Pine Creek Loses some of its Forest

 

Malden Post Office before the fire

Attribution of a single wildfire event to global warming is confounded by lots of other factors. The Malden area and Pine Creek valley are located in a climate edge area where pine forests meet grass lands (and now dry land wheat fields) in a mosaic landscape. Pine Valley where Malden is located was already in a fire prone area. Every summer the area becomes dry enough to burn with the grasses and brush being susceptible for a longer period and the trees for a shorter period. Towards the southwest that length of time becomes longer and to the north and east the length of time is shorter. Pine Valley is in a boundary area just moist enough that tree killing fires have been infrequent enough such that the valley has significant forest stands. 

With warmer average temperatures the length of time the area is susceptible to fire is now longer. But other factors can increase fire risk - years of fire suppression and changes to land use also alter the fire risk and how a fire will behave. With lots of roads, fires in Pine Valley could be readily suppressed and put out as long as fire weather conditions were not severe. Land use changes also play a role. Over time the forested areas began to encroach into the Malden town site.

The weather event associated with this fire included very high winds associated with an Arctic cold front that surged across the area from the northeast. The high winds had followed several days of at or near record daily highs in the region. The weather set up and fire risk was predicted several days before it took place (Inland Northwest Weather.blogspot). The same weather event was also associated with a much large fire that burned over 60 miles in the Okanogan Valley as well as the very intense wildfires on the west slopes of the Oregon Cascades.   

Pre and post fire aerial images show that a fair bit of the forests that were in the Pine Creek valley burned during the fire. 

Malden 1954

Malden 2017

Malden 2021

Northeast of Malden 2017

Northeast of Malden 2021

Pine City 2017

Pine City 2021

Malden, Washington Notes: Ice Age Flood Route

A bit over a year ago a wildfire burned much of Malden, Washington. Due to the extent of the destruction, the already tenuous economy of the small town and the very delayed National Major Disaster Declaration by the President, there have been follow up stories and takes on the fire and the aftermath (https://www.seattletimes.com/seattle-news/the-day-a-wildfire-took-malden/). Northwest Public Radio and Spokesman Review as well as Spokane area TV stations have continued to report on the town's effort at recovery.  

Malden Post Office before the fire

Malden is a bit off the usual routes; hence, I thought a little background on the landscape of Malden and the vicinity would be of use. I passed through Malden about a month before the fire and also on a trip to Rock Creek and Bonnie Lake (bonnie-lake-precambrian-schist). On that earlier trip I paused at the Post office (above picture). 

Malden is located in Pine Creek valley in the norther part of the Palouse. J Harlen Bretz (1923) recognized that the Pine Creek valley was a pre existing valley that was further eroded by ice age floods, "The valley during this episode in its history was but a channel. The glacial stream filled it from side to side for a depth of tens of feet. This is shown a few miles above Malden, where the stream flooded over a low shoulder of basalt, cutting a channel in the rock at least 40 feet deep, though the main valley alongside was a wide open and received gravel deposits." 

Map of Spokane Flood routes from Bretz (1925)

Flood water spillway from upper Latah Creek into the North Fork of Pine Creek (Bretz, 1923)

The ice age floods that Bretz was describing were the result of water spilling over from Latah Creek. The Okanogan ice lobe dammed the Columbia River forming glacial Lake Columbia in the backed up the Columbia River. The lake extended up the Spokane River and Latah Creek, a tributary stream to the Spokane River. When the ice dam at that formed ice age Lake Missoula collapsed, the flood waters surged out of the rapidly draining lake and into the Spokane area and into Lake Columbia. The sudden influx of a massive surge of water resulted in Lake Columbia overtopping at numerous low divides to the south. One big spill way is the Cheney-Palouse scabland tract southwest of Spokane. Interstate 90 passes through part of the tract. But some water backed up Latah Creek and spilled over a divide into the Pine Creek Valley.  

DEM of spillway from Latah Creek into Pine Creek

The ice age flood features in Pine Creek are a bit more subtle than the raw wide stripping of soil that took place in the very broad Cheney-Palouse route. But the features were noticeable to Bretz and are not consistent with the other valleys that were not flood routes that pass through the Palouse landscape. 

Another factor that softens the flood features in the Pine Creek Valley is that this flood route has a bit wetter climate than those to the west and the valley has more areas of pine -- hence the name Pine Creek. More on that on a future post.    
   

Pyrite in the Gravel

One of the sources of crushed gravel in Skagit County is a rock quarry. The quarry has mined large blocks of rock for levy projects, but the process of breaking the large intact blocks of rocks creates smaller rock. Hence a side product is angular crushed rock gravel for driveways and parking areas. The angular rock along with the fines within the crushed material forms a hard drive and parking surface. 

Crushed rock gravel parking area

Walking across one of these driveway areas on a moonlit night I noted remarkably bright spots in the gravel. My geology brain clicked in and I recalled the likely source of the gravel being a rock quarry excavated into some altered ocean floor igneous gabbro. The ocean floor rocks are a Jurassic age accreted terrain slab of ocean floor. Hot fluids flowing through and old ocean floor precipitated minerals. The bright spots I was seeing in the gravel was moonlight reflecting off of the very smooth surfaces of cubic pyrite minerals.       

A larger pyrite mineral - most are much smaller

I spotted this during the day when a very bright reflection struck my eye 

Pyrite is an iron sulfide mineral and is pretty common secondary mineral. Its breakdown via weathering in pyrite rich crushed mining tailings is a source of acid mine drainage. Its presence in some limestone deposits or the rock aggregates mixed into concrete is detrimental as the pyrite breaks down the sulfur released will form acids that will damage wiring, pipes or other metal in the concrete and can also form hydrogen sulfide foul odors.  

 

Ground Wasp Hazard Season

Field work hazards vary depending on where one is working and the time of year. In September in western Washington as well as elsewhere a hazard that I try to be alert for is ground wasp nests. 

Yellowjacket nest

The life cycle of the wasps is such that the nests become very large in late summer and the nest becomes populated with adult wasps that will readily defend the nest. Fortunately the wasps rarely sting when passing near the nest, but accidently stepping into or on a nest in late summer is a hazard.

I managed to avoid stepping into any nests last summer and thus far have a avoided doing so this late summer. Last week a client helpfully alerted me to a nest along a survey path cut through the brush prior to my field venture. I noted the small fast flying wasps near the nest shown above before spotting the entrance. 

My last encounter with stepping into a nest was on a very steep slope. The usual fast escape via running was impeded by the slope conditions which meant I had to crawl up the steep slope as fast as I could and likely further disturbed the nest as I began my escape. Once I reached the top of the slope, I was able to run, but continued to be stung. The next step was to shed my shirt and pants as fast as I could. Wasps release odors when they sting which stimulates additional stings and additional wasps to attack. My car was not far away and I had extra clothes (a typical habit as I often get wet doing field work). Even a half hour after my encounter there were still wasps stinging my dropped shirt.  

 

A Smoke Eclipse from the Schneider Spring Fire

I had a couple of central Washington projects and was relieved that the approaching cool front cleared the smoke away. The western air flow was evident as I approached the Columbia River gorge from the high plains of central Oregon.  

Lenticular clouds formed downwind of Mount Adams

However, the clearing of the stagnant air and smoke does not mean the fires are not still active. The Schneider Springs Fire (HERE) created a huge plume of smoke and cloud.

Plume of smoke and cloud above Schneider Springs Fire viewed from Yakima

In the Yakima Canyon between Selah and Ellensburg the plume of smoke passing overhead eclipsed the sunlight cooling temperatures in the canyon. 

North end of the Yakima Canyon with the Stewart Range in the distance and thick smoke overhead 

Dim evening like light south of Ellensburg

Smoke plume downwind darkening the Wenatchee Mountains

View to the west from Highway 10 northwest of Ellensburg

About half way between Ellensburg and Cle Elum I got back into the sun. 

Smoke plume and wind turbines northwest of Ellensburg

It was nice to have the smoke pass over and not breath it. There was some ash fall of white burnt fir needles while I was working in the Yakima Canyon, but no smoke, no hot sun and temperatures in the mid 80s made the work a lot easier than expected.

Back From Halle (Saale)

I returned from a two month break. I did some remote work while gone, but am now back on field work and follow up writing ventures. I appreciated the support of my associates at Stratum Group that worked more than diligently in my extended absence as well as dealing with the issues of working in and through the time of covid and the preparations for changes in Stratum Group.  

For two months one of my views in Halle (Saale) was this wall across the street from where I was staying. I sat in a chair at the window and contemplated the odd assortment of rock blocks and obvious multiple periods of window openings. 

The building is old by the Washington State standards that I am used to. As best as I was able to piece together the history, the initial structure dated back to the 1200s, but it may be even older. I suspect it has had multiple periods of use and vacancy - pictures from the 1980s showed that the roof was missing. An associated building had been badly damaged by one of Napoleon's armies. 

The rock blocks are mostly local volcanic sandstone and volcanic rocks of Permian age. 

Geology is the basis of Halle's history; the Market Square Fault cuts through the city and that fault caused salt water springs to issue from the ground on the west side of the city. The salt was a very valuable commodity. The fault is given credit in the main square of the city next to the drinking fountain. 

The English side of the marker made my translation easy

As noted on the marker salt was utilized from the site at least 5,000 years ago. Approximately 20 miles to the west there is a Paleolithic site that dates back 400,000 years. People were here for a long time compared to my homeland in Washington. 

I returned home this last week with only a brief view of scenery on the flight back as most of the flight was over clouds.

Near to coast of Greenland

I miss my night shift and walk-about companion during my stay in Halle (Salle).  

At the river lock on one of many walk-about adventures 

Flood Plain Hazards of Open Pit Mines

I missed the historic heatwave in the Pacific Northwest as I am currently in Germany. I am not in the zone that has been impacted and terrible floods, but the event is 'close to home' so to speak. Dave Petley (HERE) noted a river in the west of Germany that broke out of its course and flowed into an open pit coal mine in Inden. 

Dave noted the river course into the mine followed an old channel. That channel was the former river channel up until about 15 years ago. The channel was blocked and the river was rerouted in a long circuitous route around the mine.

Blue line shows river route around open pit coal mine

Blue line showing most recent river route and red line showing former path

Although the flooding of the coal mine was impressive, a more dangerous flood into an open pit mine took place a few miles away at Blessem. NPR led their story on the flooding with an image that had a caption about an entire field collapsing due to flooding (npr.org/germany-belgium-flooding). 

  (picture alliance/dpa/Rhein-Erft-Kreis | Rhein-Erft-Kreis) The image shows very rapid headward erosion as floodwaters drain off the flood plain down a steep gradient. The source of that gradient was and open pit sand and gravel mine. 

Same site looking toward the mine  (picture alliance/dpa/Rhein-Erft-Kreis | Rhein-Erft-Kreis)

Red line is approximate extent of area eroded. The yellow line is my measurement of the headward erosion distance of 850 feet.

The headward erosion continued after the above image and expanded into the town taking out a number of buildings. 

 

In this case it appears that flood waters on the flood plain began to flow rapidly towards the pit as the water drained towards the low area of the sand and gravel mine. While gentle slope wide flood plains have flood risk and potential hazards associated with channel movement. The rapid erosion associated with flood water flows into open pit mines is well demonstrated at this site.