是的，您能够预订到的度假短租屋非常靠近尼基思基的人气景区。或者，如果希望有更清静的入住环境，您也可以看看距离闹市区较远的选择。 自然风光爱好者都会喜欢尼基思基的湖畔。在此游玩期间，请务必留出时间体验这里的水上乐园。
Creekside Cottage near Daniel's Lake：旅客都喜欢这家尼基思基度假短租屋。该住宿在水滨， 也设有阳台、花园和烧烤炉，以便您在新环境中放松身心。 厨房设施包括冰箱、炉灶和微波炉。充分利用该度假短租屋提供的游戏，更好地放松自己。
有这 12 家 Expedia 度假短租屋，您一定能找到在尼基思基的理想住宿。
基奈国家野生动物保护区和小屋湖是走到户外亲近自然的当地好去处。科齐纳路和狗骨湖也是您在当地游览时的好去处。
度假出租屋是私人拥有产权的住宿，无论准备在尼基思基停留多久，它们都是理想的预订选择。 度假出租屋提供多种设施，如浴缸、壁炉和露台，让您体验到自家般的便利。 如果您很在意住宿环境是否清洁，度假出租屋可为您带来出色的私密性，让您避开狭窄的酒店电梯和人山人海的大堂，而仍能让您的旅途方便而省心。 相比传统酒店，度假出租屋可带来更多的空间，这也使其成为小型团体聚会的理想选择。
![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)
