Foto von Sharrie Shaw
Hotels in Nikiski
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Beliebte Hotels in Nikiski

Aspen Extended Stay Suites Kenai
Kenai
9.0 von 10, Wunderbar, (706)
Der Preis beträgt CHF 86
inkl. Steuern & Gebühren
17. Dez.–18. Dez.

Quality Inn Kenai
Kenai
8.4 von 10, Sehr gut, (564)
Der Preis beträgt CHF 91
inkl. Steuern & Gebühren
8. Dez.–9. Dez.

Alaska Angler's Inn
Soldotna
8.0 von 10, Sehr gut, (301)

The Kenai Inn
Kenai
8.4 von 10, Sehr gut, (48)
Der Preis beträgt CHF 89
inkl. Steuern & Gebühren
28. Nov.–29. Nov.

Best Western King Salmon Inn
Soldotna
8.2 von 10, Sehr gut, (377)
Der Preis beträgt CHF 99
inkl. Steuern & Gebühren
28. Nov.–29. Nov.

Aspen Hotel Soldotna
Soldotna
8.6 von 10, Hervorragend, (793)
Der Preis beträgt CHF 94
inkl. Steuern & Gebühren
26. Dez.–27. Dez.
Dies ist der niedrigste Preis pro Nacht, der in den letzten 24 Stunden für einen Aufenthalt mit 1 Übernachtung von 2 Erwachsenen gefunden wurde. Preise und Verfügbarkeiten können sich ändern. Es können zusätzliche Bedingungen gelten.
Spare mindestens 10% bei Tausenden Hotels, wenn du angemeldet bist
Übernachte in der Nähe beliebter Attraktionen in Nikiski
Erfahre mehr über Nikiski
Entdecke das abgeschiedene Reiseziel Nikiski: mit Kanufahren, einem Wasserpark, Camping und mehr!
![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 von Sharrie Shaw
Öffentliches Foto von Sharrie Shaw

Aspen Hotel Soldotna
326 Binkley Circle Soldotna AK
Der Preis beträgt CHF 94 pro Nacht vom 26. Dez. bis zum 27. Dez.
CHF 94
26. Dez.–27. Dez.
inkl. Steuern & Gebühren
8.6/10 Excellent! (787 Bewertungen)
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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)




























































