1.  How do I add my name to the mailing list?
You may call us at 509-762-5922, sign-up at the tasting room, or submit a request via our Contact Us page.  Please include your mailing address and whether you wish to receive newsletters and event notifications by mail or e-mail.

2.  How do I sign-up for the Wine Club?
Please see our Wine Club page and print out the wine club registration form provided by clicking on the "form" link.  Fill out entirely and mail to us at the address listed or call us and we will do your sign-up by phone (509 762-5922).

3.  I can't figure out how to place an order for your wine on-line.  Can you help?
We are happy to take orders by phone or you can use our Contact Us form to make your request.  If you e-mail us, we will contact you by phone to arrange payment and delivery. 

4.  Can I buy your wine in local stores or wine shops?
Our wine is currently available for purchase in our Moses Lake tasting room and at the following locations:

5. Where can I find past issues of the "Traveling Cork" Wine Club newsletter? 
Click here for archived issues:

	Fall 2008 Newsletter Page 1   ~   Page 2
	January 2009 Newsletter
	Spring 2009 Newsletter Page 1  ~  Page 2

 

6.  How did you come up with the name "Dry Falls Cellars"?
    Two of our owners are Moses Lake natives and have a keen interest in the awesome geological events that preceded the formation of the actual Dry Falls landmark to the north of Moses Lake.  In keeping with our true regional roots, we opted for a local name and we enjoy sharing the history of Dry Falls with our customers:
    In Central Washington, on the opposite side of the Grand Coulee from the Columbia River, resides a three and a half mile crescent-shaped precipice known as Dry Falls.  Twenty times the size of Niagara Falls, Dry Falls is thought to be the greatest known waterfall that ever existed.  Geologists speculate that during the last ice age catastrophic flooding channeled water at 65 miles per hour through the Grand Coulee and over this 400-foot rock face.  At this time, it is estimated that the flow of the falls was ten times greater than the current flow of all the rivers in the world combined.
Nearly twenty thousand years ago, as glaciers moved south, one ice sheet plugged the Clark Fork of the Columbia River, which kept water from being drained from Montana.  Consequently a significant portion of western Montana flooded forming the gigantic Lake Missoula.  Eventually, enough pressure accumulated on the ice dam that it gave way.  It is generally accepted that this process of ice-damming of the Clark Fork, refilling of Lake Missoula and subsequent cataclysmic flooding happened dozens of times over the years of the last Ice Age.
   This sudden release put parts of Idaho, Washington, and Oregon under hundreds of feet of water in just a few days.  These floods, which some consider to be among the most extraordinary known, created the Grand Coulee and Dry Falls in a short period.  Similar glacial flooding, though not as impressive as the aforementioned, kept the falls flowing for several thousand years.  Once the ice sheets that obstructed the Columbia melted, the river returned to its normal course leaving Grand Coulee and the falls desiccated.

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