Foto oleh Sharrie Shaw
Hotel murah di Nikiski
- Ubah fikiran andaTempah hotel dengan pembatalan percuma
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Jangkau melebihi penginapan biasa anda di Nikiski
Pangsapuri
Kotej
Semak harga untuk tarikh ini
Malam ini
Esok
Hujung minggu ini
Hujung minggu depan
Pilihan teratas kami untuk hotel di Nikiski
Harga ialah RM474
RM503 jumlah
termasuk cukai & fi
21 Dis - 22 Dis
Harga ialah RM426
RM451 jumlah
termasuk cukai & fi
20 Dis - 21 Dis

9.0 daripada 10, Hebat, (714)
Harga ialah RM446
RM473 jumlah
termasuk cukai & fi
29 Dis - 30 Dis
Harga ialah RM364
RM385 jumlah
termasuk cukai & fi
27 Dis - 28 Dis

8.0 daripada 10, Sangat Baik, (303)
Harga semalam terendah yang ditemui dalam masa 24 jam lalu berdasarkan penginapan 1 malam untuk 2 orang dewasa. Harga dan ketersediaan adalah tertakluk pada perubahan. Terma tambahan mungkin dikenakan.
Jimat purata sebanyak 15% pada beribu-ribu hotel apabila anda log masuk
Menginap berhampiran tarikan Nikiski popular
Ketahui lebih lanjut tentang Nikiski
Jelajahi yang Nikiski terpencil: berkanu, taman air, kembara dan banyak lagi!
![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
Ulasan Hotel Nikiski Popular
Penginapan murah di Nikiski

Uptown Motel Kenai
47 Spur View Drive Kenai AK
Harga adalah RM364 semalam dari 27 Dis hingga 28 Dis
RM364
RM385 jumlah
27 Dis - 28 Dis
termasuk cukai & fi
8.6/10 Excellent! (289 ulasan)
![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)































































