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Hoteles en Nikiski
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Hoteles baratos en Nikiski

Aspen Extended Stay Suites Kenai
Kenai
9.0 sobre 10, Impresionante, (702)

Alaska Angler's Inn
Soldotna
8.0 sobre 10, Muy bueno, (299)

Quality Inn Kenai
Kenai
8.4 sobre 10, Muy bueno, (562)
El precio actual es de 110 €
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Del 5 dic al 6 dic

The Kenai Inn
Kenai
8.4 sobre 10, Muy bueno, (48)
El precio actual es de 95 €
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Del 18 nov al 19 nov

Best Western King Salmon Inn
Soldotna
8.2 sobre 10, Muy bueno, (377)
El precio actual es de 127 €
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Del 19 nov al 20 nov

Aspen Hotel Soldotna
Soldotna
8.6 sobre 10, Excelente, (791)
Precio más bajo por noche encontrado en las últimas 24 horas para una estancia de 1 noche y 2 adultos. Los precios y la disponibilidad están sujetos a cambios. Pueden aplicarse términos y condiciones adicionales.
Inicia sesión y ahorra una media de un 15 % en miles de hoteles
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Explora Nikiski, un destino recóndito que se suele destacar por el piragüismo, su parque acuático, sus zonas de acampada ¡y mucho más!
![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 de Sharrie Shaw
Foto gratuita de Sharrie Shaw
Mejores comentarios sobre hoteles en Nikiski
Estancias baratas en Nikiski

Aspen Hotel Soldotna
326 Binkley Circle, Soldotna, AK
8,6/10 Excellent! (791 comentarios)
Preguntas frecuentes
Te acercamos a un mundo de viajes
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Hoteles cerca de Nikiski, Kenai
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- Close to Soldotna, large home on the Kenai River. Sleeps 15, 7 bedrooms, 6 bath
- Cabin in Soldotna near scenic Kenai River
- Aventura en el río Alaska. Pesca y paz. Belleza y Outdoora. Alojamiento de lujo
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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)



























































