18 ปี.
• ภาษา: English
• ไฮไลท์

  The Reykjavík Capital Area is the country's largest and most populated city and currently home to 211.282 people, that's two-thirds of the entire Icelandic population!

  Although it's one of the smallest capital cities in the world, it's still big enough to fit in six super-sized districts, with Reykjavík as the largest having a population of 121.230. Each district has its own elected council that governs the community and is responsible for the execution of legally determined projects.

  

  Reykjavík,

  A unique waterfall in the river Seljalandsá, about 30 km west from Skógar. It is 60 meters high with a foot path behind it at the bottom of the cliff, but with a thin cascade. It is the only known waterfall of its kind, where it is possible to walk behind it. The waterfall is very picturesque and therefore its photo can be found in many books and calendars.

  Access to the waterfall is from the farm of Seljaland along the Ring Road, Iceland's main highway. A little further to the west there are several other falls, among them the interesting Gljúfrabúi which is partially masked by its own canyon. Access to it is from Hamragarðar farm along the road, east of Markarfljót.

  Both of these "do-not-miss" attractions lie very close to the main Ring Road at the base of the Eyjafjallajökull Glacier, on the road leading in to Thorsmörk.

  

  Seljalandsfoss,

  SKOGAFOSS - WATERFALL

  Only a few kilometers away from the south shores of Iceland, lies the village of Skógar along the Southern Ring Road. It is a popular summer-resort centre surrounded by unusual scenic beauty. The breath-taking view of Skogáfoss waterfall and scenic surroundings and the snow-capped heights of two towering glaciers are Skógar's major summer attractions. There are two settlements by this name. One is Ytri-Skógar (outer or western Skógar) and the other Eystri-Skógar (eastern Skógar), located at a short distance from each other. Ytri-Skógar, commonly referred to as Skógar, is the main settlement. It is an old farm and has a church from 1890. It is located between the Skógá and Kverná rivers.
  The greatest attraction of Skógar is of course the beautiful 60-metre high Skogáfoss waterfall in the river Skógá. Like the legends of buried treasures of Egill Skallagrímsson in Mosfell near Reykjavík and Ketilbjörn in Mosfell near Skálholt, there is a similar legend about the settler Þrasi who is believed to have buried his chest of gold under the Skogáfoss waterfall.
  If the sun conditions are favourable - one can see a vivid rainbow in front of the waterfalls. The river below the falls holds a large salmon and char population and fisherman are seen here fishing July - October. The path leading to the top of the waterfalls continues following the river upstream - where numerous more dramatic waterfalls of sheer beauty are to be found. A great hike - to say the least!
  One of the finest folk museums in Iceland is situated in extraordinarily beautiful natural surroundings. The interesting local folk museum has a collection of over 6000 artifacts and examples of various types of dwellings in Iceland since the early times. The collection of tools and equipment used at land and sea is outstanding. The museum also has an old turf farmhouse, where guests can experience the standards of living in Iceland in past centuries.
  From Skógar the Ring Road runs eastwards along the foot of Mýrdalsjökull glacier, across the southern sandy plains and over glacial rivers, passes Seljavellir and continues along the soaring glaciated massive of Eyjafjöll and the two waterfalls Seljalandsfoss and Gljúfrabúi. From here runs a 10 km long trek along the river Skógá over the Fimmvörðuháls Pass between the Eyjafjallajökull and Mýrdalsjökull glaciers to the mountain oasis of Þórsmörk.
  Skógar is a place to explore the natural diversity of the south or, if the weather is good, to spend a holiday amid beautiful and rugged landscapes. It is also very close to the ocean and the unique black beach.

  

  Skógafoss,

  DYRHOLAEY

  Dyrhólaey is a 120-metre high promontory, not far from Vík. The place got its name from the massive arch that the sea has eroded from the headland. (The name literally means "door-hole"). When the sea is calm, big boats can sail through it. There has even been a maniacal daredevil pilot that flew through the arch with a small-craft airplane! From the top of Dyrhólaey there is a great view. The headland is thought to have been made in an underwater volcanic eruption late in the glacial period, not unlike the eruption of Surtsey. Several outcrops are in the sea, the highest one called Háidrangur ("High column") is 56 m. high. Dyrhólaey has been a natural reserve since 1978. The promontory is widely known among sailors as "Portland", and English trawler fishermen ubeach where one can climb (at your own risk). According to legend the Reynisdrangar needles were formed when two trolls were trying to drag a three-masted ship to land. When daylight broke they turned to stone. The Needles can be seen clearly from the village of Vík and are 66 meters above sea level at their highest. In one of the many caves here - there is a local legend about a monster having lived here for many centuries. The monster seems to have disappeared after a landslide over 100 years ago…sed to call it "Blow hole". There are also amazing rock formations all along the Birdlife here is abundant, with puffins and eider ducks being the most common species in the area. The lighthouse on the top of the cliff stands impressive and stoic in this often very windy area. Be careful not to go too close to the ledge of this dramatic cliff.

  

  Dyrhólaey,

  Reynisdrangar are basalt sea stacks situated under the mountain Reynisfjall near the village Vík í Mýrdal, southern Iceland which is framed by a black sand beach that was ranked in 1991 as one of the ten most beautiful non-tropical beaches in the world.

  Legend says that the stacks originated when two trolls dragged a three-masted ship to land unsuccessfully and when daylight broke they became needles of rock.

  Contemporary legends note the story of a husband who found his wife taken by the two trolls, frozen at night. The husband made the two trolls swear to never kill anyone ever again. His wife was the love of his life, whose free spirit he was unable to provide a home for; she found her fate out among the trolls, rocks, and sea at Reynisfjara.

  

  Reynisdrangar,

  Vatnajökull National Park was established in 2008. It includes the national parks in Skaftafell (est. 1967) and Jökulsárgljúfur (est. 1973) along with the Vatnajökull ice cap itself and extensive areas around it.

  Vatnajökull National Park is characterised by diversity on all fronts, be it landscape, biosphere, cultural remains or service levels. For simplification, however, it may be placed into two categories: uninhabited highland areas with limited services and lowland areas with higher service levels.

  The park‘s visitor centres are all located in lowland areas. Each of them has an exhibition about the park‘s nature and cultural heritage. Each also has a souvenir shop with special emphasis on local handicraft and products.

  In 2018, Vatnajökull National Park was nominated for inclusion in the World Heritage List. The nomination [PDF - 28 MB]is currently being reviewed by UNESCO.

  Vatnajökull National Park,

  Jökulsárlón glacier lagoon is one of the most famed and visited attractions in Iceland. Floating on the lagoon are enumerable icebergs that have broken off the resident glacier, creating an ever-changing scenery of incredible allure.

  The river Jökulsá connects the lagoon to the Atlantic Ocean, meaning that these icebergs eventually drift out to sea where they are polished by the waves before floating back to the black sands of Breiðamerkursandur. The name ‘Diamond Beach’ thus comes from the white ice on the black sand appearing like gemstones or diamonds, as they often glisten in the sun and sharply contrast their jet black surroundings.  

  

  Jökulsárlón,

  The Diamond Beach is a strip of black sand belonging to the greater Breiðamerkursandur glacial plain, located by Jökulsárlón glacier lagoon on the South Coast of Iceland.

  Here, the icebergs which fill Jökulsárlón glacier lagoon wash up on shore, standing dazzling and defiant in stark contrast to the black sand beach. It is, therefore, a favourite amongst photographers, nature-lovers, and wildlife-enthusiasts. Many seals call this beach home, and it is one of the best places in the country to see orcas from the shore.

  Safety at the Diamond Beach

  The Diamond Beach is a safe place for any responsible traveller; unlike at Reynisfjara, another South Coast black-sand-beach, sneaker waves and rip currents are not notorious for whisking unwitting tourists out to sea. However, there are still dangers to consider.

  The main one of these is the icebergs themselves. Under no circumstance should you climb upon an iceberg, due to their slippery surfaces and sharp edges.

  This is especially the case if the iceberg is at all in the water, as it could flip and trap you underneath, or else be pulled out to sea by a current with you on it.

  The risk of injury and illness in the form of hypothermia is so great that extortionate fines exist to deter any ‘rebels’ looking for a thrill-seek. These have only come about due to serious incidents, to protect not only tourists at the lagoon but guides and staff who may feel obligated to embark on a dangerous rescue if they see someone at risk.

  

  Diamond Beach,

  Scenic landscape, favorable weather conditions and a selection of hiking trails make Skaftafell an ideal destination for those who like to enjoy outdoor activities in Icelandic nature.

  Short and easy trails lead to waterfall Svartifoss and glacier Skaftafellsjökull, but for those who want to reach further out, the Morsárdalur valley and Kristínartindar mountain peaks are perfect in terms of distance and labour. Skaftfell is also the perfect base camp for those who seek to climb Iceland‘s highest mountain peak, Hvannadalshnjúkur.

  In 1967, Skaftafell National Park was established, but in 2008 it became a part of the newly established Vatnajökull National Park.

   

  Skaftafell ,

  Mývatn offers a unique natural environment. With large contrasts and small distances you can experience the most and the best that Iceland has to offer. Large open spaces with roads and walkways lead travellers to unworldly locations, where volcanic eruptions have played a crucial role in the formation of the landscape. Whether the plan is to enjoy the landscape, examine unique natural phenomena or take a closer look at the pant and bird life, Mývatn has it all. Furthermore the area offers a variety of services in accommodation, food and entertainment, based on years of experience and knowledge. A large number of travellers visit Mývatn in the summer, but many believe the lake and its surroundings to be no less impressive in the wintertime.

  Mývatn is the 4^th largest lake in Iceland, 37 km² in area. Its shores are indented with many coves and inlets and its surface is dotted with around 50 small islets and skerries. Midges (Chironomidae) are abundant and the ubiquitous swarms of these tiny flies give the Lake its name.

  The lake itself is very shallow, and the rays of the sun reach the lake bed over its entire surface. The ecology of the lake area is extremely diverse and interesting; one important characteristic of Mývatn, being the prolific growth and abundance of freshwater seaweed. On the bed of the lake are great quantities of diatoms, while, nearer the surface, Mývatn's famous arctic char weave their way between aquatic plants and little islets topped with fertile vegetation. 

  On and around the lake there is a teeming and varied birdlife, and Mývatn is the habitat of many kinds of lake and marsh birds. However, much of Mývatn's fame is due to the fact that, during summer, there are more different species of duck gathered on and around the lake than anywhere else in the world. Mývatn is a legally protected conservation area and appears on the register of internationally important wetlands, along with the Laxá river which flows out of the lake.

  

  Mývatn,

  DETTIFOSS WATERFALL

  The Dettifoss waterfall is with the greatest volume of any waterfall in Europe, 500 cubic metres of water per second plunges over the edge. Dettifoss is 45 m high and 100m wide. A nice hiking trail, 34km, goes along the canyon from Dettifoss to Asbyrgi. Camping possible in Vesturdalur.

  Road 864 goes from road 85 past Dettifoss on the east side towards road 1. This is a gravel road and driving speed depends on road conditions each time. Road 864 is closed durning winter time due to snow or wet condtitions (muddy road) and does not open until early summer (end of May).

  Gravel road 862 is on the west side of river Jökulsá. The road is passable for normal vehicles from Asbyrgi to Dettifoss, with Vesturdalur (Hljodaklettar) and Holmatungur between. Up until 2011 this road was categorised as a mountain road (F-road) but is now served as a gravel road. The conditions of gravel roads in Iceland can vary, so travellers are asked to be aware of road conditions at any time and adjust driving speed to the conditions.

  Road 862 is closed durning winter time, due to snow or wet conditions (muddy road) and does not open until late May or early June. From Dettifoss onwards south to road 1, on the west river bank, there is a new, paved road which is passable for all vehicles. This road is not in service from January until the beginning of April.

  

  Dettifoss,

  Goðafoss Falls

  Nicknamed by one local as ‘The Beauty’ in comparison to ‘The Beast’ of Dettifoss, the name Goðafoss could be translated roughly as The Waterfall of The Gods. An impressive site any time of year, in late spring, if you can catch it while there´s still icicles bedecking its sides, it’s a particularly otherworldly place to visit.

  
  History
  In the year 999, a holy man by the name of Þorgeir made Christianity the official religion of Iceland. To mark the occasion, he chucked some Pagan statues into the water here, making Goðafoss the famous symbolic site of Iceland´s conversion.

  

  Goðafoss,

  Aldeyjarfoss Waterfall

  (Pronunciation = Al-day-yar-foss)

  Though only twenty metres in height and a little off the beaten track, Aldeyjarfoss waterfall has symmetrical features and geologically interesting surrounds. Tumbling through a narrow passage into a wide basin, the concertinaed black basalt columns provide a stark contrast against the thrashing white foam, making it oft considered one of Iceland’s photographic gems.
  Aldeyjarfoss is one of most impressive waterfalls on the Skjálfandafljót River’s route from the Vatnajokull ice cap to Skjálfandi Bay. Others include Ingvararfoss, Hrafnabjargafoss, Barnafoss and the most famous, Goðafoss.

  
  Geology
  The land here is part of an apalhraun lava field, named Suðurárhraun, which was originally formed by eruptions, some 9500 years ago.  In Icelandic, hraun simply means lava. The official English terms for basaltic lava flows are taken from Hawaii – apalhraun is a platy lava flow known as ʻaʻā and helluhraun is a ropier kind of lava known as pāhoehoe.

  

  Aldeyjarfoss,

  Námaskarð Pass is a geothermal area on the mountain Námafjall, in north Iceland, less than half an hour’s drive from Lake Mývatn. It is located by Route 1, which encircles the country.

  Connected to the Krafla volcano system, Námaskarð is home to many hot-springs and fumaroles.

  Geography of Námaskarð
  Námaskarð is notable due to its barrenness; no vegetation grows on its slopes. This is due to the heat beneath the earth, the acidity in the soil, and poisonous fumes being expelled.

  That is not to say, however, that the site is dull; its life comes from the vivid colours that streak through the earth, dyed by the elements brought up with the steam. Expect to see shades of red, orange, yellow and green, particularly concentrated around the springs themselves.

  The air smells intensely of sulphur throughout the area, which, while unpleasant, is a constant reminder of the powerful forces at work beneath your feet. Though it would be damaging for your health to spend too long breathing it, a visit for a few hours will not cause any problems.

  While exploring Námaskarð, be sure not to touch any of the running water, as it is likely to be boiling. Also, give all the hot springs a reasonably wide berth, as the land surrounding them may be unstable, with scalding steam just beneath the surface.

  Námaskarð is about 400 metres (1312 ft) above sea level.

  Surroundings of Námaskarð
  Námaskarð is situated between the mighty waterfalls of the Jökulsá á Fjöllum river (which include Europe’s most powerful waterfall, Dettifoss) and the Lake Mývatn area, making it a natural part of anyone’s itinerary if they are exploring the north from Akureyri or Mývatn.

  Námaskarð,

  Namaskard hverir

  This spectacular high temperature area (410 m above sea level) is situated by road no. 1 by the Namaskard pass in the vicinity of Lake Myvatn. It is a prototype of such areas, consisting of stinking steam vents, solfataras and boiling mud pits. The whole area is metamorphosed by the geothermal activity and thick deposits of silica, gypsum and sulphur cover the ground. One has to be very careful crossing such areas, because the thin crust might brake.

  Unfortunately too many people have been severely burnt by stepping through. The almost pure sulphur of this area was exported during the last few centuries. These sulphur mines were considered the richest in the country and the so-called Reykjahlid-brothers, the proprietors of the area, are said to have become rich by processing the sulphur and exporting it.

  In 1563 the mines came into the possession of the Danish king and the sulphur processing continued with intervals to the middle of the 19th century. In 1939 a sulphur factory was built in Bjarnarflag, near the mines. Its operation came to an end after a few years. After that some entrepreneurs started building a factory on the spot and had some five or six boreholes sunk in the area to pipeline the steam to the factory. The foundations of the factory house had been built and the boreholes had been sunk, when the shareholders realized, that the end price of the product would be to high for the world market and decided not to continue with the project.

  

  Hverarönd,

  DIMMUBORGIR

  Dimmuborgir is an area of randomly strewn lava rocks and cliffs, surrounded by vegetation, such as low bushes and plants. Dimmuborgir is a place of surprises with its myriad forms and images, small caves and towering volcanic rock, pierced by natural apertures.

  The most famous of these formations is "The Church", aptly named, as this is a cave, open at both ends and with a dome-like ceiling.

  

  Dimmuborgir,

  Hveravellir (The Hot Spring Fields) is a very interesting low temperature area at the northern edge of the lava field Kjalhraun. It is a popular stopover with tourist huts, a meteorological watch (was occupied the whole year until 2009) and a man made bathing pool. The old route across the lava field continued through the thermal area, which is also frequently referred to in the Sagas. Attraction: The Bony Mound. The hot spring area has been protected since 1965 and people are kindly asked to stay on the boardwalk across it.

  The thermal activity can also be seen in the lava field, where there are steaming chasms.

   

  Hveravellir,

  
  Kerlingarfjöll
  Kerlingarfjöll peaks.jpg
  The peaks of the Kerlingarfjöll area, close.
  Highest point
  Elevation    1,477 m (4,846 ft)
  Coordinates    64°39′N 19°15′WCoordinates: 64°39′N 19°15′W 
  Geography
  Kerlingarfjöll is located in IcelandKerlingarfjöllKerlingarfjöll
  Location of Kerlingafjöll within Iceland
  Location    Iceland
  Kerlingarfjöll is a 1,477 m (4,846 ft) tall mountain range in Iceland situated in the Highlands of Iceland near the Kjölur highland road. They are part of a large tuya volcano system of 100 km2 (39 sq mi). The volcanic origin of these mountains is evidenced by the numerous hot springs and rivulets in the area, as well as red volcanic rhyolite stone of which the mountains are composed. Minerals that have emerged from the hot springs also color the ground yellow, red and green.

  The area was known formerly for its summer ski resort, but this was dismantled in 2000. Since 2000, Kerlingarfjöll has been operated as a highland resort, offering accommodation and food services to guests in the area.

  It was on March 17 in 2017 that the Iceland Monitor wrote that Kerlingarfjöll Mountains and geothermal area were being turned into a nature reserve. Although parts of the place already had protection, after made into reserve, all the whole 367 square kilometres are to be under the protection of the state of Iceland. Earlier, there had been thoughts of using the 140 degree Celsius hot springs as a geothermal power plant. It had already been popular of course with hiking and the tourists.

  

  Kerlingafjöll,

  LANDMANNALAUGAR - NATURE RESERVE

  Landmannalaugar derives its name from a hot pool that rises from under the Laugahraun lava field. Landmannalaugar has been a stopping point for people for centuries, and the mountain shepherds on Landmannaafréttur have stayed there while herding sheep off the mountain for as long as there have been reports of such travel.

  Many beautiful mountains can be seen from Landmannalaugar: Barmur, Bláhnúkur, Brennisteinsalda, Suðurnám and Norðurnám. There are considerable deposits of rhyolite, obsidian and rhyolite lava in the area, and the Landmannalaugar landscape is famous for its colourfulness and unique environs.

  The start of one of the most popular hiking trails in Iceland, Laugavegurinn, is at Landmannalaugar. The trail proceeds along Hrafntinnusker, Álftavatn, Hvanngil, Emstrur and ends in Þórsmörk.

  Ferðafélag Íslands (the Iceland Touring Association) provides facilities, such as showers and accommodation, for travellers at Landmannalaugar. In addition, there is a horse rental and a small café operated during the summer.

  

  Landmannalaugar,

  HAIFOSS

  The waterfall Háifoss is situated near the volcano Hekla in the south of Iceland. The river Fossá, a tributary of Þjórsá, drops here from a height of 122 m. This is the second highest waterfall of the island.

  From the historical farm Stöng, which was destroyed by a volcanic eruption of Hekla in the Middle Ages and reconstructed, it is possible to hike to the waterfall along the Fossá (5 to 6 hours both directions). Above the waterfall, there is also a parking lot, so the hiking can also be made in the other direction.

  

  Háifoss,

  Ljótipollur is an explosion crater and crater lake in the south Highlands. Its name means ‘Ugly Puddle’, despite the fact it is an incredibly beautiful site. It is part of the Veiðavötn volcanic area.

  Ljótipollur is located in the southern highlands, in the Fjallabak Nature Reserve. It is most easily reached by those who go to Landmannalaugar, and take the four-hour hike to it and back.

  Landmannalaugar is a highland oasis, open throughout the summer months, with colourful rhyolite mountains and hot springs. It is a hiker’s paradise, marking one end of the Laugavegur trail that ends in Þórsmörk. Though this journey takes four days, Ljótipollur is a perfect example of a hike within Landmannalaugar that can be done within hours.

  Those in Landmannalaugar who wish to take a shorter hike should take those to Mount Brennisteinsalda or Mount Bláhnúkur.

  Ljótipollur is a beautiful feature, with blue waters, green vegetations growing up and down its slopes, and vividly coloured red lava rock surrounding it.

  Ljótipollur,

  Bláhylur / Hnausapollur

  Lake Hnausapollur is on of two crater lakes of the Veidivotn System south of River Tungnaa.  The other one is Lake Ljotipollur.
  
  The access by car is easy and the anglers have to walk down a steep scree inside the crater and back up again with the catch.  Lake Hnausapollur is situated just north of Mt Tjorvafell and Lake Frostastadavatn, only a stone’s throw away from the mountain track between Sigalda and Landmannalaugar.  Permits are sold at the lodge at Landmannahellir or on the internet.

  Bláhylur,

  Hjalparfoss is a beautiful, two stepped waterfall near the confluence of Rivers Thjorsa and Fossa in the Thjorsa Valley. The surrounding area is called Hjalp (Help), because the travellers across the Sprengisandur Route found great help in reaching a vegetated area to graze their horses after a long journey in the barren interior.

  As elsewhere in the valley, the signs of the eruptions of Mt. Hekla are very prominent by the waterfall, ashes everywhere

  The National Energy Authority has spent much time and money to turn the valley green again with excellent results.

  Hjálparfoss,

  Sigöldugljúfur used to be a river way, but when the hydro electric damn Sigölduvirkjun was built, the water from the waterfall Sigöldufoss was directed into the damn, forming the "Valley of tears" where countless waterfalls meet and fall together down the cliffs and into the river below.

  Once every 5 years the damn closing the canyon is opened up for maintenance and then Sigöldufoss is visible again, for only a week. 

  

  Sigöldugljúfur / Valley of tears,

  Mýrdalsjökull, Icelandic for "(the) mire dale glacier" or "(the) mire valley glacier") is an ice cap in the south of Iceland. It is to the north of Vík í Mýrdal and to the east of the smaller ice cap Eyjafjallajökull. Between these two glaciers is Fimmvörðuháls pass. Its peak reaches 1,493 m (4,898 ft) in height and in 1980 it covered an area of 595 km2 (230 sq mi).

  The icecap of the glacier covers an active volcano called Katla. The caldera of the volcano has a diameter of 10 km (6 mi) and the volcano erupts usually every 40–80 years. The last eruption took place in 1918. Scientists are actively monitoring the volcano, particularly after the eruption of nearby Eyjafjallajökull began in April 2010. Since the year 930, 16 eruptions have been documented.

  The Eldgjá, a volcanic eruption fissure about 30 km (19 mi) long, which erupted in the year 936, is part of the same volcanic system.

  Before the Hringvegur (the main ring road round the island) was built, people feared traversing the plains in front of the volcano because of the frequent jökulhlaups (glacial floods) and the deep rivers to be crossed, although the road is still vulnerable to major events. Especially dangerous was the glacial flood after the eruption of 1918 when the coastline was extended by 5 km (3.1 mi) by laharic flood deposits.

  Mýrdalsjökull is an exceedingly wet location, with models suggesting it receives more than 10 metres of precipitation annually.

  Mýrdalsjökull,

  ELDGJA CANYON

  Between Kirkjubæjarklaustur and Landmannalaugar, the eruptive fissure Eldgjá is to be found. Eldgjá is a 40 km long eruptive fissure, 600 meters wide in many places, and up to 200 meters deep, formed in a gigantic eruption in 934. From Eldgjá, extensive streams of lava have flowed through Landbrot and Meðalland, reaching sea at Alviðruhamrar in Álftaver. The lava-field is believed to cover 700 km², which makes it one of the vastest lava-fields on earth since the last ice age. Eldgjá is believed to belong to the same crater system as Katla. Eldgjá is a unique natural phenomenon and is listed as natural remnants.

  Eldgjá is a part of a volcanic fissure that stretches from Mýrdalsjökull almost to Vatnajökull. Eldgjá is about 8 km long, 600 m wide and up to 150 m deep. It was formed in the year 939 during one of the largest volcanic eruptions in Iceland in historical times. Eldgjá‘s main attraction is the waterfall Ófærufoss, located a short walking distance from the area‘s car park.

  Eldgjá

• ไกด์ถ่ายภาพมืออาชีพ

• การเดินทางด้วยพาหนะที่สะดวกสบาย

• ที่พักในโรงแรมหรือเกสท์เฮ้าส์ ห้องพร้อมห้องน้ำส่วนตัว

• อาหารเช้า และ อาหารเย็นเป็นกลุ่มในวันที่ 1 และ วันที่ 12

• อาหารเที่ยงทุกมื้อ และ อาหารเย็นในวันที่ 2 ถึงวันที่ 11

• เครื่องดื่มแอลกอฮอล์, อาหารว่างและเครื่องดื่ม

• ตั๋วเครื่องบินระหว่างประเทศ

• หลังจากที่คุณสมัคร, เราจะส่งคำแนะนำเกี่ยวกับอุปกรณ์กล้องถ่ายรูปและอุปกรณ์ที่จะเป็น.

10-22 Jul 2020 - Guided by Oli Haukur
7-19 Aug 2020 - Guided by Oli Haukur

We highly recommend that you get a travel and medical insurance. Your own domestic medical insurance and private health scheme will not cover you whilst you are overseas.

The tour is always dependent on weather, as the Icelandic weather can indeed be highly unpredictable. Likewise, visits to ice caves are dependent on favorable conditions, and indeed the ice caves themselves are not permanent. When it comes to the Northern Lights, while they are most likely to be seen between September and April, there is no guarantee that they will appear on a given day.

If you cancel and the Workshop is otherwise filled, we will refund you the full amount you have paid towards the tuition, minus a $300 service charge. If you cancel and the Workshop does not fill, then you will be refunded according to the following schedule, based on the full fee of the Workshop:

Greater than 60 days from the start date of the Workshop: full refund minus $300 fee.
45 days or more: 75% refund
30 days or more: 50% refund
Less than 30 days: no refund

Refunds will be paid by the same method that the original payment was made. Refunds will be initiated within 72 hours of the time that the request is approved.