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5 Natural Marvels of Iceland

Gullfoss

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5 Natural Marvels of Iceland
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Public Domain Image

We certainly hope that you enjoy this article on 5 Natural Marvels of Iceland. While natural beauty appears in all sections of our world, this region just seems to have more than its share. It also comes in many varied forms, to be certain, but all display extraordinary beauty. Please, read on now, and partake of the wonder and majesty that this corner of the globe has been blessed with.

Reynisfjara Beach

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Reynisfjara Beach Facts

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Reynisfjara Beach Location and Geological Description

Reynisfjara Beach sits roughly 112 mi (180 km) from Reykjavik, in Iceland, in Europe, and faces the cold, open waters of the northern Atlantic Ocean. This incredible site stretches for about 3.1 mi (5 km).

Most noteworthy is the fact that the beach actually has an astonishing black color. That occurs due to is composition of basalt, gradually eroded with the relentless passage of time.

In addition, the location continues to be famous for the presence of incredible stone features just offshore. These constitute black basalt columns known as Reynisdrangar, which began as enormous volcanic boulders.

Since their expulsion from the earth ages ago, erosion occurred from the action of wind and waves. This subsequently created the incredible shapes found there today.

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Reynisfjara Beach Climate and Ecology

The climatic conditions at Reynisfjara Beach remain extreme, usually enough to dissuade investigation by all but the most ardent beach fans.

It also rains there an average of 340 days per year, making it the wettest place in Iceland. And it already rains in Iceland a lot.

One magazine named the location one of the 10 most outstanding non-tropical beaches on earth, in 1991. This was despite (or perhaps as a result of) these conditions.

Surprisingly, rather than being devoid of wildlife, the location teems with a variety of birds. These include fulmars, guillemots, and puffins, showcasing the extraordinary adaptability of Nature.

Haukadalur Geothermal Area

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Haukadalur Geothermal Area Facts

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Haukadalur Geothermal Area Origins and Nature

The Haukadalur Geothermal Area originally formed at the end of the last Ice Age. Yet, occasional earthquakes in the region continue to alter its nature even today. The last such earthquake in the region occurred in July of 2000.

There are currently 40 geothermal based features present in the remarkable region. All of these are volcanic in nature. They include multiple geysers, hot springs, fumaroles, and mud pots.

The largest of the geysers is Strokkur and many of the geysers are comparatively regular in the timing of their eruptions.

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Haukadalur Geothermal Area Physical and Biological Distinctiveness

Several of the small springs in the area are quite unique. The water within them is sodium bicarbonate thermal water due to the extremely high concentrations of sodium bicarbonate.

These same streams in the Haukadalur Geothermal Area also contain comparatively high concentrations of radon.

Living within this unique environment are numerous species of microorganism and algae that have adapted to survive within the unique water and extreme heat.

In fact, many of them are incapable of surviving in water temperatures below 158 F (70 C).

Gullfoss

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Gullfoss Facts

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Gullfoss Physical Description

Most notably, Gullfoss is situated in a unique and isolated location. The southward-flowing river takes a decidedly sharp right turn about o.62 mi (1 km) before reaching the waterfall. Then it rapidly flows into a uniquely curved, three-step staircase.

Subsequent to that, it further plummets in two distinct stages. A drop of about 36 ft (11 m) constitutes the first of these. Furthermore, a second drop measuring roughly 69 ft (21 m) represents the second of them.

Finally, these two drops take place within a crevice 105 ft (32 m) deep, and only 60 ft (20 m) wide. The crevice itself also measures about 1.6 mi (2.5 km) in length and flows perpendicular to the river itself.

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Gullfoss Cultural Significance

Additionally, Gullfoss holds a special place in the culture of the region. Throughout much of the first half of the 20th century, there was great interest in utilizing it as a source of hydroelectric power.

Foreign investors purchased the rights to the waterfall for just that reason. However, the daughter of the man who owned those rights before protested vehemently for the preservation of the pristine beauty of Gullfoss. After years of court battles, the young woman lost her case.

However, the foreign owners had exhausted their funds, partly due to the expense of the trials. As a result, the rights were sold to the government, which promptly established a conservation area to protect it.

Thorsmork

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Thorsmork Facts

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Thorsmork Climate and Conditions

The unique environmental conditions present in Thorsmork led to the formation of a climate much more temperate than most of southern Iceland. This has led to the development of a rather unique and delicate ecosystem in the region.

Within the shelter and protection of the valley, a variety of vegetation grows in great abundance. The most prevalent types of plants include Birchwood, ferns, and moss, along with a wide variety of small shrubs.

Fed by the melting glaciers, numerous waterfalls, large and small, also developed within Thorsmork. Much of the region was later inundated by a layer of volcanic ash from the aforementioned eruption in the spring of 2010.

This occurred when the nearby volcano Eyjafjallajokull erupted, to the great surprise of many experts. It required several months before the rather delicate local climate returned to normal.

Strokkur Geyser

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Strokkur Geyser Facts

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Strokkur Geyser Physical Description

Eruptions of Strokkur Geyser attain an average height of between 49.2-65.6 ft (15-20 m). Yet exceptional occurrences occasionally attain a height of as much as 131 ft (40 m).

It also comprises part of the Haukadalur valley area. There, numerous other geothermal features also exist. These include fumaroles, mud pools, and other geysers that continue to be located around it.

Shortly before eruptions, the pool of hot water fills and then pulses up and down rhythmically. Following this, a large bubble forms, and then the eruption spews forth.

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Strokkur Geyser Location and History

Most notably, geological evidence indicates that Strokkur Geyser formed roughly 1,000 years ago, subsequent to an earthquake in the geologically active region.

The earliest recorded reports of its activity date back to the year 1294. At an uncertain time after this, another quake deactivated the site.

In 1789, yet another quake reactivated it. It also subsequently remained active until 1896 when still another earthquake deactivated it once again.

In 1963 local residents succeeded in unblocking Strokkur Geyser once again, and it has remained active since that time.

This constitutes the only recorded instance of human actions intentionally creating or reactivating a geyser.

Finally, this wonder of Nature, like the others on this list, formed in what now constitutes the country of Iceland. This area is beside the Hvita River, in the southwest portion of the country.

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We certainly hope that you have enjoyed this article on 5 Natural Marvels of Iceland. Sites such as these, serve as proof that great natural beauty exists in even the most remote parts of the world. Nature created the beauty that surrounds us, but it remains up to us to make every effort to preserve it for future generations to enjoy.

Check out our other articles on Breathtaking Asian Species, Incredible Sharks of the World, North American Gulches and Canyons, Earth’s Extremely Threatened Flowers

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