IT'S OFFICIAL
we're (finally) engaged. a type A idealist meets a part-time bohemian; a 19th century family diamond meets 21st century technology. with something old and something new already taken care of, there's just one thing left to do:
let's get married.
more to come.
posted by julie & tracy @ 4:12 PM
6 comments
6 Comments:
I never really thought of Tracy as a Type A Idealist until now... but now that I think about it, you nailed it, Jules.
Congratulations, to two such wonderful people for finding each other.
James
RIME consists of white or milky and opaque granular deposit of ice formed by the rapid freezing of supercooled water drops as they impinge upon an exposed object.
It is denser and harder than hoarfrost, but lighter, softer, and less transparent than glaze. Rime is composed essentially of discrete ice granules and has densities as low as 0.2–0.3 g cm−3. Glaze is generally continuous but with some air pockets and has much higher densities. Factors that favor rime formation are small drop size, slow accretion, a high degree of supercooling, and rapid dissipation of latent heat of fusion. The opposite effects favor glaze formation. Both rime and glaze occur when supercooled water drops strike an object at a temperature below freezing. Such formation on terrestrial objects constitutes an ice storm; on aircraft, it is called aircraft icing (where rime is known as rime ice). Either rime or glaze may form on snow crystals, droxtals, or other ice particles in the atmosphere. When such a deposit is wholly or chiefly of rime, snow pellets result; when most or all of the deposit is glaze, ordinary hail or ice pellets result. The alternating clear and opaque layers of some hailstones represent glaze and rime, deposited under varying conditions around the growing hailstone. See also hard rime, soft rime.
Let me get a close up of that ring. I want to see what a tension setting looks like.
Whoooooo Hoooooo! Best of it all to you two, Love above the rest!!! I'm thrilled for you both... Nice setting for the wedding as well! Mmmm, Mountains! You both are Awesome!!!!
(p.s. I just now saw the rhime ice entry, and rhime ice is beautiful, but I think this picture is not ice formed on a surface due to atmospheric moisture as rhime ice is, but rather from ground moisture (of course, atmospheric in origin) that has frozen, risen, and frozen... see comment under that section... explains it a bit further
Rhime ice looks like this: http://www.rcn27.dial.pipex.com/cloudsrus/frost.html
Much Love You Two !!! Camilla
Opps didn't show full address...
http://www.rcn27.dial.pipex.com/cloudsrus/frost.html#Rime
http://www.rcn27.dial.pipex.com
/cloudsrus/frost.html#Rime
Huh I had to put a space in there for you to see full address
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