Fischbach‘s Reisen
Fischbach‘s Reisen
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ISLAND Island of Vikings, Geysers, and Glaciers

Published: 04.05.2026

Worth seeing
Reykjavik
Reykjavik, Island
Attraction
Thingvellir Nationalpark
Island
Museum
Glaumbaer
Island
Attraction
Geysir
Zentralisland, Island
Attraction
Vatnajökull
Island, Island
Worth seeing
Vätnajökulsbjódgardur
Island, Island
Worth seeing
südlich vom Vätnajökull Gletscher
Island, Island
Attraction
Dyrhólaós
Island, Island

Our round trip starts in Reykjavik on Ring Road No. 1, which is always snow-free and encircles all of Iceland.

Keflavik Airport is located about 50km west of Reykjavik, was a NATO military base until 2006, but not a rocket station. Currently, Iceland, like Costa Rica, has no military.

Regarding history: From 870 AD, Vikings, mostly Norwegians, conquered the land and settled it in the 9th century.

In 930 AD, the first Icelandic parliament was established in what is now Thingvellir National Park. Here, judicial proceedings were held every June. Old laws were repealed, new ones enacted, feuds were settled, and they did not shy away from imposing wergild. This means, for instance, 20 horses for a lost man or 4 horses for a woman.

Thingvellir, Source of Viking Law
Thingvellir, Source of Viking Law

The well-preserved Glaumbaer farm museum is a testament to the construction of turf houses. Grass turfs were used, which are arranged in a herringbone pattern, providing good thermal insulation. The houses are connected by corridors.

Glaumbaer, turf houses with herringbone arranged grass turfs
Glaumbaer, turf houses with herringbone arranged grass turfs

In the 13th century, the Kalmar Union was formed. The Norwegians, Swedes, and Danes united. Iceland came under Danish rule. It wasn't until 1944 that Iceland became independent and made a name for itself through the spectacular Cod Wars, which concerned the expansion of the fishing zone to ultimately 200 nautical miles. It's worth mentioning that fish is the main source of income, though it is currently overshadowed by tourism.

Iceland is a volcanic island located on the Mid-Atlantic Ridge. The Eurasian and North American plates are drifting apart, creating fissure volcanoes that fill with lava.

Iceland's geyser is the namesake for hot springs. The divergence of tectonic plates allows magma to rise and boil the groundwater.

Geysir in a state of awakening
Geysir in a state of awakening

Central Iceland is a desert. The porous lava rock cannot develop humus-rich soil, and the water drains away immediately; the low air temperatures also make it difficult for plant life.

Central desert of Iceland made up of pebbles
Central desert of Iceland made up of pebbles

The eruption of Laki, in southeastern Iceland, caused devastating sulfur dioxide-rich ash clouds from 1783 to 1784, leading to worldwide crop failures, famines, mass deaths, and a decrease in air temperatures of up to four degrees.

Vatnajökull is the largest glacier in Europe, covering almost 8,000 square kilometers. The glacial ice is partly blue, resulting from the compression of snow.

Vätnajökulsbjódgardur
Vätnajökulsbjódgardur

The lava inclusions testify to subglacial eruptions. The decrease in glacier thickness leads to the release of pressure on the magma, potentially increasing volcanic activity beneath the glacier.

The amphibious vehicles from US Army stocks serve tourism both on land and sea.

Amphibious vehicle south of the Vatnajökull glacier
Amphibious vehicle south of the Vatnajökull glacier

At the poles, there is less diversity in plant and animal life than in the tropics. Geraniums, buttercups, rowan trees, as well as the introduced lupine are commonly found.

In the bird world, you can see the eider duck, mallard, common gulls, puffins on the bird cliff at Dyrhólaós, snipes, and oystercatchers.

Common gull and puffin
Common gull and puffin


At a glance

Automatically extracted from the post
Weather
Summer
CulturalAdventurous
  • Reykjavik
  • Thingvellir Nationalpark
  • Glaumbaer
  • Geysir
  • Vatnajökull
  • Dyrhólaós
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