As an Earth Science teacher, I felt like a kid in a candy store during this hike. Chief Mountain the classic example of a "klippe" (associated with the overthrust that formed Glacier Park), plus we had great views of a landslide that happened in 1992, Slide Lake, and a weird vegetation pattern (shown in photo above; not sure how it formed). CLICK HERE to access the blog, which includes a photo tour of all that we saw.
Logan Pass (elevation 6,646 feet) on the Continental Divide is the highest point on the Going-to-the-Sun Road in Glacier National Park. Although there are higher areas in the south-central part of the state, Logan Pass gets more precipitation than any place in Montana. Mountains along the divide force moist air from the Pacific upward, causing cooling by expansion. As the air reaches its dew point, vapor changes to snow (or rain). Also, Arctic air often moves into Montana along the east side of the divide, contributing to the lifting and cooling of Pacific air from the west. An area just east of Logan Pass, called “The Big Drift”, often records over 80 feet of snow, much of it pushed there by strong westerly winds that blow in the winter. A record gust of 139 mph was recorded in April of 2014.
The Going to the Sun Road, which can be seen in the photo, is one of the most scenic drives in the USA, and also one of the most difficult to snowplow. Crews usually begin plowing in early April, and the road is usually open from early June to mid-October, with the latest opening date being July 13, 2011 due to tremendous amounts of snow that fell that winter. The road, which was completed in 1932 and opened in 1933, connects the east entrance of the park (St. Mary) with the west entrance (near Lake McDonald). Although there aren’t many glaciers left in the park, the road provides visitors with excellent views of features carved by glaciers, including, hanging valleys, horns, glacial troughs, arêtes, and cirques. For those who want a closer look, there are several hiking trailheads along the highway, including the spectacular "Highline Trail" that starts at Logan Pass. The trail passes above the highway and below a portion of the Continental Divide known as “The Garden Wall.” The Highline Trail can be seen on the left side of the photo - between the highway and the patches of snow.
More information
1. Peak Bagging Near Logan Pass (many more photos)
2. Hiking the Highline - best trail in the park
4. Wikipedia: Going to the Sun Road
CLICK HERE to find out what it will look like from various locations. You can zoom, tilt the globe, or select a new location. THIS IS GREAT! It shows what it will look like from your location, including the timing. *See credits below.
*Credits
Producer: Kevin Hussey
Ranger Task Manager: Marc Pomerantz
Software Engineering Team Lead: Andrew Boettcher
JPL Ranger Software Engineering team: Andrew Boettcher, Michael Hans, Anton Kulikov, Mi Nguyen, Marc Pomerantz, Michael Sandoval, Davit Stepanyan, Brian Wright
Additional JPL support: Jason Craig, Matthew Garcia, Kevin Hussey, Daniel Sedlacko
UI Design and Development: Moore Boeck
Copyright 2017, by the California Institute of Technology. ALL RIGHTS RESERVED. United States Government Sponsorship acknowledged. Any commercial use must be negotiated with the Office of Technology Transfer at the California Institute of Technology.
Lots of geology going on here. Two of my hiking buddies are standing on the remains of a laccolith looking at Lost Lake whose basin was carved by outburst floods during the last ice age. The mountains in the background (Highwoods) are the remains of an ancient volcano that was active 50 mya.
After visiting Lost Lake we hiked up onto Square Butte (another laccolith). Both features are made of rock formed as magma cooled beneath the surface tens of millions of years ago. However, the story of Lost Lake includes another chapter that involved an unusual set of circumstances that happened during the last ice age. To learn how outburst flooding of Glacial Lake Great Falls was involved, go to bigskywalker.com.
1. Is there a "rock cycle" on Mars?
2. How is it different from the rock cycle on Earth? What processes are missing?
3. Is there molten rock on Mars?
4. Are there metamorphic rocks on Mars?
5. What drives the rock cycle on Earth?
The lab comes in a kit we purchase from WARD'S Natural Science, which includes this 2-part activity plus another activity related to ocean currents. The kit is called "Exploring Convection." To make the blue ice cubes, add 3 drops of food coloring to each empty cube mold in an ice cube tray, add water, and freeze.
CLICK HERE to see a video of "Part I".
CLICK HERE to see a video of the other lab included in the kit (related to ocean currents).
