While the average annual number of rainy days on the central coast is not particularly notable, the terrain on Big Sur is capable of immense orographic enhancement and staggering rainfall totals when Pacific moisture and jet stream energy align with the terrain. Rises steeply from the ocean to its 5,164 ft summit, Cone Peak is particularly adept at squeezing out the moisture from clouds and when combined with its rugged and extremely steep topography you get some impressive waterfalls on the mountain’s flanks. Two such waterfalls are Vicente Falls and Limekiln Falls.
Limkiln Falls is a relatively accessible 90 ft drop at the bottom of Middle Fork Limekiln Creek. The short hike to reach the falls from the Limekiln State Park day use and camping area passes through an attractive redwood grove with a carpet of redwood sorrel and pretty cascades along Limekiln Creek. After taking the main trail along Limekiln Creek, turn right at a junction and head up the Middle Fork Limekiln Canyon to the falls, crossing the creek four times along the way. These crossings are usually dry but will be wet in higher flow with no bridges in place. The main drop is measured at 90 ft and that is all that is visible from below, but there are additional drops upstream. The falls has two distinct prongs separated by a massive mineral apron. The prongs spreading outward from the top are reminiscent of the tusks of a mammoth. In the very highest flows, this apron is entirely covered in water, but the general character of the falls is the two prongs with moss and vegetation growing on the mineral accumulation in between. Due to high visitation, vegetation at the base of the falls has been largely trampled to dirt. The falls only features a small, shallow plunge pool.
When in flow, Vicente Falls is a very pretty falls spanning 190 ft from top to bottom. The falls drains the region immediately below the southeast face of Cone Peak, which is the drier, hotter side of the mountain. Thus, appreciable flow is not the norm for this falls (especially in the last few years of drought) and the falls is light at best or more accurately a drip most of the year. However, after a heavy rain, the falls transforms into a beautiful cataract over the immense cliffs tumbling over at least four distinct drops into the redwood forest. From below, the uppermost drops are not visible, but around 120 vertical feet of the falls is visible. Similar to Limekiln Falls, the plunge pool at the base of Vicente Falls is shallow and small. Vicente Falls is located upstream of Vicente Flat in a side canyon of the main Hare Canyon. The trek up to the falls includes some photogenic cascades and small pools in a narrow canyon along with some poison oak and blowdown debris. It is interesting to note that for most of the year the main stem of Hare Canyon has higher flow but after heavy rain the side canyon containing Vicente Falls greatly exceeds the main stem. This is indicative of some large springs in the canyon along the main stem while the Vicente Falls side canyon is largely runoff based flow. Visiting Limekiln Falls, Vicente Falls, or both gives an excuse to spend some time on lovely Cone Peak, one of the centerpiece features of Big Sur with amazing vistas and scenery, some of which I’ve highlighted here. For additional waterfalls in Big Sur, see the Waterfall Project.