Helmcken Falls is a big waterfall.
It is in a park in Canada. The water falls down a deep canyon. In winter, a tall cone of ice grows at the bottom. It looks very pretty! Can you see the white ice?
Helmcken Falls is a big waterfall.
It is in a park in Canada. The Murtle River flows over the edge. Long ago, hot lava made the land here.
Then, big floods carved a deep canyon. In winter, it gets very cold. A huge cone of ice grows at the bottom. It can grow very tall! People even climb the ice. You can walk on a trail to see it. It is a grand place to visit.
Helmcken Falls is a big waterfall in Canada. It sits in Wells Gray Provincial Park. The Murtle River flows over the edge.
This place was made by lava. Long ago, lava filled the valley. Then, huge floods carved a deep canyon.
Robert Henry Lee found the falls in 1913. He wanted to name them after a leader. But the name Helmcken Falls was chosen instead. It honors a man named John Sebastian Helmcken.
There are six other waterfalls on this river. Some are easy to reach by road. Others need a long walk on a trail. You can see the falls from a viewing platform. There is also a trail called Brink Trail. It takes about one hour to walk each way.
Winter is a special time to visit. A giant cone of ice grows at the bottom. It can grow 50 meters tall or more! Some people even climb the ice here. They call it the Yosemite of ice climbing.
Helmcken Falls is a famous waterfall in British Columbia, Canada. It sits within the Wells Gray Provincial Park. The Murtle River flows over a high edge to create the falls.
This waterfall is very important to the park. In fact, protecting it helped create the park in 1939. There are six other waterfalls on the Murtle River nearby. These include names like Dawson Falls and Meadow Falls. Some are easy to reach by road. Others require long walks on trails or even travel by air.
This amazing place was shaped by fire and water. Long ago, lava flowed from cracks in the ground. This happened in the Wells Gray-Clearwater volcanic field. Layer upon layer of fresh lava built up a large plateau. This process started about 200,000 years ago. Then, a different thing happened at the end of the last ice age. Huge floods moved through the area about 10,000 years ago. These floods wore away the lava to carve out the deep Helmcken Canyon.
A man named Robert Henry Lee discovered the falls. He was a land surveyor working for the government. In 1913, he walked west from his remote camp. He reached the top of the waterfall on July 24. He liked the falls so much that he wrote a letter. He asked to name them McBride Falls after a leader. However, the Premier chose a different name instead. The falls were named Helmcken Falls to honor John Sebastian Helmcken. He was a doctor who helped British Columbia join Canada in 1871.
Visitors have many ways to see the water. You can drive a short paved road to a viewing platform. This platform sits on the rim of the canyon. From there, you can see a wide view of the falls. There is also a path called the Brink Trail. It is 4 km long and follows the river bank. This walk takes about one hour to go one way. You can also walk to see where the Murtle and Clearwater Rivers meet. This walk takes about 30 minutes from the main view.
Winter turns the waterfall into a frozen wonder. Most people visit during the warm summer months. But in very cold winters, a giant ice cone grows at the base. This cone can reach 50 m in height. Sometimes it even grows halfway up the falls. The best time to see this is from late January to February. Some people even visit to climb the ice. They use special skills to climb very hard ice walls. People call this place the Yosemite of ice climbing.
Helmcken Falls is a massive waterfall located in British Columbia, Canada. It is a central feature of Wells Gray Provincial Park. The waterfall is formed by the Murtle River. This river flows over a high edge into a deep canyon.
The presence of these falls was a key reason for creating the park in 1939. The Murtle River is home to several other waterfalls. These include The Mushbowl, Dawson Falls, Majerus Falls, Horseshoe Falls, Meadow Falls, and McDougall Falls. Some are easy to reach by road. Others require hiking on trails or even traveling by air.
The landscape here was shaped by intense volcanic and water activity. The falls drop over the western escarpment of the Murtle Plateau. This plateau is a huge lava deposit. It belongs to the Wells Gray-Clearwater volcanic field. This field began erupting from nearby fissures about 200,000 years ago. Fresh lava flowed in layer upon layer. This process eventually filled the wide valley of the Clearwater River.
Later, massive floods changed the land again. These floods occurred at the close of the last ice age about 10,000 years ago. The water eroded the lava to carve out the Helmcken Canyon below the falls.
A land surveyor named Robert Henry Lee is credited with discovering the falls. He worked for the British Columbia government. In 1911, Lee received a four-year contract to survey the North Thompson and Clearwater Valleys. By 1913, he was working south of the Murtle River. He was laying out lots for homesteaders. On July 24, 1913, Lee walked west from his remote camp. He reached the top of the waterfall and was very impressed. He wrote to the Premier of British Columbia, Sir Richard McBride. Lee requested that the site be named "McBride Falls."
The Premier chose a different name for the site. He decided to call it Helmcken Falls. This name honored John Sebastian Helmcken. He was a physician with the Hudson's Bay Company. Dr. Helmcken arrived in Victoria in 1850. He played a role in bringing British Columbia into the Canadian Confederation in 1871. Dr. Helmcken died in 1920 at the age of 95. Interestingly, he never actually saw the waterfall himself.
Many different trails allow people to explore the area. A short paved road leads to a viewing platform on the canyon rim. This platform offers a panorama of the falls. The Brink Trail is another option for visitors. It is 4 km long and follows the south bank of the Murtle River. This walk takes about one hour each way. There are no fences at the end of this trail. The Gatling Gorge trail is also available. It leads to the narrowest point of the Clearwater River. This trail takes about 1.5 hours each way.
Winter transforms the waterfall into a unique frozen environment. Most tourists visit during the summer. However, a large ice cone often grows at the base during cold winters. This cone can reach 50 m in height. In very cold, snowy winters, it sometimes reaches halfway up the falls. The best time to see this is from late January to the end of February. The ice cone usually collapses inward during March. Some remnants may still be visible in June.
Volunteers maintain the trails during this season. Travelers should use snow tires and tire chains for safety.
For athletes, the falls offer world-class ice climbing. The site is sometimes called the "Yosemite of ice climbing." Climbers tackle some of the highest graded ice climbs in the world. Notable climbs include Spray On, which was climbed in 2010. Other famous routes include Wolverine, Interstellar Spice, and Mission to Mars. These climbs are very difficult and require great skill.
This makes the falls a significant location for the sport of ice climbing.
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