We have a cast aluminum patio table that has concentric rings of daisy petal cutouts. They’re large enough that the snow can fall through the holes but far enough apart that snow can build up between the petals. The result is this extra-terrestrial formation we found outside our window this morning. Notice too the mirror image that formed on the deck. It must have been a very calm night.
The next morning we awoke to this new feature – snow drapes.
Right here in Oroville, folks. An ukulele club formed this past year and after much practice they had a playing at the North Valley Nursing home in Tonasket. Familiar faces are already members and they’re seeking new members. More information can be found at their Facebook page.
The Ookoolele players will be playing at Esther Bricques Winery on December 18. This will be a caroling sing-along and all are encouraged to bring instruments and to play and sing along or just show up. Personally I would love to see everyone show up in an ugly Christmas sweater! How much fun would that be?
Quality instruments are available locally in Omak so you have no excuses! Omak Music not only has instruments, they have their own ukulele club so driving distance shouldn’t be a problem. No more excuses!!
If you would like a very nice custom ukulele made by a local luthier you might give Oroville’s Mark Kubiak a visit. His instruments are beautiful to see and play, and he’s begun work on ukuleles.
Click the pic and have a quick read about ukulele history at Wikipedia.
Probably not what you thought…This is a story about rocks, where they are, and how they got there. This last part first: How they got there. The Okanogan River valley geography is inseparable from the effects of the great ice sheets that covered this region up to the beginning of the Holocene epoch. It is hard to imagine glaciers a mile high covering the Okanogan Highlands, the city of Oroville, all of the Okanogan River valley, and in fact all of northern Washington State. The Cordilleran Ice Sheet buried everything from the Pacific Ocean to what is now Montana and north as far as Alaska. The Okanogan lobe of that ice sheet is what provided so much beauty in our region.
The ice sheets were very active, continually though slowly sliding and grinding south for many thousands of years, ending their travels only when the southern most climate calved and melted them back as fast as they traveled. Carried effortlessly along with that ice were untold tons of rocks and boulders, some larger than houses. Some of these travelers came from places very far to the north, in fact. Some were carried to the glacial terminus while others were simply dropped in place as the glaciers retreated. They’re still here and we recognize them because they look absolutely out of place. And they are. They are known as erratics.
This article is about my quest to find as many of these notable and interesting erratics as I can and present them photographically, along with the approximate location. As such this article will be updated as I stumble onto these lurking travelers. As the mood strikes I will provide some interesting science associated with the North Okanogan, Washington State, and the stunning effects of the Great Missoula Floods.
I’ll kick things off with this beautiful image of the Waterville Plateau because there is a story to tell about this place and why it is special. From Wikipedia:
How cool is that? Now I have a story to tell you so I’m going to need a few days to spin it. Watch for Part 2