跳到页面主要部分
选购旅游产品
选购旅游产品
选购旅游产品
住宿
住宿
机票
机票
租车
租车
套餐
套餐
旅游活动
旅游活动
优惠
团体及会议
最后时限优惠
打开 App
HKD
发布您的住宿
联系我们
行程
Communication Center
登录
通过会员价解锁折扣立减
通过 One Key™ 计划在我们各品牌平台获得奖励
登录
我要提建议
北美
查斯姆省立公园
不列颠哥伦比亚
加拿大
北美
计划您的旅行
查斯姆省立公园周边酒店
飞往不列颠哥伦比亚的航班
不列颠哥伦比亚旅游活动
查斯姆省立公园租车
不列颠哥伦比亚度假
查斯姆省立公园
At the close of the Ice Age about 10,000 years ago, a stream fed by melting ice cascaded over a falls forming this chasm by cutting into some of the lava flows that helped to build the Fraser Plateau. Individual lava flows are shown here by the horizontal layering (left hand side of the pic). When the glacial ice finally disappeared, the flow of meltwater stopped. (September 2019)
At the close of the Ice Age about 10,000 years ago, a stream fed by melting ice cascaded over a falls forming this chasm by cutting into some of the lava flows that helped to build the Fraser Plateau. Individual lava flows are shown here by the horizontal layering. When the glacial ice finally disappeared, the flow of meltwater stopped. We could hear the sound of water falling in the distance. The Chasm can be accessed by taking Highway 97 to 16 km north of Clinton, and then driving 4 km to the park on a paved road east of Highway 97. It can also be accessed from further north off Highway 97 about 15 km southwest of 70 Mile House. (September 2019)
2
查看全部 2 张照片
套餐
住宿
机票
租车
旅游活动
已添加住宿
已添加机票
经济舱
已选择
经济舱
经济舱
高端经济舱
高端经济舱
商务舱
商务舱
头等舱
头等舱
出发地