One of the great places to visit of our area, Black Lassic. The great thing about this peak (5,900′), is that it is very easy to get right up on top. A road essentially crosses a broad saddle where Black Lassic connects with Red Lassic and Signal Peak. There is a turn off where you can park then walk a relatively gentle trail and be on top in 15-20 minutes. If there is snow, you might not be able to get as close so be prepared to hike for a few hours depending on how close you can get. The mountain is always in plain view so its not hard to know where to go, just make sure you get to the uphill side of Lassic before you try to get to the top. All the other sides of the mountain get extremely steep and most of it is fractured and unstable.
The Lassics are considered a unique geologic area where different pieces of ancient history collide. This grey and red soil is called ‘serpentine’ and is highly acidic, and even has naturally occurring asbestos within in it. While allot of this land can be barren, stands of incense cedar and pines can grow on serpentine. Where more developed soils occur, stands true fir stands develop.
I decided to scramble up to Red Lassic first. While this is not a hard hike, there is no trail so don’t try to take small kids or bad legs up here.
At first glance it looks like a simple enough walk, but you must cross these talus slopes and that can be hard on your knees. My knees seem to feel it more and more each year, but I have always enjoyed scrambling over this kind of terrain.
Eventually you get to relatively stable rock and can take in some fantastic views.
The highest point in this picture is called Signal Peak. I think there used to be a fire lookout here. When you visit this place, you can easily get to the top of all three of the peaks, Black Lassic, Red Lassic, and Signal Peak in a single day.
A nice view of Mad River Rock. That is on my radar for my next adventure. I have always wanted to explore it! Someday Ill find the time.
And of course a great view of Black Lassic from the top of Red.
Looking back at Red Lassic, it does not look that impressive, although shooting a picture into the sun never really works…
Making my way up Black Lassic, you can really see the black color of the rocks and soil, which is indeed in contrast to the red hue of Red Lassic.
And finally, the truly epic view. Mad River Rock again. Its the Van Duzen River between us and the Rock. The next ridge you see is ‘South Fork Mountain’ which drains the Mad River. I do not know what to call the next ridge line, however I know that the east side of South Fork drains into the South Fork Trinity River. I have some panoramas Ill be posting next taken from these peaks.
Here is one of those magical nooks and crannies I love to find. No relation to the ‘real’ hidden springs, if one exists. However if you were not right on top of this one you might not find it. This unique spot has a fairly large Douglas-fir whoes roots create a Tolkienesque’ cave from which a mountain spring emerges. This ends up being one of the headwaters of Deer Creek in the Mad River.
Obsidian flake from a archaeological site above the Mad River near Pilot Ridge. A flake is a piece of rock or obsidian that ‘flakes’ off from a larger piece during the manufacture of stone tools. Think spearheads, arrowheads, an knifes. You also produce flakes when sharpening your stone tool. While chert flakes are very common in Humboldt County, I do not come across obsidian very often. It had to travel a long way to get up into the Mad River. The aboriginal people of California traded extensively and that could be how this ended up here. I think the nearest obsidian sources from here are in Lake County. You can date a site if you find a few points, as the type of arrow or spearhead technology is diagnostic of time periods of human habitation, some going back as far as 8,000 years. Its becoming increasingly rare to find a point at a site however, mainly due to a century of people picking up arrowheads.
This ancient hulk of a black* oak tree appears unstoppable. As parts of it die, new growth emerges. In this way, trees that produce sprouts can persist indefinitely, until site conditions change. Who knows how old this tree is. Technically, white oaks are thought to have a life span of up to 300 or so years. But I always have wondered if that takes into account new growth that eventually replaces the dying stem. Could some of these trees be thousands of years old? Regardless, trees like this contribute to the biodiversity of the landscape and have practically all flavors of the food web…
*I first thought this was a white oak, but a fellow forester pointed out that it is really a black oak. Thanks!