GETTING THERE. One way to drive to HELLHOLE CANYON PERSERVE is from ROUTE 15. You exit at VIA RANCHO PARKWAY, and to travel to the east. GOOGLE map states that the name of Via Rancho Parkway is Bear Valley Parkway. But this is garbled and wrong. The correct name is Via Rancho Parkway. After a couple of blocks, Via Rancho Parkway makes a sharp bend, and turns north, and at this bend the street changes its name to BEAR VALLEY PARKWAY. Then, Bear Valley Parkway changes its name to VALLEY CENTER ROAD. Once on Valley Center Road, you turn right (to the east) on LAKE WHOLFORD ROAD. From then on, your drive will be on narrow streets that wind around a mountain side and then, after that, narrow streets that pass neighborhoods in farming areas. Eventually, Lake Wholford Road changes its name to PARADISE MOUNTAIN ROAD. GOOGLE map states that the name is Woods Valley Road, but this is not correct. The correct situation is that they are one and the same road. To the east of Lake Wholford Rd., the name is Woods Valley Rd., and to the west of Lake Wholford Rd., the name is Paradise Mtn. Rd. Fortunately, along my way I encountered two or three little signs by the road that said, "Hellhole Canyon Preserve" is this way.
MANY FLOWERS. FEW PEOPLE. There is no fee. The trailhead is inviting enough, and on the hike down into a canyon, you encounter signs that identify a nearby plant. One by one by one, you will encounter signs that read: (1) Lemonade Berry Sugar Bush; (2) Chamise; (3) Hoary leaf lilac; (4) Black sage; and then there is a large 3 ft. x 4 ft. plaque that explains the "2003 Paradise Fire," and finally (5) California buckwheat. At this time of year (May), most parts of the trail during my two hour hike were bordered by flowers. Mostly, yellow flowers. Typically, the stems of these flowers arched over the trail, and many were at shoulder height (providing that you are about 5 and 1/2 feet tall). Black sage resembles another plant, namely, fiddledock. Despite its name, Black sage has many blossoms that are colored light violet. There are many Hesperoyucca whipplei. At certain times of the year, this type of yucca sprouts fruits that are dark green and that look exactly like tiny bell peppers. Most of the yucca that I saw had a brightly colored collection of blossoms.During my entire walk, I encountered three couples (man plus woman). Two of the couples had a dog. One of the women was an engineering student at U.C. Irvine. One of the men was a fireman.
ANIMALS ON OR NEAR THE TRAIL. During the entire hike, I encountered several lizards. One was sitting on a granite boulder by the trail, and the others were crossing the trail. I encountered one black beetle, perhaps a "stinkbug," crossing the trail. I encountered one snake. Mister Snake was very small, and it was crawling across the trail and into the bushes. At two points in the trail, I heard a bird call that went like this: EEK-EEK-EEK-jih-jih-jih-jih-jih-jih-jih-jih-jih-jih-jih-ghghghghgh. The last part of this bird call (ghghghghgh) was a sound that faded out. At a couple of points in my hike, I heard a dove cooing. To reduce the chance of an encounter with mountain lions, I carried a fully extended seven foot long silver-colored aluminum tripod (15 pounds). My theory was that mountain lions would confuse me for being a radio tower, and then leave me alone.
ROCKS. There are many huge granite boulders. Most amazing are the granite boulders that have exposed veins of white quartz. Two of these veins can be seen on the main trail, where they occur in between the lower terminus of the HORSE THIEF TRAIL and the upper terminus of the HORSE THIEF TRAIL. I did not have my camera along, and so I am here posting photographs of white quartz veins in the granite at JOSHUA TREE NATIONAL PARK. The National Park Service describes the quartz veins as follows: "Visitors also wonder about the "broken terrace walls" laced throughout the boulders. These are naturally occurring formations called dikes. Younger than the surrounding monzogranite, dikes were formed when molten rock was pushed into existing joint fractures. Light-colored aplite, pegmatite, and andesite dikes formed as a mixture of quartz and potassium minerals cooled in these tight spaces. Suggesting the work of a stonemason, they broke into uniform blocks when they were exposed to the surface."
My entire hike was 5.2 miles, as measured by the hiking map. I took HISTORIC FLUME TRAIL, which brings you past the flower signs (and the flowers) and to the bottom of a canyon where there is flowing water. Charred trees occur here and there. Some of the charred trees are totally dead, while others have recovered from the fire and are covered with newly grown small branches and leaves. Then, this same trail changes its name to CANYON VIEW TRAIL. RODRIGUEZ PEAK TRAIL is very much overgrown with weeds, and so I did not take it (I didn't want to get lost). read more