On 6 July 2008 we paddled the canoe down Gee Creek to the Columbia River. The Creek itself is a winding, meandering stream, and at this time of year it’s about 30-40 feet wide, and is strewn with fallen trees, making navigation a bit tricky. Arriving at the Columbia river came as a surprise since it’s hidden from view by trees, and it’s not until Gee Creek takes a final sharp turn to the left that the mighty Columbia springs into view. Here the river is over half a mile wide. It was hard to resist the temptation to paddle out into the Columbia if only for 100 feet or so, and, needless to say, we couldn’t resist the temptation.
One of the first things we noticed was the waves flowing into the mouth of Gee Creek, as though we were in the wake of ship that was passing by. But there was no ship passing by. This was a natural wake created by the river. The waves were about 5 to 6 inches high, and they continuously rolled toward us one after another. Five to six inch high waves might not sound like much, but we were three men tightly stuffed into a 14 foot canoe with our supplies and gear, and our excitement at paddling out of the mouth of the creek turned dead serious when we realized that the rules for navigating Gee Creek did not apply here. I recall Cameron saying “I think we should turn around. These kind of waves can easily capsize a canoe like this.” And turn around we did, and we quickly paddled back inside the safe harbor of Gee Creek. [click image to enlarge].
The mighty Columbia comes into view
Having looked at various maps, and having read some things about Gee Creek, I came to wonder if Gee Creek had always emptied into the Columbia River at the same place where we had encountered the waves. I found a reference to survey notes of the General Land Office based on a U.S. Geological Survey of 1853 stating that Gee Creek enters into the Lewis River. The Lewis River does meet up with the Columbia just north of the mouth of Gee Creek. In fact, the Lewis River is so close to Gee Creek that if the creek were to continue in a northerly direction for about 500 feet, then instead of emptying into the Columbia it would empty into the Lewis River.
Now my curiosity is such that I’d like to visit the mouth of Gee Creek again to see whether the elevation around the area is low enough that Gee Creek once could have entered into the Lewis River.
Consider the satellite image below. Route C is the present mouth of Gee Creek where it enters into the Columbia. Route A could be the remains of an old creek bed where Gee Creek would have emptied into the Lewis River. And Route B is perhaps another dry bed where Gee Creek once took a winding bend before spilling back into the Columbia. It may be that Gee Creek once followed Route A, but because of sediment from the Lewis river that route became blocked. Then perhaps Route B became the way for Gee Creek to evacuate its water. And perhaps over time, erosion forced Gee Creek to break through at Route C, which is clearly the most economical route for the river to take. [click image to enlarge].

It may also be that in times of high flooding Gee Creek empties through all three of these routes at once. I was led to this view by examining the map below where a small island appears that is not in the satellite image. This small island is what remains after Gee Creek empties at all three routes at once. [click image to enlarge].

I’m not sure what to make of this map since I’ve noticed an anomaly that I can’t explain. The map shows a small island just southeast of Blackwater Island, but we discovered no such island when we paddled there recently. There could be an island that is now under water due to the high water levels around Blackwater Lake. If this island exists it would only appear when water levels are low. However, the map also has an island at the mouth of Gee Creek that would only appear when the water levels are high. It wouldn’t make sense for the water level to be low in Blackwater Lake but high at the mouth of Gee Creek since these water bodies are connected. It may be that the data for the map was collected over a period of time, so that the data for Blackwater Lake was taken when water levels were low, and the data for the mouth of Gee Creek was taken when levels were high. The data for this map was plotted 15 June 2006, and the following disclaimer on the map itself might explain a lot:
Note: Information shown on this map was collected from several sources. Clark County accepts no responsibility for any inaccuracies that may be present.
Well, I guess this means that we’ll just have to return to the mouth of Gee Creek to do some thorough exploring in order to discover what no map or satellite image can reveal.
--Chuck Sullivan