We set out on the road again for our last week of the summer trip. We left Mailea’s on Thursday afternoon, July 24, and drove south through Oregon in search of another hot springs on our way to Crater Lake and eventually the Redwoods.

Umpqua Hot Springs is located inland in southern Oregon near the northwest approach to Crater Lake. We found the turn off and drove a few miles on a National Forest dirt road before reaching the gravel parking area for the trailhead and undeveloped campground. The trail to the hot springs is a .3 mile side trail off the North Umpqua River trail and the description is “short but steep.” That describes it exactly! After crossing the solidly constructed bridge over the North Umpqua River (with a colorful parrot belonging to one of the campers gracing the bridge entrance), we started climbing up a STEEP slippery trail and I was very grateful for the hand rail that had been installed. We topped out and walked a level dry pine needle covered path before we descended slightly to the springs.

We had read that the hot springs consisted of a series of travertine lined natural pools but in person it was impressive to see these naturally formed little hot tubs created from the minerals in the water cascading down the hillside. The only man-made structure was a deck and roof built over the largest pool. It was a handy spot to put our towels and bags as we moved among the different temperature pools and soaked away the miles.

“Situated on a clifftop perch, Umpqua Hot Springs’ view of the North Umpqua River below is one of Oregon hot springs’ most memorable. It certainly adds to the soothing pleasure of soaking in this spring. There are two to three oval pools for soaking above and behind the main, covered pool. The larger pool is tub-like due to the minerals from the spring creating a travertine mound over the centuries that caps the cliffside. The main pool exists sunken into this travertine stone with the view opening like an ampitheater to soakers. The upper, smaller pool is 4 by 5 feet and 112 degrees F; the lower, larger pool is 5 by 8 feet and 110 degrees F. Both pools are 2-3 feet deep and floored with coarse sand.” OregonHotSprings

Hot Springs Geology

“Volcanic activity that formed this area within the High Cascades less than two million years ago is still cooling. Here, molten rock just a few thousand feet below the surface transmits heat upward through solid rock, heating the ground water that has penetrated to that depth. Hot water then forces its way up through fissures and fractures to escape to the surface, forming hot springs. Extremely hot water dissolves large amounts of silica, a common component of volcanic rock. These dissolved silica minerals are deposited as water flows over the surface and cools. Over thousand of years the deposits have accumulated, building the hot springs mound that overlooks the North Umpqua River.” From the information sign at the Trail entrance.

There were a few other groups enjoying the pools with plenty of space for all of us to have a private pool. We stayed until the daylight was waning and hiked back before darkness overtook the trail. We wanted to camp nearby but the undeveloped campground was full of loudly partying groups so we decided to drive on. About ½ mile away was a great spot by the river but two tents were already there. Neil asked if they minded if we camped nearby and they were fine with it. We finished setting up the tent in the dark with our headlamps. Good thing we were getting to be old hands at setting up camp. We were asleep soon after and have no idea how late our neighbors stayed up enjoying their fire.

We woke with the sun and hopped in the car back to the hot springs. Only one couple was there that early (the campground partiers were probably still asleep, yeah). We soon had the pools all to ourselves and watched the sunlight light up the forest trees as it topped the mountain. Thoroughly toasty and buoyant of spirit, we went back to pack up the tent and were on the road before most campers were up.

Photo Credit: Neil Rhoads

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