photos: Hoh rainforest, 10-11 Sep 2005
Sep. 17th, 2005 08:55 pmPics:

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That blue Hoh River water -- I don't remember scattering mechanisms. Wikipedia says that glacial rock flour is "grains of a size between 0.002 to 0.00625 mm", 2000 - 6250 nm. I thought you needed to be smaller than the wavelengths of the light if you wanted preferential scattering of high frequencies. Help me out here?
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That blue Hoh River water -- I don't remember scattering mechanisms. Wikipedia says that glacial rock flour is "grains of a size between 0.002 to 0.00625 mm", 2000 - 6250 nm. I thought you needed to be smaller than the wavelengths of the light if you wanted preferential scattering of high frequencies. Help me out here?
no subject
Date: 2005-09-18 06:09 am (UTC)Might water suspension affect scattering? I speak from ignorance. I will aim laser friend this way, who might also speak from ignorance.
Does everyone take a picture of that spruce? It should charge five bucks a pop.
no subject
Date: 2005-09-19 04:25 am (UTC)no subject
Date: 2005-09-19 04:45 am (UTC)no subject
Date: 2005-09-18 03:51 pm (UTC)i think it was 270 feet tall, and about that old.
no subject
Date: 2005-09-20 07:31 am (UTC)Yeah, we took pictures of that tree a coupl'a weekends back, which is why I asked. :-)
no subject
Date: 2005-09-18 04:48 pm (UTC)no subject
Date: 2005-09-19 05:03 pm (UTC)If i were really bright i would use my presence at a physics lab specializing in water and arctic research to figure out the answer. I will see.
no subject
Date: 2005-09-20 02:42 pm (UTC)I am thinking the latter, since limestone quarries and glacial runoff are bright blueish-white much as the source rock is whiteish, while muddy rivers like my hometown Petitcodiac are, well, mud-coloured. But I don't really know, so I look forward to your discoveries.
no subject
Date: 2005-09-20 08:21 pm (UTC)no subject
Date: 2005-09-21 05:36 am (UTC)no subject
Date: 2005-09-21 05:39 am (UTC)"As the glacial mass of ice and embedded rock moves along the ground, it grinds the surface below and the rocks within it, creating a fine dust called "glacial flour." This flour makes glacial rivers look opaque and milky. The opaque water varies in color from chocolate brown to turquoise green, depending on the type and amount of sediment it contains. Streams that do not drain from glaciers are called clearwater streams to differentiate from those of glacial origin. Glacial streams can also run clear if the glacier is not melting, such as those seen during winter."
no subject
Date: 2005-09-21 06:57 am (UTC)no subject
Date: 2005-09-22 04:01 am (UTC)no subject
Date: 2005-09-23 04:51 am (UTC)