Ramblings of a Techno-Viking

Still Creek Campground

Still Creek Campground has 27 sites in a single loop -- 21 reserveable, 5 non-reserveable, and one host site. The sites tend to be bigger than some other nearby campgrounds, and about ten of them have a creek running in back. While the campground was full most Friday and Saturday nights, it was half-full most weeknights. 2012 rates are $20/night. The campground opened June 22, and is scheduled to close October 7. There are 3 sets of vault toilets, faucets scattered around with good tasting water, and each campsite has a fire pit and table. Firewood was available at the host site most of the summer.

There is a poorly-documented picnic area with one picnic table and two fire grates. The grates are on the other side of a fork of still creek from the table.

The Barlow Trail, a portion of the old Barlow Road part of the Oregon Trail, goes from the campground to Government Camp less than a mile away. This section has been left about like it was 150 years ago. There is a small Pioneer Cemmitary and a historical marker on the Gravel Perry Vickers Road that goes from the back end of the campground to Trillium Lake Road.

The National Forest web page on the campground has some inaccuracies -- Ramona Falls in 20 miles away, near Lost Creek Campground, and while there may be fishing in Still Creek, it would be downstream from the campground.

My responsibilities as camp host included cleaning the campsites and toilets, checking people in to campsites, and selling firewood. There was a lot more paperwork involved than I expected, including copying numbers from one form to another and adding up columns of numbers.

The Verizon signal was fairly strong, but the T-Mobile one was flakey.

Posted Friday 07 September 2012 01:53 UTC
Last edited Monday 10 December 2012 04:16 UTC
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Newberry National Volcanic Monument

Newberry National Volcanic Monument is run by the National Forest Service. Most areas require either a Northwest Forest Pass ($5/day or $30/year) or an Interagency Pass ($80/year). The Lava Lands Visitors Center is about 15 miles south of Bend, Oregon on US 97. There are a couple of interpretive trails and a one-mile drive that spirals up Lava Butte to a viewpoint -- due to limited parking you need to drive a short vehicle and get a pass for Lava Butte. Trees in the lava field frequently grow in spirals, caused by the root on one side getting more nourishment than the other.

Lava River Cave, a little further south from the visitor center, is a large volcanic tube, it is about a mile from the entrance to where the cave is blocked. Almost all of it can be walked upright, only a few sections did I need to stoop. It was very busy Labor Day Sunday.

Lava Cast Forest was not busy the Friday I went. The 9 miles of bad washboard gravel road probably discourages many people. However it was an interesting mile long interpretive trail. Lava flowed around many trees and left molds where the wood was. There are a number of opportunities for dispersed camping along the many dirt side roads before entering the national monument. (Dispersed camping is not allowed in the monument.)

Paulina Falls is near the entrance to Newberry Caldera. There is a short trail from the parking area or the visitors center.

Newberry Caldera has two lakes in it: Paulina Lake and East Lake. Neither is close to as deep as the more famous Crater Lake. (Crater Lake is in another Caldera about 100 miles away.) The lakes did not have fish until they were stocked in 1912. Both have multiple boat ramps and motor-boats are allowed.

I stayed at the Cinder Hill Campground. Sites are $16/night, and many of the over 100 face East Lake. Surprisingly I was able to get a weak Verizon signal with my external antenna and amplifier. There were hundreds of tiny frogs hopping around near the lake.

Big Obsidian Flow is the most recent lava flow in the state of Oregon.
It has an interpretive loop trail with views of Paulina Lake. Good shoes are recommended, the trail surface is mostly mixed pumice and obsidian.

Posted Thursday 20 September 2012 02:26 UTC
Last edited Monday 10 December 2012 04:16 UTC
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