(I've finally had some time to work on my image backlog. this is another from the summer... looking across the valley and up towards black bear pass... shot while on the way up Red Mnt 3. south of Ouray, Co.)
Beautiful, you're beautiful, as beautiful as the sun. Wonderful, you're wonderful, as wonderful as they come. And I can't help but feel attached To the feelings I can't even match. With my face pressed up to the glass, wanting you.
Beautiful, you're beautiful, as beautiful as the sky...
Can't you hear that rooster crowing ? Rabbit running down across the road Underneath the bridge where the water flows through So happy just to see you smile Underneath the sky of blue On this new morning, new morning On this new morning with you.
Can't you hear that motor turning Automobile coming into style Coming down the road for a country mile or two ? So happy just to see you smile Underneath the sky of blue On this new morning, new morning On this new morning with you...
you look all around you and the entire world stretches out forever but seems as if it is still just right at your finger tips. a glance transports you and your thoughts over the horizon. One is never more completely removed from, yet a part of the world..... of course it could just be the oxygen deprivation.
Colorado... a Spanish word for Red, It's kind of easy to see how this was decided upon as a place name. this is near sunset, looking down on Red Mnts. #1 & #2 as seen from the summit of, the rather imaginatively named, Red Mnt. #3. the road (I use the term loosely) you see is Corkscrew Pass, the first pass of the morning.
"The stunning red, maroon, orange, and yellow colors of the Red Mountains are primarily due to past hydrothermal alteration of these rocks. Hydrothermal alteration is literally the process of "hot water" circulation through the strata that changes the mineral composition of the original rocks. Hydrothermal fluids commonly contain significant concentrations of metals and sulfur. Hydrothermally altered rocks can contain significant amounts of disseminated sulfide minerals, primarily pyrite (iron sulfide). This process happened within and surrounding the Silverton caldera. Subsequent erosion of the strata exposes the pyrite to oxidation, and as the iron combines with oxygen it turns the rock various colors evident in the Red Mountains. "