Hiking

Arroyo Tapiado Mud Caves

Arroyo Tapiado Mud Caves

If you’re a Southern California resident, and you’re looking for a challenge that is a little more exciting than Potato Chip Rock (a/k/a Mount Woodson), the adventure you’re looking for is the Arroyo Tapiado Mud Caves. Since I covered this area in detail back in 2011 here, I’m not going to go into excruciating detail today, because you can read the details here. The caves are located approximately two hours outside of San Diego, and are perhaps the largest network of mud caves in the world, comprising some twenty to thirty caves.

Directions: If you are coming from San Diego, take the I-8 east to the town of Ocotillo, California. Exit the freeway, and turn onto the S-2 hearing North (Left). Follow the S-2 past the brand sparkling new wind turbines, through the border checkpoint, and into Anza-Borrego State Park. Once you are in the State Park, you will want to look for Mile Marker 43, which is also marked as the “Palm Spring” turnout (no, it is not the turnout for the town, it is the turnout for the actual Palm Spring from the Butterfield Stage Line). From this point on you will be “off-roading”.

Winter Hiking - it's not really about the gear.

Winter Hiking - it's not really about the gear.

Don’t go any further, you’ll die. Today’s quiz, hotshots, is what you would do if you heard this phrase on the trail. Would you turn around, or would you keep going? It’s also a statement that’s led me to pen this mini-diatribe. Before I go any further, I can already hear you asking, “Wait – what’s the situation? The terrain? The temperature? I can’t answer this question until I know these things.” Fair enough, let me give you the relevant background details: it was a partly cloudy day in Zion National Park. The cloud deck was resting at around 7,000 feet, and the ambient temperature at the Weeping Rock Trailhead (Information here) was around 20 degrees, although it could have been slightly colder as there were intermittent wind gusts of around 10 mph. For the last two days it had been snowing down to approximately 4,500 feet, but at the lower elevations there had been some melting and re-freezing. These were the conditions I found when I arrived at the trailhead one Sunday in mid-December of 2012 at around 7:30 a.m.

Old Pinnacles Trail to Balconies Cave

Old Pinnacles Trail to Balconies Cave

 At Pinnacles, the two main areas for spelunking are Bear Gulch, which I talked about in December, and the Balconies network of caves, which I’ll talk about today. All of the caves in Pinnacles are talus caves, which are formed over a period of time when rocks have fallen atop other rocks at the base of a cliff. In particular though, the caves at Pinnacles formed in the following manner: “…when steep, narrow canyons filled with a jumbled mass of boulders from the cliffs above. The canyons are the result of faults and fractures in the central area of volcanic rock. These shear fractures filled with gigantic toppled boulders are clear windows into the geologic wonder of the Monument.” (More information on the geology of Pinnacles here and here).  In any case, both the Balconies cave and the Bear Gulch cave network provide a great spot to explore over 50 million years of geologic history over the course of a morning or afternoon.

A Devils Punchbowl but not "The" Devils Punchbowl

A Devils Punchbowl but not "The" Devils Punchbowl

Today I’d like to talk about the myth and legend of the “Devils Punchbowl” in San Diego County. If you’ve like me, and you’ve lived in San Diego, or spent enough time in San Diego, and you’re interested in the backcountry, chances are you’ve heard of “The Devils Punchbowl” after you heard about Cowles MountainIron Mountain, and Woodson Mountain (a/k/a “Potato Chip Rock”). Here’s the interesting thing though: unlike the above peaks, “The Devils Punchbowl” is a more nebulous concept. There’s no doubt that it exists – it’s definitely a location that exists. But, it exists in about ten or eleven different locations, depending on who you are talking to, and who is giving you directions to the “actual” site.

Current Conditions, Deer Springs Trail/San Jacinto, December 30, 2012

Current Conditions, Deer Springs Trail/San Jacinto, December 30, 2012

There’s a number of ways to celebrate the end of the year. For some, it’s all about wearing green underwear, eating twelve nuts, twelve grapes, and packing a bag to leave at home. For others, it’s the typical night out extravaganza in around the world style, followed up by watching bowl games for the entirety of the first day of the year in a near comatose state. For me, I like to try and get out at least once at the end of December. It helps me feel like I haven’t become the blob after eating oodles of home-made Peppermint Bark and other delicacies throughout the Thanksgiving to New Year’s Eve period. Getting out at the end of the year is tricky – sometimes it feels like the only place you get to is the mall; but, I always find it worthwhile because it allows me to recharge my batteries, appreciate the beauty of winter, reflect on the year past, and set goals for the coming year.

Bear Gulch Cave Trail

Bear Gulch Cave Trail

Let’s say you’re in California, or thinking about visiting California, and you’re looking for a National Park that you can hike in, camp at, climb at, and possibly do a little spelunking at. If you were seeking recommendations for such a place, chances are that you’d get the usual recommendations – Sequoia National ParkYosemite National Park, or even Joshua Tree National Park. There’s nothing wrong with any of these recommendations – these parks are known world-wide because they’re stunning. But there’s another National Park in California that’s a little bit off the beaten path, and not as well known that has all of these things, and is equally stunning in its own right. That park is none other than Pinnacles National Monument.

Rainbow Falls

Rainbow Falls

I recently made it out to the Devils Postpile, and here’s what I have to report: it is indeed something you need to see. My former boss was right: this is an area that is remote and lesser known than its bigger cousin, Yosemite. I say “lesser known” because I am well aware that it is directly outside of Mammoth. This is not something that should dissuade you from visiting: even though it is directly outside of Mammoth, it is still tucked away in its own corner of the Eastern Sierra. Also, in this case, being tucked away next to Mammoth is a good thing: there are well signed parking areas for the park from which you will take a shuttle into the park during the summer months. While Devils Postpile is named for the amazing geologic feature of the park – the columnar basalt “piles” that formed over one hundred thousand years ago from cooling lava, and the basalt is amazing to see, I think the best day hike in the park is the hike to Rainbow Falls.