斷層省立公園

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 (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)


熱門景點


熱門斷層省立公園飯店優惠

卡里布小屋

卡里布小屋

2.5 out of 5
1414 Cariboo Highway Clinton BC
卡里布小屋
朗得亞普汽車旅館

朗得亞普汽車旅館

2 out of 5
1214 Kelly Lake Road Clinton BC
朗得亞普汽車旅館
99 英哩汽車旅館

99 英哩汽車旅館

2.5 out of 5
896 Alpine Ave 100 Mile House BC
99 英哩汽車旅館
聖賢山汽車旅館

聖賢山汽車旅館

2.5 out of 5
1390 Cariboo Hwy 97 Cache Creek BC
聖賢山汽車旅館
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