Skip to main content

2016 Summer Mountain Trip Part 15; Yellowstone National Park and the Grand Loop Road

After reaching the western terminus of US Route 212 I entered Yellowstone National Park from the Northeast Entrance Station.


This blog serves as Part 15 of the 2016 Summer Mountain Trip Series; Part 14 can be found here:

2016 Summer Mountain Trip Part 14; US Route 212 over the Beartooth Highway

Yellowstone National Park is the oldest National Park in the United States having been signed into law by President Ulysses S. Grant in 1872.  Yellowstone National Park consists of land located on the Yellowstone Caldera mostly in Wyoming but also in parts of Montana and Idaho as well.

Contrary to what Google Maps might tell you, the US Routes cease to exist within Yellowstone National Park.  Yellowstone instead is traversed by a series of roadways maintained by the National Park Service, many which actually shutter in the winter months.  The Northeast Entrance Road begins at the west terminus of US Route 212 and follows the Lamar River to the Grand Loop Road at the confluence with the Yellowstone River.  The Lamar River apparently is one of the best places in all of Yellowstone to find wandering herds of Buffalo.









It isn't uncommon to see all sorts of animals along the waterways of Yellowstone.


At Tower Junction the Northeast Entrance Road crosses the Yellowstone River and meets the Grand Loop Road which circles almost all of Yellowstone National Park.  I turned south on the Grand Loop Road from Tower Junction.



On the Grand Loop Road heading southbound there are some scenic views of the Yellowstone River at Devil's Den as it descends from Yellowstone Lake through the northern extent of the Grand Canyon of the Yellowstone. 



Tower Fall along Tower Creek can be observed from Devil's Den.


The Grand Loop Road ascends over the 8,859 foot Dunraven Pass near Mount Washburn which provides a wide vista of the surrounding terrain.  The summit of Mount Washburn lies at 10,243 feet above sea level.





At Canyon Junction I pulled off the Grand Loop Road on to Rim Drive above the Grand Canyon of the Yellowstone.  Rim Drive provides access to the vistas above the Grand Canyon of the Yellowstone. The 109 foot high Upper Yellowstone Falls can be observed from Rim Drive.



I parked my car along Rim Drive and ran the rest of the way to the overlooks.  I first made my way to the top of Lower Yellowstone Falls.




From the bottom of Yellowstone Falls the full 308 foot drop can be easily observed.



From Canyon Junction I turned west on Norris Canyon Road to take a shortcut towards the western part of the Grand Loop Road.  Upon reaching Grand Loop Road again I turned south towards Old Faithful and stopped at Gibbon Falls located on the Gibbon River.


Near Madison Junction the Grand Loop Road follows the Firehole River southward.  I stopped briefly on the Fountain Paint Pot Trail to see the geyser basin.







One of the main attractions on the western segment of Grand Loop Road is Grand Prismatic Spring.  Grand Prismatic Springs is the largest hot spring in Yellowstone and the third largest in the world.  The strange colors come from microbes which produce the effect near the rim of the 370 foot diameter hot spring.  Grand Prismatic Spring is 160 feet deep and the clear blue color is endemic of the sterile environment.  Grand Prismatic Spring has a temperature apparently close to 160F.


The Opal Pool, Turqoise Pool, and Excelsior Pool are located within the vicinity of Grand Prismatic Spring.




At the very bottom of Grand Loop Road is the Upper Geyser Basin.  The Old Faithful Geyser is a well known and highly predictable geyser which was first discovered in 1870.  Old Faithful erupts on average every 90 minutes at heights generally ranging from about 106 to 185 feet.  The Old Faithful Geyser seems to be relatively predictable in nature due to it not being tied to any other feature in Upper Geyser Basin.  The steam erupting from Old Faithful generally ranges from 240F to 265F.


















At West Thumb I stopped briefly at Yellowstone Lake before heading south out of Yellowstone National Park on South Entrance Road.  Yellowstone Lake is the largest freshwater lake in the United States above 7,000 feet at approximately 136 square miles.  Yellowstone Lake isn't especially deep which causes it's surface to freeze mostly over in the winter months.  The primary inflow and outflow of Yellowstone Lake is the Yellowstone River.


South Entrance Road follows the Lewis River to the confluence with the Snake River at the boundary of Grand Teton National Park.  South Entrance Road becomes John D. Rockerfeller Parkway in Grand Teton National Park.

Part 16 of this blog series can be found here:

2016 Summer Mountain Trip Part 16; Grand Teton National Park and the nebulous disconnect in the US Routes

Comments

Popular posts from this blog

Former US Route 50 and the Pioneer Route Lincoln Highway on Johnson's Pass Road

Johnson's Pass Road is one of the oldest highway corridors in California.  Johnson's Pass was part of the Lake Tahoe Wagon Road as it was completed during 1856 over the Sierra Nevada.  The pass would later be incorporated into the Pioneer Branch of the Lincoln Highway in 1913 and US Route 50 in 1926.  Johnson's Pass Road would be bypassed by a new alignment of US Route 50 over Echo Summit in 1938.  A replacement of the Meyers Grade east of Johnson's Pass would be opened to traffic in 1947.   Johnson's Pass Road remains accessible to traffic and is still signed by the Lincoln Highway Association.  Pictured as the blog cover is the view from the top of Johnson's Pass Road overlooking modern US Route 50 and Lake Tahoe.   Part 1; the history of Johnson's Pass Much of the history of what become the Lake Tahoe Wagon Road is discussed in the  September 1950 California Highways & Public Works  during its Centennial Edition.  The or...

Former US Route 50 and the South Lincoln Highway from Folsom east to Placerville

The corridor of Folsom of Sacramento County east to Placerville of El Dorado County has been a long established corridor of overland travel dating back to the California Gold Rush.  The Folsom-Placerville corridor was once part of the path of the Lake Tahoe Wagon Road which became the first California State Highway and later the South Lincoln Highway.  In time the South Lincoln Highway's surface alignment was inherited by US Route 50.  The Folsom-Placerville corridor also includes the communities of; Clarksville, Shingle Springs and El Dorado. Part 1; the history of the Lake Tahoe Wagon Road, South Lincoln Highway and US Route 50 through Folsom-Placerville Folsom is located on the American River/Lake Natoma of eastern Sacramento County.  That lands now occupied by the City of Folsom were part of Rancho Rio de los Americanos prior to the finding of gold at Sutter's Mill during 1848.  During the California Gold Rush the lands of Rancho Rio de los Americanos were p...

Old NC 10 - The Central Highway: Old Fort to Black Mountain through the Royal Gorge

A unique way of tracing the remnants of the Central Highway is through the mountainous terrain of Eastern Buncombe and Western McDowell Counties.  From the east on US 70, you reach the base of Blue Ridge Mountains at the town of Old Fort.  Old Fort is a tiny rail town that the old Central Highway and now US 70 goes through.  The Central Highway can be followed via a right onto Mill Creek Road from US 70.  Follow the highway as it takes you closer to the mountains.  When Mill Creek Road bears right to head towards Andrews Geyser stay straight until the road ends at a gate.  The nearby Piney Grove Church can be used for parking.  At this point, the old Central Highway began a 3.5 mile climb of the mountain to Swannanoa Gap.  NC 10 and later US 70 travelers followed this road for over 30 years until a new and modern four lane US 70 was built to the south.  This same four lane road would eventually become Interstate 40.    The Centra...