Tag Archives: backyard explorations

exploration quikie: Salt creek bridge

One of the usually submerged historic highway bridges in Shasta Lake

The Salt Creek Bridge was built on the Pacific Highway in 1925 between what is now Lakehead and Redding. This bridge apparently replaced one built some years earlier, as the older abutments are visible underneath the newer structure. It was later abandoned in 1941, as US Route 99 (the former Pacific Highway) was rerouted in anticipation of Shasta Lake inundating the older route (as happened in 1948).

In dryer or drought years, the Salt Creek Bridge is one of the first submerged artifacts to make its appearance as the lake level falls. It is easily accessible from the Salt Creek exit on Interstate 5. Take Lower Salt Creek Road west for about 3 miles at which point you will come to the bridge underneath the towering Union Pacific railroad trestle.

My visit to the site got a little more interesting, as I ran into a gentleman making casts of footprints in the muddy bank of creek upstream of the bridge. He believed them to be evidence of Bigfoot-like creatures. I have to say the footprint and casting of others he had made in the area didn’t look quite human. He proceeded to show me dozens of pictures of like footprints he had found at numerous sites, as well as other weird things that apparently Bigfoot hunters believe are evidence of the mythical creature actually existing. I came away from the conversation thinking I might have to make my forays into the area forests with a new viewpoint.

The Salt Creek Bridge underneath the towering Union Pacific railroad trestle. This is looking south, as the Salt Creek Bridge is oriented east-to-west.
The south side of the bridge.
Looking west down the old highway grade. The shadow is from the trestle above.
Looking east.
Another south side view.
Date stamp on the Salt Creek Bridge.
Another south side view looking east. Notice the flared ends of the railing.
Flared railing at the ends.
Footing from a previous bridge on this spot, probably built when the US 99 predecessor Pacific Highway was built. The previous bridge would have probably been only 15 feet wide.
The underside looking towards the east end. The previous bridge footing can be seen in the center.
Since the 1925 bridge was higher than its predecessor, the road approachmentds had to raised. This is the reinforcement of the east approach.
Evidence of Bigfoot?

All in all, the bridge is in great condition. This is likely due to being submerged in the cold waters of Shasta Lake most of the year. If you decide to drive across the span, beware of the approaches, as there are gaps between the bridge and the road.

Heading west along US 99 through the settlement of Salt Creek before the site was inundated by Shasta Lake. Some structures were move elsewhere before inundation.
Eastman, Jervie Henry. (1941). “Salt Creek Bridge” on Highway 99 near Redding, Calif. Retrieved April 2, 2021, from https://digital.ucdavis.edu/collection/eastman/D-051/B-1/B-1367

The Salt Creek Bridge on bridgehunter.com

A SEARCH FOR W 12

An abandoned railroad bed, a lost benchmark, & things found

Shortly after moving back to the Mount Shasta area (after leaving as a child in 1963), I began exploring the remains of the Weed Lumber Railroad. The railroad was built in the early 1900’s by lumber baron Abner Weed, to exploit the abundant forests east of the town he founded, with the segment from Weed to Grass Lake being sold to Southern Pacific shortly thereafter. When Southern Pacific opened the new Black Butte Subdivision (from Black Butte, just south of Weed, to Klamath Falls) bypassing the Weed-Grass Lake segment in 1926, the original ex-Weed Lumber Railroad portion was abandoned.

One piece of old right-of-way of interest winds its way along a tongue of lava south of US 97 to Bolam Road, a road which heads south from 97 to the Union Pacific control point of Bolam. I initially walked this segment one day after noticing the raised manzanita and creosote choked railbed heading south off of 97. Later, after checking topographic maps of the area, I noticed that older maps indicated the presence of a benchmark along the railbed. Searching the National Geodetic Survey benchmark database, I found that this one was still listed as Siskiyou County W 12 (PID MX0021).

The datasheet station description of the benchmark is one of the more confusing that l’ve read.

  • First, it lists the benchmark as being monumented in 1919, but the description seems to have been written in 1954, during a recovery visit to the site by a Coast and Geodetic Survey team. However, it also says that the benchmark was not found.
  • Second, it describes the mark as “on the abandoned Southern Pacific Co. roadbed, 9-1/2 poles (156.75 feet) southeast along the roadbed from the crossing of the Weed-Dorris highway” which matches placements on the 1934 Macdoel and 1954 Lake Shastina topographic maps. However, then the description reads “about 300 feet west of the highway, about 300 west of milepost 12“, which doesn’t make sense as the indicated position of the benchmark on the 1934 and 1954 maps puts it south, not west, of US 97. Of further note, the description notes the old highway – I can find no record of any highway other than 97 at this spot predating 97 before its construction. The only thing I can think this refers to is perhaps that US 97 was straightened between its original construction around 1936 and 1954, when the above mentioned topo map shows its present roadbed. An aerial photo on historicalaerials.com seems to show an older highway trace crossing Yellow Butte Road (which itself is the old Weed Lumber Railroad bed heading north from the segment being discussed here) about 75 feet north of the modern US 97.
  • Third, the description says that the mark is “near the middle of a side hill rock cut, 12 feet east of the centerline of the roadbed, in bedrock, 1 foot higher than than the roadbed”. Okay, so the 1934 Macdoel map seems to indicate that the mark is on the west side of the roadbed (or, railbed), as the roadbed travels north-to-south along the east side of the lava flow. The railbed climbs up in elevation from US 97 along the lava flow, on a constructed berm, with no rock existing on the east side of the railbed. Additionally, the aforementioned “9-1/2 poles” or 156.75 feet placement from the intersection of the railbed and the Weed-Dorris highway, either from the modern intersection placement, or the suspected original intersection, lands nowhere near any “bedrock”.
Macdoel 1934 topographic map
Lake Shastina 1954 topographic map

The datasheet states that two recovery efforts were made in 1981 to locate the benchmark, both unsuccessful.

My search efforts

I’ve made three visits to the area to search for the benchmark. I examined both sides of the railbed, including the east side which does not travel next to any bedrock formations. On the west side of the railbed, I searched further than the 12 feet from the centerline where I could, and up to 10 feet or so up the side of the lava flow. Significant erosion of the andesite bedrock along the east side of the railbed has occurred, with several small landslides along the alignment present, and in other places the hillside rock has broken in large chunks, falling onto the roadbed. I spent a lot of time scraping dirt off of the hillside bedrock, hoping to find the brass disk underneath, but it wasn’t to be. My efforts extended from the railbed crossing at US 97 south for 2000 feet, well beyond the distance stated in the datasheet.

Looking south down the abandoned railbed from US 97. At the center of the photo, the railbed starts to curve to the left (east).
Example to the eroded hillside along the west side of the railbed.

I did find numerous railroad ties, remnants of signal poles, a piece of a glass insulator, and a railroad spike, as well as numerous tin cans, probably left by railroad or salvage crews.

My conclusions

The NGS benchmark locator shows both benchmarks in the wrong locations. D 495 RESET is on the north side of the highway, and W 12 was located 2000 feet to the southwest.

What happened to the benchmark disk? I suspect one of several things could have occurred: 1) a worker took the disk as a souvenir during rail salvage and demolition; 2) someone else took it while exploring the area after railroad operation ceased, looking for collectibles such as bottles, glass insulators, or tools (my grandparents did this for years, searching out old railroad, lumber, and fire camps); or 3) the disk is still attached to a piece of rock that is now buried amongst the erosion.

My efforts were not without accomplishment. On my last visit, I did recover a nearby benchmark, D 495 RESET (PID MX0023), as well as 3 Caltrans survey markers, and found a geocache as well.

W 12 on the Siskiyou County benchmarks page

A Daytrip Around a Big Mountain

After a few weeks of self isolation, and the onset of great spring weather, my wife and I headed out for a day trip through eastern Siskiyou County, as well as parts of Shasta, Lassen, and Modoc counties, California, and Klamath County, Oregon.

This is sparsely inhabited country, consisting of national forest lands, large ranching and farming operations, small towns, and stunning volcanic, forested, and high desert vistas. This was mostly a scouting trip to plan future explorations. Some parts of this country I had never been to, and others it had been decades since I visited. 

We drove this loop counterclockwise, starting in Mount Shasta.

Inside the 300 mile round loop is found Mount Shasta; the Medicine Lake Highlands, including the massive Medicine Lake Volcano; the McCloud, Pit, and Fall rivers, which flow into the Sacramento and then the Pacific Ocean through the Golden Gate some 300+ miles south; Lava Beds National Monument; the Tule Lake and Lower Klamath National Wildlife Refuges; the remains of historic lumber, agricultural, and railroad operations; large cattle ranches; numerous alfalfa, hay, potato, garlic, onion, and horseradish farms; and Native American reservations and historic sites. The trip also skirts the Klamath River along the Oregon border.

This region on the eastern side of the Cascades is classic Basin and Range landscape, combined with the spectacular results of Cascade volcanism. 

We loaded on provisions for the day to minimize our contact with others. We drove counterclockwise from Mount Shasta on this loop. State Route 89 (Volcanic Legacy Scenic Byway) going east takes you through the former lumber town of McCloud, then through federal and privately held forest lands for about an hour until reaching the junction of 89 and State Route 299 (Lassen State Highway). This portion of the drive treats one to an impressive view of Mount Shasta’s east side, as well as titillating turnoffs to a multitude of destinations (McCloud River and its falls; Pondosa ghost town; stretches of the abandoned McCloud Lumber Railroad (now a multi use trail); and Burney Falls and the nearby railroad bridge used in “Stand By Me”). 

As you approach the 89/299 junction, the forest gives way to views of grass covered valleys, flood basalts, and other volcanic structures, such as cinder cones and impressive secondary volcanic peaks in this eastern side of the Cascades, such as Burney Mountain (7864 feet). As you head east on 299 to the town of Fall River Mills, the highway climbs a volcanic ridge, with a spectacular canyon carved by the Pit River to the south. Here, one gets a view of Lassen Peak, as well as other prominent secondary volcanic peaks between Lassen and Mount Shasta. 

Forests give way to grass covered valleys as you near Burney, driving from McCloud.

It’s amazing how much water there is in these parts. Just north of Fall River Mills lays Ahjumawi Lava Springs State Park, which is only accessible by boat. According to Wikipedia, “The park sits on “one of the nation’s largest systems of underwater springs.” They produce some 1.2 billion US gallons (4.5×109 l) of fresh water per day into the aboveground waterways. Water in the springs originate as snowmelt from the Medicine Lake Volcano highlands.”

A readout just outside of Fall River Mills reveals the volcanic structure of the area. Layered cinder cone deposits are covered by a newer lava flow.

The towns along this trip are for the most part shells of their former selves. With the mechanization of logging and farming operations, the closing of smaller milling operations, railroad mergers, and the shift towards more sustainable industries (i.e. tourism), these are settlements still looking for a purpose and relevance in today’s world. Fall River Mills has done better than most, with a golf resort, nearby hot springs, and retirement development. Other towns are struggling to repurpose themselves. 

We stopped to inspect a forest service campground and have lunch. Just a few miles north of Adin is the Lower Rush Creek forest service campground, only 3/4 of a mile off of combined State Route 299/139. It was a nice little campground with the creek running through it, but you drive past several manufactured home hovels to get to it. In fact, the campground is situated within 200 yards of one of these shacks. I’m not quite sure what a night would be like at this site, as it seems that several of the nearby properties house cannabis grow operations. There is another campground (Upper Rush Creek) farther up the road, but the road was not yet open for the season beyond this campground.

At Canby, we turned north on 139 towards Oregon, we finally popped into the southern end of the Klamath Lake Basin. We made our way into the Lava Beds at Petroglyph Point, containing one of the largest panels of Native American rock art in the United States. It was pretty awesome, but sad at the same time, as one also sees the the results of vandalism thrust upon such a significant cultural treasure. 

From here, Mount Shasta again dominates the landscape, with Mount McLoughlin in Oregon also visible to the north. By this time, it was getting late in the afternoon. We headed briefly to Merrill, Oregon, where we used the bathrooms at the local Dollar General, then headed west on California State Route 161. We stopped for a few moments to enjoy the golden hour at Lower Klamath Wildlife Refuge, watching the birds at a gorgeous viewing platform. With hunger pains not too far from manifesting themselves, we headed home to Mount Shasta to grab some takeout before finally arriving home.

The Lower Klamath Wildlife Refuge, with Mount Shasta in the distance.

Historic Highways: Old US 99, Weed, CA

I spent an hour or so this afternoon exploring a small section of Edgewood Road going north out of Weed. This used to be US Route 99, before Interstate 5 was built and replaced Highway 99.  I concentrated my efforts on one curved section of the road, examining old wooden guard rails, and looking for “C-blocks”, which are old California Division of Highways survey monuments. I did not find any, but I’ll return and spend a little more time in the brush looking for any that might exist.

The general location of my efforts was 41.43049, -122.39933

1954 USGS 15 minute topographic map showing the US 99 alignment.

2010 USGS 7.5 minute topographic map showing the US 99 alignment next to Interstate 5.

Heading north into the curve. Broken wood guard rail is on the right.

Reflector bracket.

Railroad property line markers delineate the old highway right of way on east side. These should assist in locating any “C-blocks”.

The rail is actually comprised of three pieces of layered lumber.

Bolt head.

Retaining nut.

Guard rail at the north end of the curve (looking south).

Dog Creek Bridge

An accessible, historic, and photogenic bridge worth exploring

Trip dates: November 24 & 25, 2017

The Harlan D Miller Memorial Bridge, known also as the Dog Creek Bridge, is an abandoned concrete arch bridge completed in 1927 as part of US Route 99 just north of Lakehead, Shasta County, California. After Route 99 was replaced by Interstate 5, it carried traffic as part of Interstate 5 until a bridge to the northwest was expanded to accommodate both directions of traffic in 1974. It was abandoned and slated for demolition, until saved due to efforts of concerned citizens, and is now managed by the US Forest Service.

According to Bridgehunter.com,

Harlan D Miller (1880-1926) was the State Bridge Engineer for the California Highway Department from 1923 until his untimely death in 1926. During his short tenure as State Bridge Engineer he made radical changes to the way California designed bridges. These changes included requiring all highway bridges in the state be designed by the state and designing bridges that matched the geometry of the roadway. The latter often complicated design fork but the final result (skewed or curved bridges) justified the efforts in drivability.

Miller’s most visible effect on California bridges was the consideration given to design aesthetics. His designs were recognized in their own periods as possessing beauty and boldness. Many fine details can be seen on Miller designed bridges including rail and end post details, as well as clean lines and details of the superstructure design.

When my family relocated to the Bar Area in 1963, I remember driving across this bridge as we traveled to the Mount Shasta region to visit relatives several times per year. After the bridge was decommissioned, it had always been my desire to explore the now abandoned structure. I finally had a chance to do so this past week.

Looking west at the span. Photo taken from bridge that crosses the Sacramento River. A short railroad bridge is visible to the left which also spans Dog Creek.

Looking south down the bridge deck.

Looking south along the west side of the bridge. Notice the blue tiles in the deck wall pillars.

Curb details.

The view south looking down the Sacramento River.

Looking north up the Sacramento River.

At several places benched areas were provided for travelers to stop, enjoy the views, and rest a bit.

Stone retaining on the northern approach to the span.

Dog Creek.

Looking north. The Interstate 5 span can be seen near the center.

DIRECTIONS & ACCESS

Off Interstate 5, take the Vollmers/Delta exit. Proceed west about a quarter mile and turning left onto Fenders Ferry Road. Drive down along the Dog Creek watershed for about a mile, crossing the creek twice and underneath the I5 span until reaching the historic bridge. Park just before the railroad tracks, and climb up the east side of northern end of the bridge.

According to a couple of other websites, there is supposedly access at the northern end of the bridge from the top, at end of a private road where a Forest Service begins. I checked it out and I’m not comfortable at this time on recommending its use. The adjoining property owners have posted a lot of onerous signage, and have tried to unsuccessfully block the easement. I would be nervous parking my vehicle here. Check this post for updates, as I will attempt to get clarification from the Forest Service regarding use of this easement.

FURTHER READING

redding.com (Redding Searchlight newspaper website) article Travelin’ in Time: Dog Creek Bridge, a work of art, was almost demolished,  posted June 26, 2008

CalTrans Digital Collections, Historic Bridges and Tunnels: Dog Creek

 

Deadfall Lakes, Siskiyou County, CA

A string of lakes located in the Trinity Mountains
Trip date: August 11, 2017

The trailhead is 19 miles west of Weed on Forest Service Road 17/42N17.

One of several meadows that the trail passes through.

The Pacific Crest Trail crosses the Deadfall Lakes Trail just east of the lowermost lake.

Lake 7259 (it’s noted elevation on topo maps) is the largest lake of the 5 lakes.

The uppermost of the Deadfalls lake. Mount Eddy is the peak in the background.

Looking north across the uppermost Deadfall Lakes.

Wildflowers were abundant along the trail.

Yellow Butte, Siskiyou County, CA

Looking south to Mount Shasta from the Yellow Butte high point. The middle and south peaks of the ridge line can be seen in the center.

Trip date: May 4, 2017

Yellow Butte is a hill on the north side of US Highway 97 about 12 miles northeast of Weed. Unlike other nearby peaks which are some kind of volcanic feature (dome, cinder cone or shield volcano), Yellow Butte is an uplifted complex of intrusive igneous and metamorphic rocks. This makes for some interesting quartzite outcrops on the top of the hill, and the unexpected diorite pluton along the first third of this route I hiked today.

Yellow Butte is actually more of a ridge, with three distinct peaks, the northernmost being the highest.  The route I’ve seen described elsewhere is a 3 mile round trip starting inside a Forest Service gate alongside Highway 97 that traverses the west side of the hill. Because my available time was short, I chose a shorter route on the east side of the hill on Yellow Butte Road, a narrow, dusty two-track off of 97.  This route proceeds up to saddle area between the middle and north peaks. Truth be told, both routes to the peak are old two tracks themselves – in fact, one could drive to the summit in a 4WD high clearance vehicle. But, as I got near the top, I encountered a guy camping in a beat-up, 30 year old, 2WD, low clearance Chevy van at the top – so don’t I guess I don’t know what I’m talking about.

Summit area of Yellow Butte high point.

Quartzite outcrop atop Yellow Butte.

Looking west at Haystack (left) and cinder cone 3924 (right).

Thistle along the trail.

 

I could not locate a survey triangulation mark indicated on some older topo maps. Neither could I find a summit log, so I left a new one behind.

NOTES:

Trip time is about 25 to 30 minutes each way.

For an excellent discussion of the geology of the lower Shasta Valley, see a masters thesis by Joseph Holliday, “The bedrock geology of the southeastern Shasta Valley, Siskiyou County, California”

 

Haystack

No needles involved, just a great little hike
Trip date: April 21, 2017

Haystack is a volcanic feature rising above US Route 97 11 miles northeast of Weed. The peak offers wonderful views of Mount Shasta to the south,  the Trinity Mountains to the east, and the Mount Shasta Valley to the north. The trail is an overgrown 4WD trail to the top. Good parking is just off the highway inside a Forest Service gate. One walks about .4 mile before reaching the actual trail that starts the climb up the east flank of Haystack. The short climb takes a moderate effort to reach the top. The trail circles the rather flat, open top. Vegetation is typical high desert scrub with the scattered juniper tree. There is a high point marked with a cairn with a survey mark underneath and a summit log. The summit log revealed that Haystack is visited every few days by hikers. The distance from the parking area to the high point is about one mile.

Haystack as seen from US Route 97.
My hiking partner & daughter, Claudia, on the trail as it climbs the east flank of Haystack.
Old growth juniper dots Haystack.
Summit cairn with benchmark and summit log.
Panorama from east to west, with Mount Shasta to the south. The Whaleback is to the left of Mount Shasta, and Mount Eddy is to the right. Click on the photo for a larger view.
Mount Shasta as seen from Haystack.

Spud Rock Spring Via Turkey Creek Trail

A challenging but spectacular scenic hike

Trip dates: November 13-15, 2015

This was my first backpacking trip in over 10 years. I went with my buddy Joe, who’s about the same age as I, and we took the 15 year old son of a friend who couldn’t go due to back problems. Ryan is a good kid, in great shape, and has a great attitude.  And who has a fondness for aluminum foil.

Sign at the primary trailhead at Miller Flat.
Sign at the primary trailhead at Miller Flat.

Our destination was the Spud Rock Spring campsite by way of the Turkey Creek Trail, located in the eastern side of the Rincon Mountains, in the Saguaro Wilderness Area of Saguaro National Park.  From the eastside of Tucson, it’s about a 2 hour drive east towards Benson, getting off Interstate 10 at Mescal. From there, you head north into the Coronado National Forest to the Happy Valley area on Forest Service road 35. If you don’t have a high clearance four wheel drive, you have to park at Miller Flat and walk an extra 1.5 miles or so up FS 4408; otherwise, you can proceed through a gate and park at the end of FS 4408 to start the hike.

A great place to car camp at Miller Flat in Happy Valley.
A great place to car camp at Miller Flat in Happy Valley.

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Heading up Forest Service road 4408 to the secondary trailhead. This road is suitable for high clearance 4WD vehicles only.

We left Tucson at 6:30 on Friday morning and arrived at the trail head in Happy Valley around 8:20 AM. Joe has a Jeep Liberty, so we were able to get the end of Forest Service  road 4408 to start our journey, rather than having to park down the ridge and hike another 1.5 miles in. The weather was great, though still chilly at this time of morning – 36 degrees and clear. We hit the trail at 8:45, quickly shedding a couple of layers as we warmed up from the sun and exertion.

Joe and Ryan amid tall grass on the Turkey Creek Trail about 1.5 miles from the secondary trailhead.
Joe and Ryan amid tall grass on the Turkey Creek Trail about 1.5 miles from the secondary trailhead.

For the first couple of miles, the trail climbs slowly through savanna grasslands and oaks. After that, it was a slog for pretty much the next 3 miles. It was like doing Blackett’s Ridge in Sabino Canyon twice. We stopped frequently to catch our breath, as well as to enjoy the view and take photos. At Mud Hole Spring, we ate lunch and took a half hour nap.

Mud Hole Spring.
Mud Hole Spring.

It was evident that this trail doesn’t get much use. It was overgrown almost all the way up, and in many spots, felled trees crossed our path. Near the end, about 3/8 mile from Spud Rock Spring, we spent about 20 minutes trying to follow the trail, due to overgrowth and debris on the trail. We finally arrived at the campsite at 5 PM. Of the three sites available, we made ours nearest the pit toilet and the bear box, which served double duty as a camp table. There was ample firewood about, but the no water at the spring, just a wet bog, surrounded by a large grove of aspen trees. Even if there had been a flow, the ranger had told Joe it was not good for drinking.

The ranger had also told Joe that we would be by ourselves on Friday night, but that the other two sites would be occupied on Saturday. We thought this odd, given it was November, it was the far side of the Rincons, and the threat of inclement weather loomed.

Ryan contemplate uses for aluminum foil by the camp fire.
Ryan contemplates uses for aluminum foil by the camp fire.

All of us had frozen meat with us (2 steaks and 2 chicken breasts) that had thawed out nicely during the day. We cooked these on small wire we had brought along, and supplemented these with baby carrots, dinner rolls, potatoes, and nuts.  Ryan had not brought any plateware. Rather, he had a roll of aluminum foil. He took a flat piece of rock, and covered it with foil, using this as his plate. After dinner we made hot chocolate while a roaring fire danced before us. Ryan did not have a cup. Using mine as a mold, he fashioned one out of foil. We called it a night around 7:30. The night time temperature was quite pleasant, with almost no wind during the night.

Aspen grove at Spud Rock Spring.
Aspen grove at Spud Rock Spring.

Saturday morning found us getting up around 7 AM. Quickly Ryan made a fire (he being 15, the fire was much larger than it needed to be, but boys will be boys) and we went about making coffee and breakfast. We spent most of the morning sitting around the fire, taking a nap mid morning, before getting our act together and heading over to Devil’s Bathtub to procure water. We missed the trail for the most direct route, taking a route that led us to a farther south meeting with the Heartbreak Ridge Trail, causing us to have to climb back up 500 feet, rather than staying fairly level.

At Devil’s Bathtub, we filled our bottles and bladders, ate lunch, and napped again in the warm rays of the sun on the gently sloping granite at the top of the falls. We didn’t go to the bottom of the falls, as we just didn’t want to do any more climbing than we had. After about an hour and a half, we made our back on the correct route to Spud Rock Spring.

Cool, clear water at Devil's Bathtub.
Cool, clear water at Devil’s Bathtub.

As evening approached, we prepared dinner and built another roaring fire. The temperature dropped, but it was still comfortable. Ryan threatened to make a jacket out of, you guessed it, aluminum foil. Joe and I convinced him that he would be better served by just climbing into his sleeping bag. The skies overhead were clear, with no wind whatsoever. We began to doubt any arrival of rain during the night. Too, no other campers appeared either, though around 8 PM both Joe and myself thought we heard voices in the distance, but we never saw any lights or smelled smoke from other fires. About that time, we called it a night.

The rain came at 1:45 AM on Sunday.

It drizzled most of the night. Joe and I stayed dry, but neither of us noticed that Ryan had not put a rain fly on his tent, so he got a bit wet. By the time we got up at 7, the rain had abated, allowing us to eat some breakfast bars and break camp without too much fuss. We made our way out at 8:25 AM.

To make your way in or out of Spud Rock Spring, you climb a small ridge. As we went over and down that ridge, we came across 5 women in 3 tents in the area of the poor trail marking/overgrowth/felled trees. These were the hikers that held the permits for the other 2 sites, and the ones we had heard the night before. They had fought their way up the Turkey Creek Trail the day before, only to be stymied by the poor trail conditions and impending nightfall. The apparent leader walked over to us, inquiring about our campsite and water, as they had run out and were in the process of collecting what they could off their tent rainflies. Then, as panic set manifest itself in her eyes, she said “Perhaps this wasn’t the best trail or time to bring a couple of newbies on.” I think some friendships were damaged that day.

Looking back up at the Spud Rock Spring area as we made our way down the trail.
Looking back up at the Spud Rock Spring area as we made our way down the trail.

We made our way down through almost constant drizzle in four hours, without slipping and breaking anything. It was actually a pleasant experience. Sunlight shone upon us for the last mile, allowing us to dry somewhat before getting into the Jeep.

Rain drizzles as we descend the trail into the lower foothills of the eastern Rincon Mountains near Miller Flat.
Rain drizzles as we descend the trail into the lower foothills of the eastern Rincon Mountains near Miller Flat.

We enjoyed a late and large lunch at Reb’s Café in Benson before heading back to Tucson.

QUESTION: Why is Spud Rock Spring not even close to to Spud Rock? They are not even on the same ridge.

GEAR NOTES: I had checked out my old Coleman Peak 1 gas stove (dating back to 1982) last May, and it worked fine. When I tested it out before this trip, it was evident that it had developed bad seals, because the flames were burning yellow, and I couldn’t get new parts in time to rebuild it for use on this trip. So I bought an Optimus Crux Lite canister stove and the Optimus Terra Solo Cook Set. A small canister sits inside the cook set, along with the stove, and the cook set comes with a mesh stuff bag that doubles as a scrub cloth. The stove worked perfectly, and the cook set was just right for what I needed (making hot drinks and boiling water for instant oatmeal, a pouch dinner, and clean-up).

My humble $39.99 tent.
My humble $39.99 tent.

I also needed to get some shelter at the last minute. An offer of a borrowed bivy did not come through, and I didn’t want to pack my Mountain Hardware Optic 3.5 up the mountain, so I ended up getting a $39.99 1 person tent at Big Five at 8:55 PM on Thursday night. It worked great. It’s actually pretty well made for the price, with a generously sized mesh side panel to get in and out of, mesh panels on the other sides, a rainfly, and a fitted footprint. It was vented well, and I didn’t get any condensation. Both the tent and rainfly have good zippers, reinforced tie-down points, and the weight is 3 pounds. The factory sealed seams did not leak in the rain. Not a bad deal for back up or light duty bivy. Branded “Golden Bear”, one of the Rec-Out brands (Rugged Exposure, Columbus).

Exploring Scotts Knob

Scotts Knob is little hill (marked elevation of 2915 feet) on the eastern side of Tucson, about 1 mile east of the end of Speedway Boulevard, just north of the Saguaro National Park boundary, apparently on the property of the Tanque Verde Ranch (a local guest ranch). Unlike a couple of other hills in the area, this one is named on topographical maps, with an indicated elevation. (NOTE: On the Forest Service topo map below, “Scots Knob” with one “t” is used, but on all other maps it is spelled with two t’s)

Capture

My buddy Rob and I checked it out this Labor Day morning.  Access is through a gate to the left of the TV Ranch sign; stay on any trail that goes right and hugs the boundary fence of the national park. You will eventually pass through a fence line that goes north/south – you will see the hill on your left. Proceed another 100 yards or so and another trail going north towards Scotts Knob will become apparent. Within a few minutes you will be on top of the summit. From the top you have nice views towards the Santa Catalina Mountains and Agua Caliente Hill to the north, and a great southwest sightline of the northwest face of Tanque Verde Ridge component of the Rincon Mountains.

Below are a few pictures from our exploration of Scotts Knob.

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Scotts Knob is the small hill in the foreground. Agua Caliente Hill is behind it with it’s summit to the right. In the far distance are the Santa Catalina Mountains. This view is from the Douglas Springs Trail in Saguaro National Park.

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One of the small washes we crossed on our way to Scotts Knob.

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My best guess is that this is a male Filigree Skimmer dragonfly.

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Benchmark on the summit of Scotts Knob.

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Looking southwest from Scotts Knob. The Rincon Mountains are to the left.

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