Whois & Analysis for bluelagoon.com

Iceland is a Nordic island country in the North Atlantic Ocean.

It has a population of and an area of, making it the most sparsely populated country in Europe.

The capital and largest city is Reykjavík.

Reykjavík and the surrounding areas in the southwest of the country are home to over two-thirds of the population.

Iceland is volcanically and geologically active.

The interior consists of a plateau characterised by sand and lava fields, mountains and glaciers, while many glacial rivers flow to the sea through the lowlands.

Iceland is warmed by the Gulf Stream and has a temperate climate, despite a high latitude just outside the Arctic Circle.

Its high latitude and marine influence still keeps summers chilly, with most of the archipelago having a tundra climate.

The Blue Lagoon (Icelandic: ) geothermal spa is one of the most visited attractions in Iceland.

The spa is located in a lava field in Grindavík on the Reykjanes Peninsula, southwestern Iceland.

Bláa lónið is situated approximately from the Keflavík International Airport and from the capital city of Reykjavík, roughly a 21-minute drive from the airport and a 50-minute drive from Reykjavík.

Geothermal gradient is the rate of increasing temperature with respect to increasing depth in the Earth's interior.

Away from tectonic plate boundaries, it is about 25 °C per km of depth (1 °F per 70 feet of depth) near the surface in most of the world.

Strictly speaking, geo-thermal necessarily refers to the Earth but the concept may be applied to other planets.

A line tracing the gradient through the planetary body is called a geotherm on Earth and other terrestrial planets.

On the Moon it is called a selenotherm.

A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface.

Seawater, or salt water, is water from a sea or ocean.

On average, seawater in the world's oceans has a salinity of about 3.5% (35 g/L, or 0.600 M) This means that every kilogram (roughly one litre by volume) of seawater has approximately of dissolved salts (predominantly sodium and chloride ions).

Average density at the surface is 1.025 kg/l.

Seawater is denser than both fresh water and pure water (density 1.0 kg/l at) because the dissolved salts increase the mass by a larger proportion than the volume.

The freezing point of seawater decreases as salt concentration increases.

At typical salinity, it freezes at about.

The coldest seawater ever recorded (in a liquid state) was in 2010, in a stream under an Antarctic glacier, and measured.

Seawater pH is typically limited to a range between 7.5 and 8.4.

However, there is no universally accepted reference pH-scale for seawater and the difference between measurements based on different reference scales may be up to 0.14 units.