Glenn Herbert wrote:"Exposed bedrock" can mean many things depending on the type of rock. Some like shale might be fairly easy to quarry or pull up chunks, while others like granite would be totally impractical to modify without specialist tools and knowledge... and a whole lot of energy :)
Jay Angler wrote:
Eric Hanson wrote:... Strangely, the only time I ever remember it being audible was when the sky was overcast.
I don't think that's strange at all - clouds can reflect light. I suspect they can reflect sound to some degree also?
OK, a quick bit of research implied that it isn't actually the clouds, but different layers of air at different temperatures slowing, speeding or focusing the sound. The clouds tend to form at different levels and are definitely affected by temperature.
Do we have any physicists out there who could explain this better? Is it actually a thing that works? I recall from my son's music classes that low notes travel further than high notes (which is also why fog horns are the tone they are.)
Joao Winckler wrote:Been following Götsch's work for a while and it keeps showing up in unexpected places. The chopping and mulching in place idea sounds simple but trusting it takes time, especially when the plot looks a mess for a few months. Phil, curious what you've seen most improvement in, soil structure or water retention?
Syd Smith wrote:I think this will depend so much on other environmental factors that it would be hard to be universal about it. Tropical volcanic areas where soils form from rocks and ash quickly will be very distinct from arctic ones where soil formation is very slow. The styles of volcanism and volcanic products in a place like the Congo would be dramatically different from, say, Hawaiian or Icelandic volcanism.