We began the day by traveling south on the Iron Mountain Road. this route goes through part of Custer State Park, where we spent the rest of the day. As we traveled on this torturous hairpin turn road, the huge granite outcroppings, ledges and bolders made me think of Smugglers Notch in Vermont. The road twists and turns around mountains (Hills) which squeeze the traveler from both right and left. Th
Next we took the wildlife loop through the southern half of Custer State Park, where I saw my first wild buffalo (bison) herd. I saw them dotted over a far field, and then on the road in front of us. Shortly thereafter, I saw my first pronghorn antelope. Several times on the loop, we saw wild burros, which are not native to the region, but were released from a tourist trap that failed many years ago. This entire wildlife loop was composed of valleys and dry gullies. The land was not good for agriculture. It was dry and had a lot of stone in it and it was obvious that it had very little rainfall. What rainfall it did have came in heavy rain storms which washed through the gullies and into what I saw as dry streams. In fact, we had heard on TV that there was flooding in the Black Hills just a week prior to our arrival here. I saw evidence of this flooding in a number of the valleys in this park. Lots of tree branches, tree stumps with roots attached, and clay.
I need to take a little detour from the travel narrative here. When I was in the Southwest, I learned, discovered, and that the beauty of the landscape there was really due to massive erosion. Now that I'm in southwestern South Dakota, I can see that the beauty of the landscape here is also due to massive erosion. In the Badlands, you can see the results of years, millennia of erosion. You see the gullies, where the water erosion continues to this day. Here in the Black Hills, you can see much of the same problem. Only here, I think it is earlier in the progression. Major erosion has already taken place here in the Black Hills, but the result is to expose massive slabs of granite which underlies the soil in this area. In Custer State Park, I also saw eroded sandstone, which in some cases appeared to be attached to the granite, like it had been melted together. Today, we were riding north into Rapid City (the second largest city of South Dakota) to do a little shopping, and we started down a hill from a high flat prairie area and I saw in front of me red sandstone or just red soil showing on the grassy hillsides. I suddenly realized that this valley we were driving into was just as eroded as anything I've seen in Custer State Park or even in large parts of the Badlands. The only difference was
The last part of our trip was along Needles Highway. This was a great deal like the iron Mountain Road, but the switchbacks were sharper and there were a lot more of them. And we were going down steep hillsides with deep ravines alongside. Again, there were three tunnels, but no views of Mount Rushmore. We did stop after a tunnel to view the natural eye of the needle cut into the rock by erosion (see pic at right).
More pics here.
1 comment:
Excellent blog. They're actually called the Black Hills because ponderosa pine needles direct light downward, and so from a distance the hills appear to be black.
shawn
www.blackhillstravelblog.com
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