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New Wave Rafting New Mexico Whitewater Rafting
New Wave Rafting New Mexico Whitewater Rafting
New Wave Rafting New Mexico Whitewater Rafting
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New Wave Rafting Blog

Whitewater Rafting in Northern New Mexico


How River Levels Affect Your River Trip

Summer river levels of the Rio Grande.

River levels of New Mexico’s Rio Grande are dynamic.

Why Do Water Levels Fluctuate?

The Rio Grande is one of the longest continuous rivers in the United States. Born in the deep snows of southern Colorado it provides water and recreation for Colorado, New Mexico and Texas. The winter snow pack determines just how much water fills the river in the spring.  Every year that amount is different. Other factors such as water rights for irrigation and municipal water affect that amount of flow.

River levels in late summer on the Rio Grande.

Late summer water level at Big Rocks Rapid.

How Do Different River Levels Affect Your Trip?

Rafting conditions depend on just how much water flows through the river canyon. Water levels tend to be higher throughout the spring and into the summer. Some years our monsoon season in July and August can also raise levels. For those seeking the highest adventure level, the early season May and June can provide the thrills and chills and the best whitewater excitement. Further into the summer the river becomes lower and produces the best whitewater fun for families and kids.   Summer fun includes piloting your own inflatable kayak or funyak through the scenic parts of the canyon.
    The Racecourse, so named for the annual Mother’s Day race event, becomes technically challenging through medium size rapids. Here your guide will  pilot you through Albert’s Falls, Herringbone, The Narrows, Big Rocks, and Souse Hole!

High water of the Taos Box on the Rio Grande, New Mexico.

Early spring high water of the Taos Box.

SEE YOU ON THE RIO!

(images courtesy of BrittRunyonImages)

Hold On Tight

“Hold On Tight” is the headline, but it’s not accurate. Rafting in big whitewater is a participatory activity. The guide yells out paddle commands and the guests respond with enthusiastic strokes of their paddles. As a rule, holding on is not an option. But what keeps you in the boat, as it crashes into waves and then bucks upward? It’s your paddle that keeps you in the boat. You get support from the paddle as you pull on it. It’s your third item of attachment to the raft, along with your rear-end contact and your feet placed under a thwart. Believe me … it really works like that. And your aggressive strokes are needed to power the raft through big waves and propel the boat in the direction determined by your guide. So, don’t hold on tight!  New Wave Rafting Co co-owner Steve Miller is quoted below.

 

 

 

 

Rafters looking for big water, big year

Rafters looking for big water, big year

For all you rafters out there, Excerpts from Albuquerque Journal, May 5, 2019.

“And as Northern New Mexico’s rafting season gets underway, local outfitters say they are gearing up for what are expected to be “phenomenal” conditions … “

“We’re tickled pink,” said Steve Miller, co-owner of New Wave Rafting based in Embudo. “For us, water is everything …”

Two rafts from New Wave Rafting Co. leave John Dunn Bridge and head through the Taos Box on Thursday. (Eddie Moore/Albuquerque Journal)

Rafters pass under the Gorge Bridge.

Britt Runyon, top, the operations manager for New Wave Rafting Company, guides a raft through a rapid in the Taos Box stretch of the Rio Grande on Thursday. River flows are starting to build toward a peak expected in late May. (Eddie Moore/Albuquerque Journal)

The Sleeping Beauty Wave!

The Sleeping Beauty Wave is found on the Racecourse section of the Rio Grande, and is guaranteed to get you wet, as you can see in this video. The Racecourse half-day trip is offered twice a day, at 9m AM and 1 PM. It is also the afternoon portion of the full-day Rio Grande Gorge trip. This is a very scenic section of the Rio Grande, with black volcanic mesas on the right side of the river, and steep quartzite cliffs on the left side of the river. Why the difference? It’s because the river is following the Embudo fault here, which broke off the end of the quartzite Picuris Mountains, making the cliffs. Then, lava flowed from the west up against the base of the cliffs, pushing the river ahead of it and into its present position, up against the base of the cliffs. The video is by Britt Runyon, New Wave’s Operations Manager and Videographer. And that is Britt also guiding the raft. Clever, isn’t he?

https://www.facebook.com/NewWaveRafting/videos/645974902492357/