Foto di Sharrie Shaw
Hotel a Nikiski
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I nostri consigli sugli hotel in questa destinazione: Nikiski

9.0 su 10, Meraviglioso, (716)
Il prezzo attuale è 113 €
tasse e oneri inclusi
1 feb - 2 feb
Il prezzo attuale è 113 €
tasse e oneri inclusi
8 gen - 9 gen
Il prezzo attuale è 101 €
tasse e oneri inclusi
18 gen - 19 gen

8.2 su 10, Ottimo, (379)
Il prezzo attuale è 126 €
tasse e oneri inclusi
9 gen - 10 gen
Prezzo a notte più basso trovato nelle ultime 24 ore, per un soggiorno di 1 notte per 2 adulti. Prezzi e disponibilità possono cambiare. Potrebbero essere previste condizioni aggiuntive.
Accedi al tuo account e risparmia in media un 15% su migliaia di hotel
Soggiorna vicino alle attrazioni popolari di Nikiski
Maggiori informazioni su Nikiski
Lasciati conquistare dal fascino di una destinazione tranquilla come Nikiski: tra le attività in canoa, l'imperdibile parco acquatico e l'escursionismo, le alternative non mancheranno affatto!
![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°33′45.6″ 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 50′ (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 50′ 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)
Foto di Sharrie Shaw
Foto gratuita di Sharrie Shaw
Migliori recensioni hotel nei pressi di Nikiski
Alloggi economici a Nikiski

Uptown Motel Kenai
47 Spur View Drive Kenai AK
Il prezzo è 81 € a notte nel periodo 17 gen - 18 gen
81 €
17 gen - 18 gen
tasse e oneri inclusi
8,6/10 Excellent! (294 recensioni)
Domande frequenti
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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°33′45.6″ 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 50′ (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 50′ 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)



























































