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Yosemite Nature Notes - 10 - Rock Fall

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[Music]
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This is actually a really interesting viewpoint
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to view the runout zones for rockfalls from Glacier Point.
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Usually we're looking either across the Valley
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over at Glacier Point,
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or we're down at the bottom looking up,
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and those are valuable views as well,
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but this is really useful to be able to be up here
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and look down.
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And from right here I can see runout zones
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for about five different rockfall events
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that have occurred in the past decade or so.
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The cliffs are eroding very slowly, grain by grain,
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all the time, but when suddenly a piece of the cliff
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that's 200 feet wide and 100 feet tall
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and 20 feet thick just falls off the cliff
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and falls 1,000 feet to the Valley floor
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and breaks up in all these pieces,
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you know, that's a really different style of erosion.
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When we look around Yosemite Valley,
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we see abundant evidence that rockfalls have been occurring
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here for thousands of years.
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Yosemite Valley is a glacially carved canyon,
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and since glaciers retreated about 15,000 years ago,
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rockfall has been the major force
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shaping this landscape.
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We don't always know what causes a rockfall
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in a particular event.
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Sometimes it's obvious in that
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there might have been a large rainstorm or snowstorm
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that then caused a lot of seepage and so we surmised that,
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that seepage must have caused the rockfall.
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It's not always the case, sometimes
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rockfalls happen without any known trigger,
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so it could just happen on a nice bright summer, sunny day.
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We had decided to rent bikes to ride around the Valley,
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we were only here about an hour and
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heard this loud thunderous roar and
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couldn't tell where the sound was coming from.
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And looked around and I saw a rock falling off the wall
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over to my right.
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Whoa, a rockfall, look!
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I had to get my camera off the bike as quickly as I could,
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that's why the footage is a little shaky.
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I had to take the wide angle lens off of it
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and was lucky enough to catch the third rockfall.
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Look at that piece!
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In the particular rockfall that was captured on video,
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you can see a rock slab detaching from the cliff face,
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sort of skipping down the cliff face,
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