Page 16 of buddymedbery Travel Blog Posts


North America » United States » Wyoming » Gillette July 20th 2011

After a violent thunderstorm the previous evening, after which we finally ate a delicious dinner in the Mural Room with a table by the large picture windows looking out onto the mountains, we headed north again. By driving back through part of Yellowstone, we were able to save substantial mileage.That turned out to be fortuitous, because the drive out the East Entrance of Yellowstone was one of the more beautiful drives we took. After passing Mary Bay, underneath which lie the hottest parts of the park, you climb out through a high pass with new snow patches and waterfalls around every bend. Eventually, on the other side of the pass, you enter an area of fantastically carved hoodoos in soft welded ash and rhyolite rock. Streams and lakes abut the highway. Eventually you come out onto ... read more
Mountains, lake near Yellowstone East Entrance
Waterfall near Yellowstone East Entrance
Hoodos near Yellowstone East Entrance


We did not attempt to arise ery early since we knew we would have plenty of time to see the greatest part of the park. We started just a couple of miles south of Jackson Lake Lodge at Lake Jackson Dam, taking pictures of the tremendous water flow through the dam spillway and of the Tetons reflected in the still lake. we then worked our way southward, stopping at every byway and turnout we could find, traveling along the slower low road. It is difficult to describe the experience of the Tetons. At every stop, you are presented with another view that can make even the most recognizable peaks unrecognizable. The glacial valley through which you drive is flat but curiously terraced away from th river, reflecting the height of the river at various stages in ... read more
Tetons reflected in Jackson Lake
Balsamroot-and-Tetons
Beaver-dam-at-Schwabacher-Landing


Rising up almost directly from the plains, the Tetons present some of the most picturesque mountain views in the world. There is no crawl upward through ever higher foothills - it is just a straight shot up to the summit of Grand Teton at 13,775', rising 7000' above Jackson Hole. However, this is partly illusory, since Jackson Hole is depressed below the surrounding plains. Although containing some of the oldest rocks in North America ) 2.5 billion years old), the Tetons are one of the youngest mountain ranges on earth, their formation having started some 6-9 million years ago. The were created by a graben fault that resulted in the mountains being pushed up while Jackson Hole fell. The parks was created in 1929, and expanded with the addition of the previous Jackson Hole National Monument ... read more
Jennie, Jan at highest point Rendezvous Peak
"watermelon snow"
Grand Teton at sunset


In 1950, a frightened, orphaned bear cub with badly burned paws was retrieved from a tree where he had taken refuge from the Capitan Gap fire in Lincoln County, NM. Flown by private plane to Washington's National Zoo, he became the living embodiment of the U.S. Forest Service campaign against fires which had begun with the debut of a new ad campaign in 1944 in which Smokey Bear ("the" was added later by popular usage) told us that by taking care we could prevent 9 out of 10 forest fires. The official policy was to suppress all fires by 10 A.M. the morning after they were spotted. Thousands of fire spotting towers were set up in national forests, and a small army of men was employed to fight the fires as needed. Unfortunately, Smokey ran afoul ... read more
Deer caught in Yellowstone fire
Extensively burned area near Mary Bay Yellowstone
Stand of new lodgepole pines in burned area


A current video about Yellowstone calls the park "a symphony of fire and water" and I can't come up with a better description. Water is everywhere - flowing, spouting, steaming and gurgling. Water has shaped the landscape and provided much of the explosive energy that has created such features as the West Thumb limb of Yellowstone Lake. It constantly percolates down from the surface into the porous and cracked rock underneath, reaching great depths where pressure can result in water remaining in the liquid form at temperatures higher than 400 degrees. Water in the form of glaciers formed many of the valleys and left behind rock piles known as moraines, as well as large boulders strewn about haphazardly. But one of the most visible activities of water is to emerge from underground as one of the ... read more
Thumb Paint Pots
Old Faithful
Opal Pool


The other reason for visiting Yellowstone is to view the astonishing geographic/geologic features. Although Old Faithful is the very icon of Yellowstone, it represents only one aspect of the park. Yellowstone sits atop an ancient caldera, one which has blown up catastrophically about every 640,000 years, the last time being about 640,00 years ago. For comparison, the Lava Creek supereruption about 1.2 million years ago produced about 2500 times as much ash as Mt. Saint Helens. Herds of animals in Nebraska were killed in the resultant ash fall, as seen at Ashfall Fossil Beds State Historical Park. The Yellowstone caldera is situated over a hot spot in the earth's crust, similar to Hawaii, where molten magma is unusually close to the surface. Like the Hawaii hot spot, it is showing apparent motion, though what is really ... read more
Grand Canyon of the Yellowstone from brink of Lower Falls
Artists Point
Brink of Lower Falls


A short drive from Bozeman brought us to the Gardiner entrance to Yellowstone National Park. This is the big one- the oldest national park in the world, about 2 million acres of mountains, plains, rivers, and geothermal features. Instead of sticking to a daily journal, it is a lot more useful to divide this into the two main categories of things to be seen: animals and geographic/geologic features. Yellowstone has been called the "American Serengeti". Having seen both, I would agree. Yellowstone comprises a large ecosystem with relatively balanced predator/prey populations, particularly since the reintroduction of wolves in 1995. There are about 30-40,000 elk, 2500-4500 bison, about 600 grizzly bears, an approximately equal number of black bears, and about 200 wolves. Elk and bison are essentially omnipresent throughout the park, while bears are much less commonly ... read more
BIson male
Grizzly sow and cubs
Grizzly (?)


Luck is on our side. Our itinerary was based on going across Glacier National Park on the Going to the Sun Road, one of the most beautiful drives in the world. It is almost always open by July 1, and it never occurred to me when planning that it would not be open when we arrived to traverse it on July 13. The unusually heavy snows had presented unusual challenges in plowing, and it was a close thing. Where it crosses the Continental Divide at Logan Pass and just to the east, the snow cam top 80' or more. It opened today for the first time this year. We were following the news with some anxiety until the last minute. It generally opens in early June, and today is the latest opening ever. The road cuts ... read more
Triple Divide Peak
Jan with wall of snow
Buddy, Jennie at Logan Pass


At the end of our Crypt Lake hike, a fellow hiker came down with his hiking poles and after talking with him we realized that they could be quite helpful. As we discovered, they allow you to use your arms to take some of the strain off your legs. This is useful both in ascent and in descent, sparing muscles going up and knees coming down. So we bought collapsible hiking poles before attempting our next hike. Today's goal: Grinnell Glacier. We had done this hike many years ago with the kids, and it was one of the most beautiful things I had seen, so we wanted to repeat the experience. On our previous experience, Clint was ten and Ashley eleven. When we finished the hike, a woman was sitting alone in the boat back to ... read more
Many Glacier Hotel across Swiftcurrent Lake
Jennie, Jan on Grinnell Glacier Trail
Lake from Grinnell Glacier Trail


After the rigors of the Crypt Lake hike, we needed an easier day and got it on our drive back into the USA to the Glacier National Park area. Heading south from Canada, we encountered Chief Mountain again from the north side, giving us a much different perspective. This 9080' mountain is composed of limestone that is much older than the underlying gray shale. This occurred as part of the Lewis overthrust when Precambrian rocks were forced by tectonic forces over the 1400 million year young shale, forming the Rocky front that extends from Montana to Alberta. Erosion removed much of the surrounding rock, leaving the surrounding tower we now see. It has long been considered a sacred place by the native Blackfeet indians of the area. The very difficult climb was first made by a ... read more
Swiftcurrent Lake in front of Many Glacier Hotel
Jennie at Luna Restaurant
Glacier-fed river




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