Gravel Tongue Draped into The Snake River Canyon

I was going through some pictures of the Snake River canyon through the southeastern Washington Palouse. The four dams on the lower Snake have been the subject of ongoing legal wrangling and policy debate. One big issue that may be under appreciated by some is the transport infrastructure and economy of the dry land wheat on the high plains above the canyon. I have previously touched on the subject of the Snake River and wheat transport (getting-wheat-to-river and mayview-tram-snake-river). There is no getting around the damage these dams as well as the dams in Hells Canyon have done to salmon populations. There is also no getting around how important the dams are for wheat transport. There is no good solution, or if there is, it will be costly. Indeed the existing circumstance has been costly.

The above said, I was looking at a picture of a grain loading facility on the south side of the Snake River just a bit upstream of the confluence with the Palouse River.  

Tongue of gravel descending slope across the Snake River from the grain facility

The facility is located on huge ice age flood bar that formed when the largest flood spilled across the Palouse from Spokane, completely filled the Palouse River valley and spilled out of the Palouse and into the Snake, permanently altering the course of the Palouse River (palouse-falls), and flooded into the Snake River canyon at this location. The flood completely filled the Snake River Canyon and due to the restriction at Wallula Gap water backed up the Snake all the way to Idaho (ice-age-floods-dem-and-lake-lewis).

The tongue of gravel on the slope shown above was from one of the spill over routes of flood water into the Snake River Canyon. It is the easternmost of the spill routes from the ice age flood. The togue of gravel descending down the slope is a rather unique feature. Lidar imagery of the canyon captures this feature rather well.

One more example of the need to reorient one's thinking when in ares impacted by the ice age floods. 

Summit of Guemes Mountain

Guemes Mountain is on Geumes Island. Guemes is one of the San Juan Islands, but is in Skagit County. It is a very short ferry ride across Guemes Channel from Anacortes on a Skagit County ferry. 

Nothing to do with the mountain but this layer of organic rich muck pulled up by blown over trees along Eden Road was a pretty cool site.   

The trail up the mountain is a moderate climb on a well established trail through a mixed forest stand.

The summit provides nearly 360 degree views:

The view of Anacortes is a reminder that despite the ferry ride and hike, the big city is not far away 

View west along Eden Road with Cypress Island in the distance. 

Cypress is another San Juan Island that is in Skagit County. Most of Cypress is owned by the State of Washington and is managed as a Natural Resource Conservation Area. No ferry service to Cypress.

Jack Island with Lummi Island in the distant right

Jack Island is managed as a natural area by the San Juan Preservation Trust (https://sjpt.org/preserves-easements/jack-island/). It is a rather well hidden island as Guemes blocks the view from Anacortes and the small island blends into the background of other more distant islands when viewed from other angles.

Eliza Island

Eliza is in Whatcom County in the southern part of Bellingham Bay.

Samish Island.

Samish Island is another Skagit County Island. The island is connected to the mainland due to the presence of dikes that hold tidal water out of a quarter mile neck of former tideland. Hence, no ferry is needed to get to Samish. 

The summit of Guemes is underlain by intrusive rocks of the Fildago Ophiolite. The specific rocks of the ophiolite on Guemes Mountain are sheet-like igneous intrusions of granite, diorite, andesite and basalt - likely the roots of an island volcanic arc built up on the underlying ocean crust.
 

Notes From west side of Elwha Delta

I visited the west side of the Elwha River delta. The road dead ends at a trail head at a dike with a wide gravel path along the top of the dike.

Dike trail

Dike trail with estuary pond

View west from the dike

The  dike was built to block the river from cutting hard to the west and eroding the homes and former Elwha village site as well as a cemetery along the shore to the west of the delta. An 1860s map indicates that the village was there at that time. The dike was in place by 1977.  

Oblique aerial view (Ecology, 1977)

The river has since shifted away from the dike so its purpose is not so obvious when walking it today. 

Oblique aerial (Ecology, 2016)

The past few years there has been a very large influx of sediment post dam removal on the Elwha (https://www.usgs.gov/news/moving-mountains-elwha-river-still-changing-five-years-after-world-s-largest-dam-removal). 

One of the gig changes at least in the short term is the expansion of the beach to the west of the delta. The beach has become wider and substantially less steep and has a large accumulation of wood on the uppermost part of the beach. 

beach to the west

Wood on expanded upper beach

outlet of the Elwha

Broad gravel plain along river in the tidal area

I followed a trail through the riparian area of the forest to the river bank and then followed the river to the dike and returned to the trail via the dike trail. Hence, the pictures are in reverse order of my own visit.

Gravel deposits and bars at the former river ford above the delta

sediment and wood deposited within the riparian forest along river

Very high cut bank into the ice age former coastal plain

Canola in Central Washington

In the slightly wetter dry land farming zones of central and eastern Washington, canola fields have become part of the crop rotation.

Central Washington canola field with North Cascades in the distance

Connolly, McCracken and Painter (2016) describe a cost spread sheet developed for farmers considering planting canola. There has been an uptick in canola in Washington in part due to a canola oil plant built in Warden in 2013. Viterra recently gained full ownership of that plant (Press Release to WSU). Improvements to infrastructure and technical support may lead to expansion of canola in Washington.

The term canola is derived from combining "Canada" with "ola". Canola is a product of breeding out the undesirable part of rapeseed and was developed on the plains of Canada. Viterra is a Canadian Company.

Changes in farming can be global, and a big market for canola oil is China. The US-China trade struggles may impact these brilliant yellow fields. China has its own canola agriculture and has had trade disputes regarding canola imports to China from Canada that recently popped up again likely associated with the Huawei case.

Big Lake Black Bear

Considering my field time and the areas of much of my field work I do not see bears very often despite often seeing signs of the presence. This one was not interested in being seen but I spotted the bear traversing open ground before plowing through the brush back into the forest.

Black bear in Skagit County near Big Lake

Glacier Peak Tephra on the Waterville Plateau

Geology is a critical component of agriculture. The recessional glacial outwash plains around Lynden in northwest Washington formed some of the best agricultural lands in western Washington. The narrow gap at Wallula in the Horse Heaven Hills backed up ice age flood waters which in turn filled the Yakima and Walla Walla valleys with thick blankets of silt (lake-lewis-and-wallula). 

I had a nice geology outing with a soil scientist last week. It was informative interaction and we were traversing through country where Jay had completed soil mapping projects. Jay noted subtle features in the soil I would never have noticed without him.     

Note tiny tan grains

The small grains in the soil are tiny pieces of volcanic tephra. Given the central Washington location and the distribution of the grains Jay described, the source of the tephra is likely from Glacier Peak (Porter, 1978 and Kuehn and others, 2009).

(Kuehn and others, 2009)

This seeming small feature is a big deal to the local agricultural productivity. The tephra fragments allow the soil to hold a lot more moisture and thus adds significantly to the productivity of the fields where the volcanic material is present. The various tephra deposits are an important dating tool and thus tephra deposits are of great interest to more than geologists. Glacier Peak had a particularly violent eruptive period during and after the last glacial period. Mount Saint Helens and Mount Mazama also deposit tephra over a large areas. The three volcanoes have left dating markers over wide swaths of teh northwest.

Skagit County Greenschist Headed to the Columbia

It is a bit unusual to see a single rock being transported on the highway.

Large rock on I-5 north bound through the Chuckanuts

Large rocks are being transported from the Big Rock Quarry in Skagit County northward to to the Bellingham waterfront and from there to the North Jetty at the Columbia River.

 

Mouth of The Columbia River

The rock is greenschist - metamorphosed ocean floor basalt. It was mined from one of the terrains that make up the Northwest Cascades. The advantage of this rock is they can be broken into very large blocks, they have high density relative ti other rocks and are resistant to both physical and chemical weathering. Good material for a jetty that must resist huge waves. 

This has resulted in a proposal to mine additional greenschist in the Skagit Valley with a mine proposed and in at a greenschist outcrop near Marblemount.