Rock Trail in the Chuckanuts updated

I updated my geo guide to the Rock Trail in Larrabee State Park; I hiked it last Friday on a gorgeous warm spring day. This is one of my favorite geology hikes in the park; I wrote the original description on this website shortly after the trail was finished in 2014. So, what’s new? A ways beyond the last high sandstone wall I came across a new [to me] exposure of sandstone, scoured and cleaned off. Looks like the overlying soil and vegetation slid off and the beautiful rock has since been been flushed clean by heavy rains. The slab reveals some very fine cross beds so I added this near the end of the guide. Go now- before the trees leaf out there are views east to snowy Mount Baker and the Sisters Range.

Cross-bedded stream sand in the ‘pale slab’.

About these field trips- they are not actually ‘virtual’.

Dear friends and subscribers,

There seems to be considerable misunderstanding of my use of the term ‘virtual’ field trip. I do not actually lead the field trips i publish on this website. I write them up so YOU can go do them yourself; they are intended to be self guided. My apologies for misunderstandings and apparent misuse of the term. I will no longer these field trips as ‘virtual’, as that apparently implies you can ‘join me’ on line somehow.

It is my hope you will find field trips to places near you, or that pique your interest, and go there. You can take along the website on a smart phone, or use the tips here to show you how to efficiently print out the trip on actual real paper.

Dave Tucker

Point Whitehorn: updated field trip

I updated my 11-year-old virtual field trip to Point Whitehorn, up the coast from Bellingham and just south of Birch Bay. I have been there many times in the intervening years. It’s always a fine jaunt, especially in winter and most especially on the day after Thanksgiving! There is plenty of changing geo scenery due to wave erosion of the beach bluff. The updated page has a lot of new pictures. Like this one.

Whoo hoo! If any visitors have pictures documenting further erosion around this big erratic, send them to me. How much longer until it is on the beach?

Damfino lakes geology hike

Mazama O and Baker BA ash on the Damfino Trail.

I just posted my geology field trip guide to the Damfino Lakes Trail, reaching Excelsior Pass from the Canyon Creek road to the north- and a much shorter hike than the Excelsior Trail.

The rock exposures aren’t all that great, but there is a small and lovely exposure of Mazama ‘Layer O’ volcanic ash and Mount Baker BA ash sitting right on top. And of course the flower meadows and the views.

Excelsior Trail geology guide is up!

As promised a week ago, I completed the geology guide to the Excelsior Trail, rising from the Nooksack River east of Glacier to Excelsior Pass and ‘Excelsior Peak’. I will post a separate description for the ‘back door’ trail via the Damfino Lakes trail.

Steeply dipping Jurassic Nooksack Formation marine sedimentary rocks just east of Excelsior Pass.

Mount Baker Geology Report is published!

Dear friends,

Many of you will know that for years I have been among a group of geologists putting together a USGS report on the volcanic history of Mount Baker since the end of the last glacial maximum {that’s geologese for ‘Ice Age’). That paper has just gone up on line and you can read it here: https://doi.org/10.3133/pp1865

The authors are Kevin Scott (USGS, retired); myself; Jon Reidel (North Cascades National Park); Cynthia Gardner (Cascades Volcano Observatory, USGS); and Jack McGeehin (USGS, who did the C14 analyses)

The brief citation reads:

Latest Pleistocene to Present Geology of Mount Baker Volcano, Northern Cascade Range, Washington: This report summarizes the multifaceted and complex surficial geologic history of Mount Baker just before, during, and after withdrawal of the latest Pleistocene Cordilleran ice sheet from the Mount Baker area. Nearly 80 new radiocarbon ages are reported that constrain the timing of glacial and volcanic events and help define four post-glacial eruptive periods: Carmelo Crater (ca. 14–11.6 ka), Shriebers Meadow (ca. 9.8–9.1 ka), Mazama Park (ca. 6.7 ka), and Sherman Crater  (1842–1880 C.E.).  The end of the Carmelo Crater eruptive period marks the end of Mount Baker edifice construction and the beginning of mainly destructional processes (flank failures and resultant lahars) during the Holocene.  It also marks a shift of vent location from the summit to off-summit locations. Findings from this paper dovetail with the bedrock history of Hildreth and others (2003) to give a comprehensive view of the United States’ most northern Cascade volcano.

 

Scott, K.M., Tucker, D.S., Riedel, J.L., Gardner, C.A., and McGeehin, J.P., 2020, Latest Pleistocene to present geology of Mount Baker Volcano, northern Cascade Range, Washington: U.S. Geological Survey Professional Paper 1865, 170 p.  https://doi.org/10.3133/pp1865

Coming up: Excelsior Trail geology guide

Looking west along Excelsior Ridge from just below the pass.

In the next couple of days I plan to post a geology guide to the Excelsior Pass Trail. The trailhead is near Nooksack Falls; the trail climbs out of the North Fork Nooksack valley to Excelsior Pass. The trail ascends through the Jurassic Wells Creek Volcanic Member of the Nooksack Formation; I wrote of them waaaaay back in 2010, here. Find the glory of flower meadows and views and, at the pass, the reach small exposures of conglomerate and breccia in the slightly younger Nooksack Formation.

A fragment of greenstone from the Wells Creek volcanics. Exposure to the atmosphere and water has produced the 1-cm-thick weathering rind on two sides of this bit of rock, but the greenish rock in the center is fresh greenstone- at one time a submarine volcanic deposit.

Racehorse fossil fields- update

I visited the Racehorse Fossil Fields up the North Fork Nooksack on July 10. I have updated the access directions. If you haven’t been there in a while you may marvel at the amount of biomass that is now covering the 2009 landslide and growing on the road. It is now a foot path, in places a green tunnel. A relatively simple walk though, for 1 mile and there are still plant fossils to be found.

It was fun to see so many website subscribers up there. Dave

New geo field trip to Chuckanut rocks posted on this website

Dear Friends,

Outcrops along the road.

I just posted a new virtual field trip. It is a 3-mile round trip walk on a logging road in the Chuckanut Mountains just south of Bellingham. It examines near-continuous exposures of a variety of rocks in the Chuckanut Formation. The road is gated so no vehicle traffic.

You will see conglomerate transitioning to sandstone and vice versa. The trip describes the dip, or tilt, of the rock layers, and finishes up at a quarry in remarkable conglomerate. Plus a very nice view down the length of Lake Samish.

Virtual Geology Fieldtrips offered

My friend David B. Williams in Seattle is hosting virtual geology field trips. If you read

Chapter 14 is a tour of  Seattle building stone

chapter 14 in my book, Geology Underfoot in Western Washington, you will love the ‘Stories in Stone’ tour. My chapter was inspired by David’s downtown Seattle Urban Geology tour.

New edition of David’s book. GET IT!

Through the Seattle Architectural Foundation, David is offering Stories in Stone (June 10)- Most people do not think of looking for geology from the sidewalks they travel, but for the intrepid geologist any good rock can tell a fascinating story. On this virtual walk, which incorporates illustrations and photographs, you will explore a range of rocks equal to any assembled by plate tectonics, from 3.5-billion-year-old gneiss to 120,000 years old travertine; fossils the size of cinnamon rolls, and rock used by the Romans to build the Colosseum. In this tour of Seattle building stone, David will discuss history, transportation, and architecture to give you a new way to appreciate urban geology. Plus, you’ll even be able to “visit” a couple of quarries and see where the stone originates. $5/person

Through Airbnb David is offering The Secrets of Seattle’s Disappearing Hills (Multiple dates) [Mondays and Thursdays in June- dt]- On this virtual walk you will explore Seattle’s most famous land alteration project: the complete removal of a hill in the downtown area. Through a series of illustrations and maps and historic photos, we’ll virtually cover about 1.5 miles circumnavigating the old hill in the area known as the Denny Regrade, where Amazon’s campus is now located. Along the walk, we’ll learn about how and why early Seattleites undertook this audacious and ambitious project, which they completed between 1897 and 1930. We’ll also see clues in the landscape that allow you to visualize Denny Hill as well as see historic images to better understand the story. $7/person

Chuckanut Fm. sandstone forms the vertical columns on the Pioneer Building in Seattle. Photo copyright Dave Tucker.