The Washington Cascade Range & Mt. St. Helens National Volcanic Monument: Road Log & Backcountry Geology

★★★★★ 4.1 96 reviews

$90.00
Price when purchased online
Free shipping Free 30-day returns

Sold and shipped by www.asmed.net
We aim to show you accurate product information. Manufacturers, suppliers and others provide what you see here.
$90.00
Price when purchased online
Free shipping Free 30-day returns

How do you want your item?
You get 30 days free! Choose a plan at checkout.
Shipping
Arrives Jun 30
Free
Pickup
Check nearby
Delivery
Not available

Sold and shipped by www.asmed.net
Free 30-day returns Details

Product details

Management number 231892068 Release Date 2026/06/18 List Price $90.00 Model Number 231892068
Category

During the Middle Eocene, the Siletzia and Crescent terrains accreted basalt along the continental margin. Two large marine basins received sediments belonging to the Cowlitz Formation and Puget Group. The shoreline was positioned around Interstate 5 corridor or slightly east in Central Lewis County. Sedimentary deposits covered the Siletzia and Crescent oceanic basalts. The volcanic arc was positioned in Idaho and eastern Washington.The earliest Cascade Range volcanoes erupted in Western Washington producing high silica rhyolites and fragmental material during the Late Eocene time. Shield volcanoes erupted west of the present day Mount St. Heleens producing basalts.During Late Eocene, Oligocene, and Early Miocene, a large volcanic pulse produced a new volcanic arc east of the Late Eocene arc. Basalt and basaltic andesite yielded to andesite and dacite. Eruptions became more explosive. The Spirit Lake Pluton was injected near the end of this time period.During the Middle Miocene, volcanism in the Cascades slowed. Tectonic uplift eroded most of these volcanoes away. Dikes and sills became common. Flood basalt erupted from feeder dikes in eastern Washington, eastern Oregon, and Idaho. During Late Miocene, dikes and sills intruded north and south of Mount St. Helens. Gentle folding of rocks continued.During Pliocene through Pleistocene, volcanism in the Cascades picked up again. Glaciers covered much of the Cascade Range. For major glaciations are recorded. Mount St. Helens began erupting 40,000 years ago.Chapter 1 presents an introduction to the evolution of the Cascade Range. Chapter 2 presents an M.S. Thesis on the Cascadian Foothills. Chapter 3 discusses Southwestern Washington tectonic rotation. Chapter 4 begins with an introduction to stages and eruptive events of Mt. St. Helens. Chapter 5 begins the roadside geology of Mt. St. Helens National Volcanic Monument. Chapter 6 describes WA 503 road log geology and road logs to the south and east. Chapter 7 presents the final road log along US 12 from Randle to Salkum. Read more

ASIN B0CLJ3R645
XRay Not Enabled
ISBN13 979-8865046578
Language English
File size 36.9 MB
Page Flip Enabled
Publisher Earth2Energy Educational Publishing
Word Wise Not Enabled
Print length 250 pages
Accessibility Learn more
Screen Reader Supported
Publication date October 20, 2023
Enhanced typesetting Enabled

Correction of product information

If you notice any omissions or errors in the product information on this page, please use the correction request form below.

Correction Request Form

Customer ratings & reviews

4.1 out of 5
★★★★★
96 ratings | 39 reviews
How item rating is calculated
View all reviews
5 stars
77% (74)
4 stars
7% (7)
3 stars
4% (4)
2 stars
2% (2)
1 star
10% (10)
Sort by

There are currently no written reviews for this product.