In an effort to get a handle on some land forms, I set the approximately 350 meter contour and below as blue. The elevation is the approximate height of the highest overflow path at Wallula Gap, the narrow point in the above digital elevation map where the Columbia River cuts through the Horse Heaven Hills. The contour approximates shores of Lake Lewis, the temporary lake that backed up behind the narrow gap during the ice age floods. The pool of blue down stream of the gap would not have filled that deep with flood water; however, the water did back up in that area as well due to the constriction in the Columbia River Gorger further down stream off the map.
The water pooled to the east as well inundating the Walla Walla valley.
The back up from Wallula Gap extended far up stream. This image is the Columbia River at Wenatchee with water backed up the Wenatchee River into the Cascades. The blue area extending across the lower right is Moses Coulee, one of the numerous flood route paths.
Wallula Gap with highest flood overflow channel marked with blue on the left upon which the lake level projection is based.
Islands formed for brief periods along the fist anticlinal ridge south and west of Kennewick
Snipes Mountain a ridge within the Yakima Valley west of Sunnyside and east of Granger stuck up above the water in this scenario.
The water backed up the Yakima River including through Union Gap forming a pool in what is now Yakima and perhaps a small pool north of Selah Gap. The flood matches fairly well the inundation in the Yakima area.
The water pooled to the east as well inundating the Walla Walla valley.
Water also backed up the Snake River canyon all the way into Idaho on the east of the above map. Keep in mind water from Lake Missoula was likely still poring into the lake from the north. The river north of the Snake is the Palouse and its old channel, now Washtucna Coulee. That sharp canal-like line connecting the Palouse to the Snake is the current route of the Palouse as it follows a joint carved by the flood (the-palouse-river-leaves-its-valley). The back of water portrayed in the image is matched by thick silt units that fill the valley of the lower Tucannon River, a tributary that flows into the Snake from the south.
Have you ever field checked any of the drainages to see if there is "shoreline" evidence on the ground. Did you project your DEM model up the Grande Ronde?
ReplyDeleteI have done some field checking. Two of the islands south of Kennewick i looked for ice berg carried erratics and found a few. Others have done the same. I also had a project in Yakima that based on my DEM would have been under the water, but no silts related to the flood waters were present; however, that could be due to post depsoition erosion and/or minimal deposition.
ReplyDeleteIf you click on the first map, you might be able to see that the water did back up into the lower end of the Grande Ronde. Another ice-age flood also came down the Snake when ice age lake in northern Utah over topped the basin. A big flood but not near the scale as the Missoula Floods.