DayTrip
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- May 13, 2013
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This question is really curiosity more than anything and with so many well read people on this forum I assume somebody would know. Is there a technical term for the "ice" that forms when snow continuously freezes and thaws, forming that cloudy gray ice that really is much softer and more grippable than true ice? I've read in various books about terms like verglas, hoarfrost, etc, etc and I'm wondering if there is such a technical term for this melted monorail ice/compacted snow. Seems misleading in trip reports to call this type of snow ice when it is much easier to travel on than ice that obviously formed from layers of freezing water, which is grayer and much harder.
When submitting trip reports on NETC it only distinguishes between blue, black and breakable crust and the frozen granular of monorail isn't truly the same thing either. Something I've pondered this year with all the ice and wide types of ice out there this year. I always post overly detailed trip reports and using the correct term to distinguish the types of ice is something I'd like to be able to do for the more advanced hikers out there (I'm sure the tennis shoe wearing explorers have no use for such a term).
Anyone who might be "in the know" on these terms or can point me in the direction of a website, maybe an ice climbing site? Appreciate the info if you have.
When submitting trip reports on NETC it only distinguishes between blue, black and breakable crust and the frozen granular of monorail isn't truly the same thing either. Something I've pondered this year with all the ice and wide types of ice out there this year. I always post overly detailed trip reports and using the correct term to distinguish the types of ice is something I'd like to be able to do for the more advanced hikers out there (I'm sure the tennis shoe wearing explorers have no use for such a term).
Anyone who might be "in the know" on these terms or can point me in the direction of a website, maybe an ice climbing site? Appreciate the info if you have.