![The Arctic Circle is one of the five major circles of latitude that mark maps of the Earth. As of 16 February 2015, it runs 66°33âČ45.6âł north of the Equator.
The region north of this circle is known as the Arctic, and the zone just to the south is called the Northern Temperate Zone. The equivalent polar circle in the Southern Hemisphere is called the Antarctic Circle.
The Arctic Circle is the southernmost latitude in the Northern Hemisphere at which the sun can remain continuously above or below the horizon for 24 hours (at the June solstice and December solstice respectively). North of the Arctic Circle, the sun is above the horizon for 24 continuous hours at least once per year (and therefore visible at midnight) and below the horizon for 24 continuous hours at least once per year (and therefore not visible at noon). On the Arctic Circle those events occur, in principle, exactly once per year, at the June and December solstices, respectively. However, in practice, because of atmospheric refraction and mirages, and because the sun appears as a disk and not a point, part of the midnight sun may be seen on the night of the northern summer solstice up to about 50âČ (90 km (56 mi)) south of the Arctic Circle; similarly, on the day of the northern winter solstice, part of the sun may be seen up to about 50âČ north of the Arctic Circle. That is true at sea level; those limits increase with elevation above sea level, although in mountainous regions there is often no direct view of the true horizon.
The position of the Arctic Circle is not fixed. It directly depends on the Earth's axial tilt, which fluctuates within a margin of 2° over a 40,000-year period,[2] notably due to tidal forces resulting from the orbit of the Moon. The Arctic Circle is currently drifting northwards at a speed of about 15 m (49 ft) per year; see Circle of latitude for more information.
#snow](https://images.trvl-media.com/place/6140564/a9f9449e-bab4-40a6-a9a1-5356b0cc2aa8.jpg?impolicy=fcrop&w=1200&h=500&q=medium)
Photo de Sharrie Shaw
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Aspen Extended Stay Suites Kenai
Kenai
9.0 sur 10, Merveilleux, (710)
« The room was clean and quiet. »
Sandra
Quality Inn Kenai
Kenai
8.4 sur 10, TrĂšs bien, (566)
« Etape sur la route de Homer, ville trÚs agréable »
Muriel
Le nouveau prix est de 99 âŹ
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15 déc. - 16 déc.
Alaska Angler's Inn
Soldotna
8.0 sur 10, TrĂšs bien, (302)
« Clean room. Room faced highway - pretty quiet until a plow truck showed up to sand or plow the business across the highway. »
Lori
Aspen Hotel Soldotna
Soldotna
8.6 sur 10, Excellent, (794)
« Love the pool and good location in town. »
Ryan
Best Western King Salmon Inn
Soldotna
8.2 sur 10, TrĂšs bien, (377)
« Did not eat breakfast »
Tom
Le nouveau prix est de 110 âŹ
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10 déc. - 11 déc.
Uptown Motel Kenai
Kenai
8.6 sur 10, Excellent, (295)
« Great place to stay! »
Edward
Le nouveau prix est de 75 âŹ
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9 janv. - 10 janv. 2026
Prix par nuit le plus bas trouvĂ© au cours des 24 derniĂšres heures sur la base dâun sĂ©jour dâune nuit pour 2 adultes. Les prix et la disponibilitĂ© sont susceptibles de changer. Des conditions supplĂ©mentaires peuvent sâappliquer.
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![The Arctic Circle is one of the five major circles of latitude that mark maps of the Earth. As of 16 February 2015, it runs 66°33âČ45.6âł north of the Equator.
The region north of this circle is known as the Arctic, and the zone just to the south is called the Northern Temperate Zone. The equivalent polar circle in the Southern Hemisphere is called the Antarctic Circle.
The Arctic Circle is the southernmost latitude in the Northern Hemisphere at which the sun can remain continuously above or below the horizon for 24 hours (at the June solstice and December solstice respectively). North of the Arctic Circle, the sun is above the horizon for 24 continuous hours at least once per year (and therefore visible at midnight) and below the horizon for 24 continuous hours at least once per year (and therefore not visible at noon). On the Arctic Circle those events occur, in principle, exactly once per year, at the June and December solstices, respectively. However, in practice, because of atmospheric refraction and mirages, and because the sun appears as a disk and not a point, part of the midnight sun may be seen on the night of the northern summer solstice up to about 50âČ (90 km (56 mi)) south of the Arctic Circle; similarly, on the day of the northern winter solstice, part of the sun may be seen up to about 50âČ north of the Arctic Circle. That is true at sea level; those limits increase with elevation above sea level, although in mountainous regions there is often no direct view of the true horizon.
The position of the Arctic Circle is not fixed. It directly depends on the Earth's axial tilt, which fluctuates within a margin of 2° over a 40,000-year period,[2] notably due to tidal forces resulting from the orbit of the Moon. The Arctic Circle is currently drifting northwards at a speed of about 15 m (49 ft) per year; see Circle of latitude for more information.
#snow](https://images.trvl-media.com/place/6140564/a9f9449e-bab4-40a6-a9a1-5356b0cc2aa8.jpg?impolicy=fcrop&w=900&h=675&p=1&q=high)
Photo prise par Sharrie Shaw
Photo libre de droits prise par Sharrie Shaw
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Aspen Hotel Soldotna
326 Binkley Circle Soldotna AK
8,6/10 Excellent! (793 avis)
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