Foto oleh Sharrie Shaw
Temukan Hotel Bintang 3 di Nikiski mulai dari mulai dari Rp2.220.108
- Berubah pikiranPesan hotel dengan pembatalan gratis
- Banyak pilihanCari di hampir jutaan properti di seluruh dunia
Cek ketersediaan Hotel Bintang 3 di Nikiski
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Pilihan terbaik kami untuk hotel bintang 3 di Nikiski
Harga sekarang Rp2.018.280
total Rp2.220.108
termasuk pajak & biaya lainnya
13 Jan - 14 Jan

8.0 dari 10, Sangat Baik, (304 ulasan)

10.0 dari 10, Sempurna, (1 ulasan)

10.0 dari 10, Sempurna, (3 ulasan)

Woodsy Cabin Near Kenai River: Great for Anglers!
Woodsy Cabin Near Kenai River: Great for Anglers!Soldotna

10.0 dari 10, Sempurna, (2 ulasan)

10.0 dari 10, Sempurna, (2 ulasan)
Hemat rata-rata 15% untuk ribuan hotel saat Anda login
Jelajahi hotel bintang 4 yang serupa
Banyak hotel bintang 4 memiliki fasilitas yang sama dengan hotel bintang 3. Lihat semua hotel bintang 4 di Nikiski.

ALASKA LAKE and LODGE AT LONGMERE
38780 Longmere Way Soldotna AK
8,2/10 Very Good! (26 ulasan)
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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=900&h=675&p=1&q=high)
Foto oleh Sharrie Shaw
Foto Terbuka oleh Sharrie Shaw
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Panduan Saku: Hotel Bintang 3 di Nikiski
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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)









































































