Strokkur Geyser Facts
- Strokkur Geyser represents a powerful fountain geyser found in a geothermal area in a remote and sparsely populated portion of Europe.
- The beautiful and extremely regular geyser remains one of the most famous of its kind within the region in which it formed.
- This marvel of geology erupts in a frequency range of between 4-8 minutes.
- This lovely geyser also remains one of the few known geysers to erupt with a regular frequency.
- This has made it a leading tourist attraction in the region.
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 comprises part of the Haukadalur valley area, where numerous other geothermal feature such as fumaroles, mud pools, and other geysers 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.
Strokkur Geyser Location and History
Geological evidence indicates that Strokkur Geyser first formed approximately 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 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.
This wonder of Nature formed in what now constitutes the country of Iceland. This area is beside the Hvita River, in the southwest portion of the country.