WONDERS OF ICELAND | The country that looks like another planet

Iceland, where fire and ice coexist. Despite being a small country, it's  filled with astonishing natural wonders. Here, nature reigns over man.

The intense volcanic activity  has crafted a unique terrain. Landscapes seem from distant planets. In this documentary, we'll explore  Iceland's most amazing places.

A journey to the most remote  and hidden enclaves on Earth. Fagradalsfjall It's a volcanic system located in the Reykjanes  Peninsula, in the country's southwest. But it's not just one volcano, rather a  collection of several cones and fissures.

It lies in a tectonically active area, where  the Eurasian and North American plates diverge. Its formation began during  the last glacial period, indicating it emerged under a layer of ice. Initially, the lava erupting from  a volcano is bright red and exceeds 1000 degrees Celsius or 1800 degrees Fahrenheit.

As the lava flows and comes into contact with  air, it cools quickly, forming a solid crust. Accessibility from Reykjavik  has turned Fagradalsfjall into a site frequently visited by the curious. During eruptions, spectacular rivers of fire  and formations of fresh lava are created.

However, after an eruption, the levels  of volcanic gasses are dangerous. After a while, it seems safe, but there  might be burning lava beneath a thin layer. Litli-Hrutur This volcano is part of the Fagradalsfjall system.

When Litli-Hrutur erupts, lava  bursts through ground fissures. Instead of a violent explosion, the magma  flows smoothly, creating lava streams. A line of fire is visible, with  lava emerging from a linear crack.

Pieces of cooled lava  accumulate around the fissures. Over time, volcanic materials  rise and form a volcanic cone. Gradually, a more stable structure forms, with a  central crater acting as the main lava exit point.

During the eruption, the flows  extend, leading to vast lava fields. Geysir Geothermal Area Considered one of the most spectacular  geothermal fields in the world. The Haukadalur valley, where it is located,  is a highly active geothermal area.

It's filled with hot springs, mud pits, and  geysers, with a surface marked by vibrant colors. The great Geysir has had periods of  activity and inactivity over the years. Earthquakes often reactivate it, though  its activity decreases again as years pass.

In contrast, the geyser Strokkur erupts every  few minutes, shooting huge columns of hot water. In geothermal areas like this, hot magma  is close to the surface, heating the rocks. Water heats up, increasing  pressure in the geyser's conduit.

Upon reaching an unsustainable pressure level,  hot water and steam are expelled forcefully. Thingvellir National Park A site of historical and geological significance. This is where Icelandic democracy originated, with  the establishment of the first parliament in 930.

But what's truly captivating  is its location at the point where the North American and Eurasian  tectonic plates slowly drift apart. In Thingvellir, this process occurs on  land, allowing for direct observation. The tension and movement between the  plates has created numerous fissures.

The most astonishing is Silfra, a channel filled  with meltwater from the nearby Langjökull glacier. The water is so clear because it has been  filtered for decades through lava fields. This clarity earns it a rank among the  world’s best spots for cold-water diving.

Visibility is so good that divers feel  like they are flying over an abyss. One might say they are swimming  between two continents. Vatnajokull In terms of area, it's the  largest glacier in Europe.

A vast ice cap covering about 8  percent of Iceland’s territory. Its icy mantle spreads over mountains, valleys,  and even reaches the ocean at some points. It has multiple glacier tongues that extend from its central mass to the  valleys and lowlands below.

In areas where the ice is  thicker, a bluish hue appears. Fissures open perpendicular to the  glacier's flow, like a natural artwork. To geographers, these are known as "crevasses".

They have formed due to stresses  and compressions in the glacial ice. In each area of Vatnajökull,  the crevasses look distinct. They are more visible during the warmer  months, when the glacier’s surface melts.

This leads to meltwater rivers and streams. They can carve intricate paths through the  landscape, creating mesmerizing patterns. The water’s celestial hue is caused by the fine particles of glacial flour  that remain in suspension.

Jokulsarlon Glacier Lagoon Relatively young, this body of water  began forming about a century ago due to the retreat of the Breidamerkurjökull  glacier, an extension of Vatnajökull. It contains numerous detached  icebergs that float around the lake. They vary in shape, size, and color.

Some display an intense blue color, a result of ice compression over  hundreds or even thousands of years. Others appear white, indicating  they contain air bubbles in the ice. Additionally, Jökulsárlón is a prime spot  for seal spotting, especially in winter.

It is said to be a paradise for them, as  there are no predators like orcas or sharks. The lake is connected to the  Atlantic Ocean via a short river. Icebergs slowly drift through it.

Later, the waves carry some to the shore. This is called the diamond beach. The black sand contrasts with the ice  fragments, resembling precious stones.

Studlagil Canyon The construction of a dam in 2009 reduced the flow  of the Jökulsá á Dal river, revealing this gorge. Its walls are made up of basalt pillars. These appeared due to the slow contraction of  lava as it cooled, creating geometric patterns.

The river runs through the canyon, acquiring  a beautiful turquoise color in summer. The red coloring seen in certain  rocks is caused by iron oxides. Northern Lights Iceland's proximity to the  Arctic Circle enables the observation of this fascinating natural phenomena.

They are most visible away from  the light pollution of urban areas. These occur when electrons and protons  from the solar wind reach Earth. The weaker terrestrial magnetic field at the poles  allows some particles to enter the atmosphere.

Upon colliding with atmospheric gasses, these  charged solar particles cause atoms to emit light. The most common color, a bright green,  is produced by oxygen molecules. Sometimes red hues appear, when solar  particles react with oxygen at high altitudes.

Ice Caves These are natural formations located within  glaciers like Vatnajökull and Langjökull. They develop from water flowing through the  glacier or from geothermal heat melting the ice. Tunnels with beautifully  sculpted ice walls are created.

The ceiling, with its translucent  surface, casts a luminous glow. The denser ice, compressed over the  years, exhibits an intense blue. In warmer months, water begins to flow.

It seeps through cracks and fissures in the  ice, forming streams that run inside the cave. Vestmannaeyjar Also called the Westman Islands, this archipelago lies off the southern Iceland, isolated  in the waters of the North Atlantic. It consists of a main island, Heimaey,  and 15 small uninhabited islands.

Geologically, the youngest islands are also the  smallest, created by underwater volcanic activity. Bjarnarey, the island closest to Heimaey, has  historically been a hunting ground for puffins. The lone house visible is a refuge for hunters.

Ellidaey is slightly more distant and flatter. Its only structure is a hunting  lodge built in the 1950s. Heimaey is the largest and only  inhabited island of the Westman Islands, formed by multiple volcanic eruptions that  occurred between 10 and 12 thousand years ago.

It's a small community with a quiet lifestyle,  particularly dedicated to fishing and tourism. In the eastern sector is located the  volcano Eldfell, which erupted in 1973. The volcanic explosion covered  one-third of Heimaey with lava and ash.

Lava flows added new land, expanding  the territory of the island. Most of its coast is outlined by  steep cliffs of volcanic rock. The ocean has sculpted numerous natural arches.

Elephant Rock stands out, naturally  carved by the force of the waves. Hverir Located at the base of Krafla volcano, this geothermal region is influenced  by an underground magma chamber. It resembles another world, with its  vast plains of red and orange earth, interspersed with mud pots and white smoke.

The soil's colors are due to the  high concentration of minerals. The area is filled with fumaroles, emitting  steam and gasses at high temperatures. The heat from the magma warms the groundwater, which rises as steam through  fractures and pores in the rock.

Mud pots are another visual attraction at Hverir. They form when steam rises  through deposits of clay and soil. Despite its beauty, the area can  be dangerous due to gas emissions, so it is necessary to stick  to the tourist walkways.

Reynisfjara Known for its black sands which are  composed of heavily eroded volcanic rocks. The lava cooled when it touched the ocean  and broke down into small fragments. The landscape is complemented  by huge basalt columns.

The lava from multiple eruptions solidified,  contracting and fracturing into geometric shapes. As winter approaches, Reynisfjara  undergoes drastic changes. The waves of the North Atlantic reach  the shore with a penetrating cold.

The sand, partially covered by snow and  ice, creates a stunning visual contrast. Off the coast rise the Reynisdrangar,  rock pillars that emerge from the sea. According to local legend, they are  trolls that tried to drag ships ashore.

But they were caught by the first  light of dawn and turned to stone. Visitors must be aware that the waves at  this beach are strong and treacherous. They sometimes appear suddenly  and can drag people into the sea.

Skogafoss This waterfall is distinguished by its wide  water drop that plunges into a deep pond. It is bounded by cliffs that  once formed the Icelandic coast. It maintains a powerful flow all year round, with  water coming from the Eyjafjallajökull glacier.

Legend has it that the area's first Viking settler  buried treasure in a cave behind the waterfall. Locals discovered the chest years later, but  only managed to touch it before it vanished. Reykjadalur Hot Springs Dubbed the world's hot spring capital, this is  a geothermal area near the town of Hveragerdi.

Hot springs, mud pots, and steam vents  abound, creating a misty landscape. A warm river runs through the  valley, forming natural pools. Each has a different temperature, allowing  bathers to choose their preferred warmth.

Due to the geothermal activity, the area is characterized by a strong  sulfur smell, typical in volcanic areas. Fjadrargljufur Canyon It's a breathtaking gorge located  in the southern part of the country. A masterpiece of nature with  its meandering rocky formations.

Fjadrárgljúfur is believed to have  been formed during the last Ice Age, over nine thousand years ago. The Fjadrá river runs along the bottom  of the gorge, zigzagging its way. The moss thriving on nearby rocks  gives them a green appearance.

This vegetation is capable of surviving in extreme  conditions, typically growing in volcanic areas. Eyjafjallajokull Considered one of the country's smallest glaciers. The area is highly seismic, with frequent  earthquakes preceding volcanic eruptions.

Hidden beneath the ice cap of Eyjafjallajökull  lies the caldera of a volcano. The eruption that began in 2010,  though small by volcanic standards, caused significant disruption across the region. The interaction between the hot magma and  ice created a massive cloud of volcanic ash, leading to the cancellation of tens  of thousands of flights across Europe.

Thrihnukagigur It is a dormant volcano, one of the few in  the world whose interior can be explored. It hasn't erupted in about four thousand years. Most volcanoes seal their magma chambers  with solidified lava after an eruption.

However, when this volcano last erupted, the lava drained into the ground,  leaving a large empty space. Surtsey Among the Vestman Islands, this geological wonder  stands out as the southernmost point of Iceland. It emerged from an underwater eruption that  began in 1963 and continued until 1967.

It was one of the most significant  geological milestones of the 20th century, giving scientists the chance to  study the creation of a new island. Serving as natural laboratory  without human intervention, it reveals information about  geological and biological processes. It is currently inhabited by  numerous plants and birds, along with hundreds of species of invertebrates.

Laki Fissure It emerged as a volcanic fissure due to the devastating eruptions that  occurred between 1783 and 1784. It released such a massive  volume of lava that it ranks among the largest documented volcanic eruptions. The volcanic gases poisoned the pastures,  killing much of the livestock and causing a famine that wiped out 25%  of the Icelandic population.

The eruption had a significant  impact on the global climate, causing a drop in global temperatures. The toxic fogs that spread across  Europe deteriorated air quality, causing thousands of deaths  from respiratory diseases. According to some historians, the poor  harvests caused by the eruption helped stoke the social discontent that  culminated in the French Revolution.

Eldhraun Beneath a thick blanket of  moss lies a vast lava field. The result of the Laki eruption. Lava spread across the terrain,  covering valleys and fields.

Over time, the molten lava hardened,  creating a rough and rugged surface. Initially, the environment was devoid of life, but gradually it began to be  colonized by mosses and lichens. The moss, in particular, adapted  to the cooled basaltic rocks, establishing and expanding its presence.

Seljalandsfoss These waterfalls cascade over a cliff  that was once part of the coastline. A reflection of how tectonic movements have  altered the Icelandic landscape over time. It belongs to the Seljalandsá river, whose  source is the Eyjafjallajökull glacier.

It features a unique geological structure,  with a cavity behind the waterfall. This makes it one of a few waterfalls in the  world where it's possible to walk behind. Landmannalaugar Its name, meaning "the people's  hot springs," comes from its centuries-old use as a bathing spot.

It's a popular destination  among hiking enthusiasts and those seeking to bathe in natural hot springs. Located in a valley between  mountains and endless lava fields. The mountains display an incredible variety  of colors, including bluish-green hues.

This is due to the minerals present in rhyolite,  a rock formed when silica-rich lava cools rapidly. The black lava field of Laugahraun, resulting  from a 1477 eruption, lies among the mountains. It covers a large area, with the  solidified lava forming complex shapes.

To the north lies Frostastadavatn  lake, formed from volcanic eruptions. Lava flowed across the land, creating  natural barriers that trapped the water. Near this area is Bláhylur,  a volcanic crater lake.

It formed within the crater left  by a powerful volcanic explosion. Kerlingarfjoll It's a mountain range known for its rhyolite  peaks and extensive geothermal areas. The mountains are painted in vivid  hues of oranges, reds, and yellows, due to the high presence of volcanic minerals.

Kerlingarfjöll is part of a volcanic  network with a large central caldera, with the landscape shaped by magmatic activity. Various geothermal phenomena  are observed in the area. Water emerges at the surface as springs,  heated by the proximity of magma.

In the mud pots, boiling and  bubbling mud can be seen. Thorsmork A nature reserve located  between the Tindfjallajökull, Mýrdalsjökull, and Eyjafjallajökull glaciers. It comprises a zone of protected valleys,  flanked by mountains and vast glaciers.

The name Thórsmörk literally translates to "Thor's  forest," in honor of the Norse god of thunder. Unlike much of Iceland, this area has lush  vegetation, rich in mosses and wildflowers. Various rivers flow through the valleys,  originating from the nearby glaciers.

Their flow varies with the  seasons and weather conditions. During periods of thaw, they swell  rapidly, and crossing becomes a challenge. In 2010, Thorsmork was affected by the  eruption of nearby Eyjafjallajökull, but the area has since recovered.

Blue Lagoon It's a geothermal spa located in a lava field. Its waters are a milky blue,  surrounded by black volcanic rock. They contain high levels of silica and  sulfur, which give it this appearance.

The water temperature remains  warm throughout the year. In the colder months, the steam  intensifies the ethereal atmosphere. Despite its natural appearance,  this lagoon was created in 1976 as a byproduct of the Svartsengi geothermal plant.

Dettifoss It is characterized by its impressive  width and the large volume of water that descends in a powerful and noisy fall. It is one of the most powerful waterfalls in  Europe measured by the sheer volume of water. The amount of energy released is so  great that one can feel the ground tremble underfoot when approaching the edge.

The water of the Jökulsá á Fjöllum  river, which feeds the waterfall, carries glacial sediments that  give the water a brown color. Dettifoss was featured in the  science fiction movie "Prometheus," directed by Ridley Scott, which  increased its number of visitors. Borgarfjardarhofn This small remote village in  the northeast of the country, Borgarfjördur Eystri, is one of the best  places in the world for bird watching.

Here lies Borgarfjardarhöfn, a  reserve for Atlantic puffins. Facilities were built to  minimize human disturbance in the natural habitat of this curious species. Puffins are seabirds that only  come to land to reproduce and nest.

They arrive at the coast in April and  by the end of August return to the sea, where they stay the rest of the year. They nest in colonies on cliffs or islands,  digging tunnels to lay a single egg. They are usually monogamous, returning  with the same partner each breeding season.

Excellent in flight, they flap their  wings hundreds of times per minute. They are also notable swimmers, using  their wings to chase fish underwater. Skutustadagigar In the Mývatn lake area in northern Iceland,  this series of pseudocraters stands.

It's a very rare geological phenomenon worldwide. After an eruption, the hot lava came into contact  with water, quickly turning it into steam. The rapid transformation from  liquid to gas caused explosions, leaving holes in the ground and  accumulations of volcanic material.

Kerid Crater At the bottom of this volcanic crater, there is a lake, whose walls are  stained with rusty red and brown. At only six thousand five hundred years old, it is young compared to other  geological formations in the area. It is thought to have been a conical volcano  whose eruption caused the collapse of its cone.

Unlike other craters filled with rainwater, it is  believed that Kerid's lake is fed by groundwater. Gullfoss In summer, the abundant flow of this  waterfall creates a marvelous scene. It is said that Gýgur, who owned a  large amount of gold, threw a chest into its depths, which earned it  the name of the golden waterfall.

Located in the Hvítá river canyon,  it features two main waterfalls. Over millennia, the flow of the water shaped  the rock, creating the crevice seen today. Snaefellsjokull National Park It's one of the country's  most iconic national parks.

Named after the Snaefellsjökull volcano, which  features a glacier visible from Reykjavík. Jules Verne's novel "Journey to the Center of the Earth" was based on this stratovolcano  as the gateway to the underground world. The park showcases a diversity  of geological formations, such as lava tubes and volcanic craters.

Nearby is Arnarstapi, a small  village with striking rocky outcrops. These hexagonal basalt columns arose  from the cooling of a thick lava flow. Also notable is Gatklettur, a natural arch sculpted by the force  of the waves against the volcanic rock.

Kirkjufell Located on the Snaefellsnes Peninsula,  this mountain has an unusual conical shape. It rises alone from sea level,  independent of other mountains. Volcanic eruptions followed by glacial  erosion gave rise to its peculiar appearance.

In summer, Kirkjufell turns intensely  green, covered with grass and moss. Kirkjufellsfoss, the nearby waterfall,  seems to spring directly from the mountain. It is fed by the Kirkjufellsá river, which originates in the nearby  mountains and flows to the sea.

Grimsey Island To the north of Iceland's north coast, within  the Arctic Circle, lies this small island. Due to this position, for much of the  summer there are 24 hours of light, while in winter almost the  entire day remains in darkness. Unlike mainland Iceland, full of mountains  and volcanoes, Grímsey's terrain is flat.

Only a few dozen people live on the island,  though there are thousands of birds. Amid this isolation stands  a notable mobile monument: a large stone sphere that marks  the position of the Arctic Circle. Thridrangaviti Lighthouse A solitary guardian in the vast blue of  the North Atlantic, south of Iceland.

This sanctuary of peace is accessible by sea,  though helicopter is another viable option. The construction of the lighthouse  in 1939 was a remarkable feat, considering the complex geography of the location. Godafoss In winter, these falls transform into a frozen  paradise, with elaborate ice formations.

It is one of Iceland's most spectacular  and historically significant waterfalls, known as the waterfall of the gods. It is part of the Skjálfandafljót river,  flowing from the central highlands, an uninhabitable area formed by  basalt mountains and lava fields. Legend has it that in the year 1000,  when Iceland converted to Christianity, statues of Norse gods were  thrown into the waterfall.

Krafla It's a volcanic caldera located near Lake Mývatn. Defined by fissures that cut through a  central volcano, forming a volcanic system. In the crater of one of the  eruptions, the Víti lake emerged, whose turquoise waters stand out  against the rocky and red surroundings.

The Krafla geothermal power station  utilizes the energy from the subsurface, one of the first of its kind in the world. It employs turbines driven by the steam  of hot water obtained from the ground. Hengifoss The area surrounding these waterfalls has  experienced volcanic eruptions for millennia.

The striking red lines visible on the cliff wall  are layers of clay originating from volcanic ash. During eruptions, the ash was deposited  on the ground, compacting into clay. When the iron minerals in the clay were exposed  to oxygen, they oxidized, giving it a red hue.

Over thousands of years, lava from  new eruptions covered the layers of reddish clay, explaining the dark layers. This alternation between dark and red layers  illustrates the various geological ages. Sigoldugljufur This is a spectacular canyon  nicknamed the "Valley of Tears”.

Defined by steep walls and a series of  waterfalls cascading into the deep valley below. The force of water and earthquakes  gradually wear down the rocky walls. The river flowing through the canyon, coming from nearby reservoirs and meltwater,  feeds the numerous waterfalls.

Hafragilsfoss A powerful natural wonder within  Vatnajökull National Park. It is one of the waterfalls of  the Jökulsá á Fjöllum river, downstream from the famous Dettifoss. It falls into the Jökulsárgljúfur canyon,  formed by volcanic activity and glacial floods.

The torrential river has carved the  bedrock for more than two thousand years. After Hafragilsfoss, the water continues  its course and reaches a glacial spring, resulting in what is known as a water encounter. The clear turquoise water is typical  of waters coming from glaciers.

When it merges with the river,  which carries murkier water, abstract patterns are  created at the meeting point. Katla Volcano Considered one of the most active  and powerful volcanoes in Europe. Its crater remains hidden, covered  by the Mýrdalsjökull glacier.

Katla is named after a malevolent  witch in Norse mythology, who, when pursued by her enemies,  threw herself into the volcano. Over the past 20 years, it has  experienced numerous major eruptions. They are particularly explosive and dangerous.

Given its activity, Icelandic volcanologists  constantly monitor it using seismographs. Within the Katla volcanic system lies Eldgjá,  the largest volcanic canyon in the world. The eruption that occurred here in 939 was  one of the largest lava floods of all time.

Gljufrabui Hidden behind a cliff, this  waterfall is more difficult to reach. Its name, meaning "Dweller of the gorge," refers  to its hidden location in a narrow canyon. Because it is behind a large cliff, its visibility from a distance is  less than that of other waterfalls.

Visitors can access the base, an  enclosed space with moss-covered walls. Hraunfossar The meltwater from the Langjökull glacier seeps  through porous volcanic rock to reach this spot. Known as "lava waterfalls," it is a series  of cascades that spring from a small cliff.

After the colonization of Iceland, a volcanic eruption created the lava  field through which the water flows. Legend has it that a sorcerer diverted  the Hvitá river, creating the waterfalls. Mulagljufur Canyon Also known as Múlafoss, this deep and narrow  gorge features vertical walls of volcanic rock.

Access is challenging, especially  during the winter months. A river runs along the canyon floor, fed by  meltwater from nearby glaciers and rainfall. The topography, with its steep slopes and  rocky cliffs, gives rise to tall waterfalls.

Foss a Sidu A hidden gem, this waterfall is near  the village of Kirkjubaejarklaustur. It falls dramatically from a cliff  partially covered in vegetation. It incorporates a historic farm that has been operational continuously  since the Viking settlement era.

Indeed, this area is mentioned  in one of the earliest works of Icelandic literature, the Book of Settlements. Maelifell It's a volcano in the Highlands, starkly  visible against a desert of black sand. Accessible only by 4x4  vehicles and only in summer, it is in one of Iceland's most remote regions.

It has an almost perfect conical shape,  composed of layers of hardened lava. It was once covered by the Mýrdalsjökull glacier, emerging about 10,000 years ago  at the end of the last Ice Age. Glacial rivers surround it,  forming branches as they flow.

Dyrholaey Lighthouse Located at the highest point in the area, it offers a stunning panoramic  view of the Atlantic Ocean. It was built in 1927 to assist ships  approaching the southern coast. These cliffs are primarily  composed of black basalt, the most common magmatic rock in the country.

It consists of an area rich in geological  formations, like the Dyrhólaey arch. Formed over millennia from volcanic  eruptions, it has been sculpted by the waves. The area around the lighthouse  is ideal for bird watching, especially for puffins that nest on the cliffs.

Westfjords It's a large peninsula filled with  mountains, cliffs, and fjords. With few inhabitants, this area is  one of the most remote in Iceland. It features multiple deep  bays that cut into the land.

And some mountains formed millions of years ago. The Látrabjarg cliffs are  among the tallest in Europe. It's a breeding ground for Atlantic puffins.

Many of the roads in the Westfjords are  narrow and traverse the steep mountain slopes. One of them leads to Raudisandur  beach, which translates to "red sand. " But it is not a single shade of red.

It  varies between red, pink, gold, and white. The presence of mollusk shells and other marine organisms in its composition is  the reason for its appearance. Another natural phenomenon of this  peninsula is the Dynjandi waterfall.

It resembles a bridal veil, cascading in steps. The upper level is the widest,  spreading across the mountain. Ljotipollur Despite its beautiful appearance, its name  in Icelandic translates to "ugly puddle.

" It is a crater lake formed in  1477 by an explosive eruption. The blue of the lake's water  enhances the color of the red walls. Additionally, green lines of mosses and  lichens have grown on the volcanic terrain.

Vestrahorn and Stokksnes Beach Vestrahorn is a majestic mountain,  considered one of the most iconic in Iceland. It features sharp peaks and jagged  ridges that extend towards the sky. It is made of gabbro and granite,  which gives it a dark color.

Stokksnes, which borders  Vestrahorn, is equally stunning. It consists of a black sand  beach with unusual green mounds. These are plants adapted to sandy  environments that grow in the dunes.

Eystrahorn It is a long mountain near Vestrahorn. Not easily accessible, it offers  a more solitary experience. It rises directly from the  sea, surrounded by waters.

Its slopes are often covered  with snow in the colder months. Like many other parts of the country, Eystrahorn experiences rapid weather changes  that alter the landscape within minutes. Nauthusagil A waterfall located in a remote  and difficult-to-access place.

It falls at the end of a canyon, and  reaching it requires being well-equipped. To get there, one must pass  through narrow passages. At the end, a hidden small pool that  receives water from the stream is revealed.

Hverfjall Almost perfectly circular, it is one  of the largest tuff rings in the world. It is part of the highly geothermal and lava  field-surrounded Krafla volcanic system. It was created from an explosive eruption  about two thousand five hundred years ago, which is quite recent in geological terms.

Due to the acidity of the soil and its  volcanic origin, it is devoid of vegetation. Husavik A coastal town in the north, set against  a backdrop of mountains and blue waters. According to the Icelandic sagas, it was one  of the first Viking settlements on the island.

It is known as the "whale watching capital" due to the diversity of cetacean  species sighted in Skjálfandi Bay. It is possible to see humpback whales, fin  whales, and minke whales, among other species. During the 19th and early 20th centuries, whale hunting was crucial to Húsavík's  economy and much of the nation.

However, the town evolved into a  center for cetacean observation. Asbyrgi A massive flood during the last glacial  period created this horseshoe-shaped canyon. It is a small geological wonder  of Vatnajökull National Park.

According to local folklore, Sleipnir, the horse of the Norse god Odin, left  the imprint of one of his hooves. This environment hosts a lush forest of birch and  willow trees, unusual in the Icelandic landscape. Bjarnafoss It stands out for its height and the powerful  waterfall cascading from a rock cliff.

Local legends claim that mythical  beings live in nearby caves. As it falls, the water  passes over basalt formations that line up in hexagonal columns along the cliff. Solheimasandur Plane Wreck These are the remains of a Douglas  DC3 from the United States Navy.

It ran out of fuel while flying  over the area on November 21, 1973, and crashed on the Sólheimasandur beach. After the accident, the cost of recovering it  was deemed too high, and it was left abandoned. What remains is the fuselage, parts of the wings, and the tail section, all resting on  a desolate surface of volcanic sand.

Reykjavik It is the capital closest to the North Pole. It was the site of the island's  first permanent settlement, established by the Viking  explorer Ingólfr Arnarson in 874. It is reputed to be one of the cleanest,  greenest, and safest cities on the planet.

Underlying volcanic activity allows  for the generation of electricity. Due to its location, it  experiences illuminated nights from May to August and few hours  of light from December to February. Buildings like the Hallgrímskirkja church stand  out, whose design is inspired by lava columns.

Started in 1945, its completion  took more than 40 years. Isafjordur It serves as the administrative  center of the Westfjords. Its natural setting is splendid,  with towering mountains, and the fjord opening out to the Greenland Sea.

It was once one of the country's largest fishing ports, with a trading history  dating back to the 16th century. Some of the town's oldest  buildings are made of wood, painted in bright colors, in  a style unique to this region. Seydisfjordur This settlement was colonized  in 1848 by Norwegian fishermen.

In 1906, the first telegraphic cable linking  Iceland to Europe was installed here. It remains a fishing village, but the  economy has been developing towards tourism. Although located in the northeast, it  has a tundra climate with high humidity.

Lupine Fields They have become a true  natural spectacle in summer. Introduced in the 20th century, they have since  thrived, covering vast areas of the country. They were introduced to combat  deforestation and improve soil fertility.

By densely covering the ground, they support the growth of native plants  and the survival of local animals. When in bloom, they transform  into a colorful carpet that sometimes surrounds other natural wonders. Eldborg It is an oval-shaped volcanic crater,  with steep sides and a defined rim.

In Icelandic, "Eldborg" means  "fire fortress," alluding to its fortification-like shape and volcanic origin. It developed from a fissure eruption, with lava erupting from a crack in the  ground about 5,000 to 8,000 years ago. The ease of access and views  from the top make the hike to the crater very popular with tourists and locals.

Akureyri Sometimes called the capital of the north, it  is located very close to the Arctic Circle. Helgi magri Eyvindarson, a Norwegian  Viking, was the first to settle in the area. The city is situated at the  base of the Eyjafjördur fjord, surrounded by snow-capped  mountains well into spring.

The architecture blends traditional and modern styles, with colorful wooden houses  alongside contemporary buildings. Despite its location, Akureyri enjoys a relatively  mild climate thanks to warm ocean currents. Hornstrandir It is the most remote area of the Westfjords.

Only accessible by boat or on foot  from the south, it is uninhabited. Its ecosystems remain largely intact, as it is  one of the country's most protected natural areas. This isolation makes it one of  the best places in the world to observe the Arctic fox in its natural habitat.

In summer, their fur darkens, helping  them to camouflage in the tundra. Siglufjordur It is a small fishing village nestled  in a fjord on the Tröllaskagi peninsula. Surrounded by steep mountains  and the North Atlantic Ocean, with traditional houses and a small harbor.

Once known as the "Atlantic herring capital. " Before the construction of tunnels, it was one  of the most isolated settlements in the country, accessible only by sea or mountainous paths. Grjotagja Cave Hidden in this small cave is  an underground thermal spring.

The water is an intense blue, and light filters  in softly, creating a mystical atmosphere. Until the 1970s, locals  frequently came here to bathe. However, seismic activity raised the water  temperature, making it too hot for safe bathing.

Myvatn Nature Baths These are large pools of milky blue thermal  waters, surrounded by volcanic landscapes. The water is naturally heated by  an underground geothermal source. It is believed that their high concentration of  silica and minerals is beneficial for the skin.

While other natural baths are more touristic,  these are also frequented by Icelanders. Grabrok Crater Considered an extinct volcano, it is part of  a volcanic system that contains three craters. It was created by a volcanic eruption  about three thousand years ago.

It has the typical conical  shape of a volcanic crater, with walls composed of rocks  from ancient eruptions. Bruararfoss It consists of a series of small  waterfalls that flow over a lava field. The glacial river Bruara makes  its way through a deep crevice cutting through the center of  dark volcanic rock formations.

This results in rapids of celestial blue, a product of the mix of meltwater  and mineral-rich spring water. Vik It is the southernmost village in Iceland,  positioned on the coast of the Atlantic Ocean. A small, tranquil community with  traditional Icelandic architecture.

It is under constant threat due to  its proximity to the volcano Katla. The Atlantic Ocean stretches out in  front with its black sand beaches, while tall mountains rise behind. Svartifoss Its name, meaning "black falls," is due to  the dark basalt columns that surround it.

The base is covered with sharp rocks that  have broken off during seismic activity. Its appearance has influenced  Icelandic architecture, as seen in Reykjavík's Hallgrímskirkja church. Fjallsarlon At the foot of the Fjallsjökull glacier lies  this lagoon, part of the vast Vatnajökull.

It is less known than its neighbor Jökulsárlón,  but equally spectacular, with large ice masses. Along the lagoon, icebergs  break off from the glacier. The water is a deep blue, and the icebergs,  compressed over centuries, display various colors.

Kolgrafafjordur A fjord located on the Snaefellsnes peninsula. It was a fishing and trading post  for the surrounding communities. It extends inland from the coast, with steep  cliffs and mountains rising from the shore.

The waters are generally calm,  reflecting the sky and surroundings. Solheimajokull It is a glacier situated between the  volcanoes Katla and Eyjafjallajökull, part of the larger Mýrdalsjökull glacier. Notable for its enormous crevasses,  some of which are suitable for climbing.

Appropriate equipment, such as  crampons, harnesses, and ropes, along with technical skills  for moving on ice, is required. Participants often rely on guides who  are well acquainted with the geography and know how to conduct the activity safely. Although some glaciers are accessible year-round, the best conditions for climbing  are usually in the summer.

Hrunalaug This small natural thermal pool is  located near the village of Flúdir. It is believed that locals have  used it for bathing for centuries. The underlying geothermal  activity heats the waters, providing an authentic hot spring experience.

Aldeyjarfoss Fed by the Vatnajökull glacier, this waterfall  plunges down the Skjálfandafljót river. Framed by black basalt columns, it  shines with its white and foamy water. The contraction and gradual solidification of  the lava have created geometric structures.

To reach it, a 4x4 vehicle is necessary,  as it is located in a remote area. Hvitserkur It is a unique rock formation in Húnaflói Bay. A monolith of tuff surrounded by the North Sea.

Its appearance is reminiscent of a rhinoceros,  an elephant, or a dragon drinking water. Legend has it that it is a troll petrified by  the first rays of dawn as it attempted to destroy a nearby monastery. Secret Lagoon This geothermal pool is naturally heated.

It is the oldest pool in  the country, opened in 1891. Its rustic appearance has been preserved  over time to maintain its historical value. Eskifjordur A small town in the Eastern Fjords.

Nestled in the fjord of the same name,  surrounded by rugged terrain and serene waters. Historically, it has been a vital port  and fishing center for this region. It is characterized by its colorful houses against the backdrop of the mountains  and the North Atlantic Ocean.

Haifoss One of the tallest waterfalls in Iceland, accompanied by its neighbor  Granni, which means "neighbor. " They are somewhat isolated, in the valley of  Fjórsárdalur, requiring a short hike to reach. Haifoss is surrounded by steep cliffs, and  its water falls directly onto the rocky base.

Raudaskal Surrounded by a black desert, this  volcanic crater has a wavy shape. It formed through a violent eruption  that brought magma to the surface. The name "Raudaskál" indicates a reddish  hue, caused by the iron oxides in the rocks.

Studlafoss A lesser-known but incredibly beautiful waterfall. Recognized for the basalt  columns that surround it. They form a structure similar to an  amphitheater of hexagonal columns.

Viking Village Originally conceived as a film set, it was  later transformed into a tourist attraction. Located at the foot of Mount  Vestrahorn, flanked by grasslands. It is a recreation of an authentic Viking  village, with traditional Nordic architecture.

Viking villages were typically  situated along rivers or coastlines. Those prone to attacks placed protective  structures like fences, walls, or ditches. Arctic Henge A modern monument near the  remote town of Raufarhöfn.

Its huge stone structures are  arranged in a circular pattern. Inspired by Norse mythology, particularly the poem "Völuspá," which speaks of a  cycle of creation and destruction. It acts as a gigantic sundial, with openings that capture sunlight  and project shadows at specific points.

Selfoss The largest residential area in southern  Iceland, a service center for the region. Serves as a gateway to some of Iceland's  natural attractions, such as the Golden Circle. The Ölfusá river, the largest in the  country by volume, flows through the town.

Rebuilt after the 2008 earthquake, it combines modern earthquake-resistant  structures with traditional buildings. Hafnarfjordur Located south of Reykjavik, it is one of  the most populated cities in the nation. The first settlers were Vikings  who arrived in the 9th century, and in the 15th century,  trade began with the English.

It is built on the lava from the Búrfell volcano, which erupted over seven  thousand three hundred years ago. According to folk tales, elves and trolls  live in the lava fields surrounding the city. Stykkisholmur This town, located at the northern  tip of the Snæfellsnes peninsula, features well-preserved ancient wooden houses.

It gained worldwide recognition when selected as a location for the film "The  Secret Life of Walter Mitty. " It serves as a starting point for ferry services to the Westfjords and tours  around Breidafjördur Bay. The church, Stykkishólmskirkja, stands  out for its modern architecture, distinct from traditional Icelandic designs.

Grundarfjordur Also on the Snaefellsnes peninsula, this small village is set against  a stunning natural backdrop. Traditionally, the area has been a fishing  community, thanks to its access to the sea and plentiful fishing grounds. Around 1800, French traders settled  in the area, constructing a church.

Among all the natural wonders nearby, Kirkjufell,  visible from the village, stands out the most. Krisuvikurberg Cliffs They rise on the Reykjanes peninsula,  forming a natural wall along the coast. Lava flows from past eruptions solidified,  creating the rocky layers of the current cliffs.

The force of the wind and waves  shapes the basalt into vertical walls. The reddish hue in some sections is  due to the oxidation of iron minerals. Strandarkirkja Sailors from the 12th century who  survived a storm built this church.

They believed an angel had guided them  safely to shore, erecting it in gratitude. Its reputation for harboring miraculous powers makes it one of the most visited  pilgrimage sites in the country. Other Places Despite its small size, Iceland hides  dozens of treasures worth exploring.

The Langanes Peninsula, with its flat  surface, is defined by its steep cliffs. Mígandifoss, a waterfall in the east of  the country, flows directly into the ocean. Built in 1884, Hofskirkja is one of the  last turf churches remaining on the island.

These tiny houses, known as alfhol, are  built to signal the presence of elves. The Glaumbaer farm, with its traditional turf  houses designed to withstand the harsh climate. Laufás, a 19th-century farm, has  been inhabited by clergy since the early years of Christianity in Iceland.

Krafla's shower, which continuously supplies  hot water from an underground source. The Gjáin canyon, with  waterfalls and lush vegetation. Here, mosses, ferns, and other plants thrive,  forming a green oasis amid the rocky surroundings.

Arnardrangur, an unusual rock  structure on Reynisfjara beach. Its name means eagle rock, although no  eagles have nested there since 1850. The DC-3, a US Navy aircraft that crashed in 1969 north of Iceland, later moved  to Eyvindarholt in the south.

The Vattarnes lighthouse, on the eastern  coast, is located on a remote peninsula. Brimketill, a natural pool of volcanic  rock located on the Reykjanes Peninsula. Grafarkirkja, the country's oldest  church, dating from the 17th century.

Borgarnes, a town situated on a small  peninsula in Borgarfjordur fjord. Stjórnarfoss, a tranquil  waterfall, in a less-traveled area. It flows over basalt rocks in two main levels.

Gerduberg, a cliff with a row of basalt columns. They are unusually uniform in size and  shape, creating a long natural barrier. Sigöldufoss, a waterfall in the Highlands.

The weather here can be unpredictable, with  sudden temperature changes and strong winds. Búdakirkja, a nearly 2-century-old  church known for its black facade. A common sight while touring Iceland is sheep.

They arrived on the island with the  first Viking settlers and over more than a thousand years have adapted  to the climate and environment. They survive by feeding on pastures in  summer and hay during the long winters. During the summer, their owners  allow them to graze freely.

They are often seen near  Iceland's natural wonders. They are known for having little herd  instinct, dispersing and reaching remote areas. In September, farmers gather  for the "réttir," an event in which they collect the sheep and bring  them back to the farms for the winter.

Another animal commonly seen while touring  the country is the Icelandic horse. It is believed that settlers brought  breeds of Nordic and Celtic origin. Due to geographic isolation and laws  prohibiting the importation of horses, the Icelandic breed has remained  pure for over a thousand years.

They are smaller than most horse breeds but  possess incredible strength and endurance. Their efficiency in finding food makes  them ideal for enduring this harsh climate. Reindeer, imported from Norway in  1771 to diversify food sources, are less likely to be seen.

They inhabit the eastern part of the country,  especially in the highlands and mountainous areas. We have reached the end of  our journey through Iceland, an island filled with breathtaking  landscapes and untamed nature. Thank you for joining us on this  journey.

See you on our next adventure.