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Hotel Nikiski
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Nikiski : optez pour un hébergement qui change de vos habitudes
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HĂŽtels pas chers Ă Nikiski

Aspen Extended Stay Suites Kenai
Kenai
9.0 sur 10, Merveilleux, (706)
Le nouveau prix est de CHFÂ 86
taxes et frais compris
17 déc. - 18 déc.

Quality Inn Kenai
Kenai
8.4 sur 10, TrĂšs bien, (564)
Le nouveau prix est de CHFÂ 91
taxes et frais compris
8 déc. - 9 déc.

Alaska Angler's Inn
Soldotna
8.0 sur 10, TrĂšs bien, (301)

The Kenai Inn
Kenai
8.4 sur 10, TrĂšs bien, (48)
Le nouveau prix est de CHFÂ 89
taxes et frais compris
28 nov. - 29 nov.

Best Western King Salmon Inn
Soldotna
8.2 sur 10, TrĂšs bien, (377)
Le nouveau prix est de CHFÂ 99
taxes et frais compris
28 nov. - 29 nov.

Aspen Hotel Soldotna
Soldotna
8.6 sur 10, Excellent, (792)
Le nouveau prix est de CHFÂ 95
taxes et frais compris
17 déc. - 18 déc.
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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SĂ©journez Ă proximitĂ© dâattractions populaires Ă Nikiski
En savoir plus sur Nikiski
Plongez dans l'ambiance tranquille de Nikiski : des sorties en canoë, des parcs aquatiques, des espaces de camping agréables et bien plus encore vous attendent.
![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
Nikiski : les hÎtels les mieux notés
Séjours pas chers à Nikiski

Aspen Hotel Soldotna
326 Binkley Circle Soldotna AK
Le prix est de CHF 95 par nuit du 17 déc. au 18 déc..
CHFÂ 95
17 déc. - 18 déc.
taxes et frais compris
8,6/10 Excellent! (792 avis)
Foire aux questions
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HĂŽtels prĂšs de Nikiski, Kenai
Nikiski : hĂŽtels les plus populaires
- Close to Soldotna, large home on the Kenai River. Sleeps 15, 7 bedrooms, 6 bath
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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=1200&h=500&q=medium)



























































