Top Attractions in Yellowstone National Park

Upper Geyser Basin

Upper Geyser Basin has the highest concentration of geothermal features in the park. This complement of features includes the most famous geyser in the park, Old Faithful Geyser, as well as four other predictable large geysers. One of these large geysers in the area is Castle Geyser which is about 1,400 feet northwest of Old Faithful. Castle Geyser has an interval of approximately 13 hours between major eruptions, but is unpredictable after minor eruptions. The other three predictable geysers are Grand Geyser, Daisy Geyser, and Riverside Geyser. Biscuit Basin and Black Sand Basin are also within the boundaries of Upper Geyser Basin. The hills surrounding Old Faithful and the Upper Geyser Basin are reminders of Quaternary rhyolitic lava flows. These flows, occurring long after the catastrophic eruption of 640,000 years ago, flowed across the landscape like stiff mounds of bread dough due to their high silica content.

Lower Geyser Basin

Lower Geyser Basin has a much less concentrated set of geothermal features, including Fountain Paint Pots. Fountain Paint Pots are mud pots, that is, a hot spring that contains boiling mud instead of water. The mud is produced by a higher acidity in the water which enables the spring to dissolve surrounding minerals to create an opaque, usually grey, mud. Also found in this basin is Great Fountain Geyser, whose eruptions reach 100 to 200 feet in the air, while waves of water cascade down its sinter terraces.

Midway Geyser Basin

Midway Geyser Basin is much smaller than the other basins found alongside the Firehole River. Despite its small size, it contains two large features, the 200-by-300-foot wide Excelsior Geyser which pours over 4,000 U.S. gallons (15,000 L; 3,300 imp gal) per minute into the Firehole River. The largest hot spring in Yellowstone, the 370-foot (110 m) wide and 121-foot (37 m) deep Grand Prismatic Spring is also found here.

Grand Canyon of the Yellowstone

The Grand Canyon of the Yellowstone is the first large canyon on the Yellowstone River downstream from Yellowstone Falls in Yellowstone National Park in Wyoming. The canyon is approximately 24 miles long, between 800 and 1,200 ft deep and from .25 to .75 mi wide.

Norris Geyser Basin

The Norris Geyser Basin is the hottest geyser basin in the park and is located near the northwest edge of Yellowstone Caldera near Norris Junction and on the intersection of three major faults. The Norris-Mammoth Corridor is a fault that runs from Norris north through Mammoth to the Gardiner, Montana, area. The Hebgen Lake fault runs from northwest of West Yellowstone, Montana, to Norris. This fault experienced an earthquake in 1959 that measured 7.4 on the Richter scale (sources vary on exact magnitude between 7.1 and 7.8; see 1959 Hebgen Lake earthquake). Norris Geyser Basin is so hot and dynamic because these two faults intersect with the ring fracture zone that resulted from the creation of the Yellowstone Caldera of 640,000 years ago. The Basin consists of three main areas: Porcelain Basin, Back Basin, and One Hundred Springs Plain. Unlike most of other geyser basins in the park, the waters from Norris are acidic rather than alkaline (for example, Echinus Geyser has a pH of ~3.5). The difference in pH allows for a different class of bacterial thermophiles to live at Norris, creating different color patterns in and around the Norris Basin waters. The Ragged Hills that lie between Back Basin and One Hundred Springs Plain are thermally altered glacial kames. As glaciers receded the underlying thermal features began to express themselves once again, melting remnants of the ice and causing masses of debris to be dumped. These debris piles were then altered by steam and hot water flowing through them. Madison lies within the eroded stream channels cut through lava flows formed after the caldera eruption. The Gibbon Falls lies on the caldera boundary as does Virginia Cascades.

Lake Fish Hatchery Historic District

The Lake Fish Hatchery Historic District comprises nine buildings built between 1930 and 1932 by the U.S. Fish and Wildlife Service in the National Park Service Rustic style. The buildings exhibit a consistency of style and construction, with exposed gable trusses and oversized paired logs at the corners, all with brown paint. The district is located on the shore of Yellowstone lake near the Lake Hotel The hatchery was established to provide Yellowstone cutthroat trout eggs for state and federal hatcheries outside of Yellowstone.

Old Faithful Historic District

The Old Faithful Historic District in Yellowstone National Park comprises the built-up portion of the Upper Geyser Basin surrounding the Old Faithful Inn and Old Faithful Geyser. It includes the Old Faithful Inn, designed by Robert Reamer and itself a National Historic Landmark, the upper and lower Hamiltons Stores, the Old Faithful Lodge, designed by Gilbert Stanley Underwood, the Old Faithful Snow Lodge, and a variety of supporting buildings. The Old Faithful Historic District itself lies on the 140-mile Grand Loop Road Historic District. A notable missing portion of the district is the Old Faithful Museum of Thermal Activity, which formed part of the trailside museum group that includes the Madison Museum, Norris Museum and Fishing Bridge Museum, all listed as National Historic Landmarks. The Old Faithful Museum was torn down in 1971 to make way for the Mission 66 visitor center, which in turn has been replaced by the Old Faithful Visitor Education Center.

Old Faithful

Old Faithful is a cone geyser located in Wyoming, in Yellowstone National Park in the United States. Old Faithful was named in 1870 during the Washburn-Langford-Doane Expedition and was the first geyser in the park to receive a name. It is one of the most predictable geographical features on Earth, erupting almost every 94 minutes. The geyser, as well as the nearby Old Faithful Inn, is part of the Old Faithful Historic District.

Grand Prismatic Spring

The Grand Prismatic Spring in Yellowstone National Park is the largest hot spring in the United States, and the third largest in the world, after Frying Pan Lake in New Zealand and Boiling Lake in Dominica. It is located in the Midway Geyser Basin. Grand Prismatic Spring was noted by geologists working in the Hayden Geological Survey of 1871, and named by them for its striking coloration. Its colors match the rainbow dispersion of white light by an optical prism: red, orange, yellow, green, and blue.

Castle Geyser

Castle Geyser is a cone geyser in the Upper Geyser Basin of Yellowstone National Park. It is noted for the particularly large geyserite sinter deposits, which form its cone. These deposits have been likened in appearance to a castle. When the geyser was given this name in 1870, the top edges of the structure resembled the typical profile associated with the modern concept of a castle, having the appearance of a large keep, multiple turrets, and especially because of the crenellation along the top edges of what resembled its towers. As the drawing below shows the cone had distinctive appearance at the time. Over time the cones shape changes because of the layers of mineral deposited in successive eruptions.

Chromatic Spring

Chromatic Spring is a hot spring in the Upper Geyser Basin of Yellowstone National Park in the United States. It is connected to the nearby Beauty Pool. When the water level in one of the two pools rises and overflows, the water level in the other decreases. These fluctuations in water level take place over periods ranging from a few weeks to several years. During this energy shift, the temperatures can change about 10 °F . Its temperature ranges from 164 to 175 °F .

Giant Geyser

Giant Geyser is a cone-type geyser in the Upper Geyser Basin of Yellowstone National Park in the United States. Giant Geyser is the namesake for the Giant Group of geysers, which includes Bijou Geyser, Giant Geyser, and Mastiff Geyser. Giant Geyser is also the namesake for the Giant Platform, a raised stone structure incorporating all these geysers. Giant is notable for its spectacular, but sporadic eruptions, as well as for its very large cone of geyserite, which stands about 12 feet tall.

Steamboat Geyser

Steamboat Geyser, in Yellowstone National Parks Norris Geyser Basin, is the worlds tallest currently-active geyser. During major eruptions, water may be thrown more than 300 feet into the air. Steamboats major eruptions last from 3 to 40 minutes, and are followed by powerful jets of steam. Steamboat does not erupt on a predictable schedule, with recorded intervals between major eruptions ranging from four days to fifty years. The geyser was dormant from 1911 to 1961. Minor eruptions of 10 to 15 feet are much more frequent. After an eruption, the geyser often vents large amounts of steam for up to 48 hours. Cistern Spring, located nearby, will drain completely during a major eruption of the geyser; the spring refills within a few days. Prior to 1904, Waimangu Geyser, in New Zealand, had some taller eruptions capable of reaching 1,600 feet but in 1904 a landslide changed the local water table and since then Waimangu has not erupted. Excelsior Geyser in Yellowstones Midway Geyser Basin likewise was taller, with eruptions reaching 300 feet . However, Excelsior has not erupted since 1985, and is now classified as a hot spring. The last eruption of Steamboat Geyser occurred on 3 September 2014. The last nine major eruptions were on the following dates: October 2, 1991 May 2, 2000 April 26, 2002 September 13, 2002 March 26, 2003 April 27, 2003 October 22, 2003 May 23, 2005 July 31, 2013 September 3, 2014 Steamboat Geyser has two vents, a northern and a southern, approximately five meters apart.

Overhanging Cliff

Overhanging Cliff is a cliff of vertical basalt that overhangs the Grand Loop Road just north of Tower Fall on the north rim of the Grand Canyon of the Yellowstone in Yellowstone National Park. The point was most likely named by a member of the Cook–Folsom–Peterson Expedition, David Folsum in 1869.

Mammoth Hot Springs

Mammoth Hot Springs is a large complex of hot springs on a hill of travertine in Yellowstone National Park adjacent to Fort Yellowstone and the Mammoth Hot Springs Historic District. It was created over thousands of years as hot water from the spring cooled and deposited calcium carbonate . Because of the huge amount of geothermal vents, travertine flourishes. Although these springs lie outside the caldera boundary, their energy has been attributed to the same magmatic system that fuels other Yellowstone geothermal areas. The hot water that feeds Mammoth comes from Norris Geyser Basin after traveling underground via a fault line that runs through limestone and roughly parallel to the Norris-to-Mammoth road. The limestone from rock formations along the fault is the source of the calcium carbonate. Shallow circulation along this corridor allows Norris superheated water to slightly cool before surfacing at Mammoth, generally at about 170 °F . Algae living in the warm pools have tinted the travertine shades of brown, orange, red, and green. Thermal activity here is extensive both over time and distance. The thermal flows show much variability with some variations taking place over periods ranging from decades to days. Terrace Mountain at Mammoth Hot Springs is the largest known carbonate-depositing spring in the world. The most famous feature at the springs is the Minerva Terrace, a series of travertine terraces. The terraces have been deposited by the spring over many years but, due to recent minor earthquake activity, the spring vent has shifted, rendering the terraces dry. The Mammoth Terraces extend all the way from the hillside, across the Parade Ground, and down to Boiling River. The Mammoth Hotel, as well as all of Fort Yellowstone, is built upon an old terrace formation known as Hotel Terrace. There was some concern when construction began in 1891 on the fort site that the hollow ground would not support the weight of the buildings. Several large sink holes can be seen out on the Parade Ground. This area has been thermally active for several thousand years. The Mammoth area exhibits much evidence of glacial activity from the Pinedale Glaciation. The summit of Terrace Mountain is covered with glacial till, thereby dating the travertine formation there to earlier than the end of the Pinedale Glaciation. Several thermal kames, including Capitol Hill and Dude Hill, are major features of the Mammoth Village area. Ice-marginal stream beds are in evidence in the small, narrow valleys where Floating Island Lake and Phantom Lake are found. In Gardner Canyon one can see the old, sorted gravel bed of the Gardner River covered by unsorted glacial till.

Yellowstone Lake

Yellowstone Lake is the largest body of water in Yellowstone National Park. The lake is 7,732 feet above sea level and covers 136 square miles with 110 miles of shoreline. While the average depth of the lake is 139 ft, its greatest depth is at least 390 ft . Yellowstone Lake is the largest freshwater lake above 7,000 ft in North America. In winter, ice nearly 3 ft thick covers much of the lake except where shallow water covers hot springs. The lake freezes over by early December and can remain frozen until late May or early June.

Fishing Bridge Museum

The Fishing Bridge Museum is one of a series of "trailside museums" in Yellowstone National Park, Wyoming, USA, designed by architect Herbert Maier in a style that has become known as National Park Service Rustic. It is one of three parts of a 1987-declared National Historic Landmark, the Norris, Madison, and Fishing Bridge Museums. It seems not to have been listed separately on the National Register of Historic Places as the other two were. Built in 1931, the Fishing Bridge Museum is the largest in the series, and is used as a small visitor center. The museum displays stuffed mounts of birds and animals found in Yellowstone Park.

Madison Museum

The Madison Museum is one of a series of "trailside museums" in Yellowstone National Park designed by architect Herbert Maier in a style that has become known as National Park Service Rustic. It was listed on the National Register of Historic Places in 1982, and is one of three parts of a 1987-declared National Historic Landmark, the Norris, Madison, and Fishing Bridge Museums. Built in 1929, the Madison Museum is the smallest of the three. It is sited on a small rise that overlooks the meadows and canyon of the Madison River, and still fulfills its function as an informal interpretive center.

Specimen Ridge

Specimen Ridge, el. 8,379 feet is an approximately 8.5-mile ridge along the south rim of the Lamar Valley in Yellowstone National Park. The ridge separates the Lamar Valley from Mirror Plateau. The ridge is oriented northwest to southeast from the Tower Junction area to Amethyst Mountain. The ridge is known for its abundance of amethyst, opal and petrified wood. It was referred to as Specimen Mountain by local miners and was probably named by prospectors well before 1870. The south side of the ridge is traversed by the 18.8-mile Specimen Ridge Trail between Tower Junction and Soda Butte Creek. The trail passes through the Petrified Forest and over the summit of Amethyst Mountain el. 9,614 feet .

Yellowstone Caldera

The Yellowstone Caldera is the volcanic caldera and supervolcano located in Yellowstone National Park in the United States, sometimes referred to as the Yellowstone Supervolcano. The caldera and most of the park are located in the northwest corner of Wyoming. The major features of the caldera measure about 34 by 45 miles . The caldera formed during the last of three supereruptions over the past 2.1 million years: the Huckleberry Ridge eruption 2.1 million years agothe Mesa Falls eruption 1.3 million years ago and the Lava Creek eruption 640,000 years ago .

Clagett Butte

Clagett Butte el. 8,041 feet is a mountain peak butte in the Gallatin Range in Yellowstone National Park. Clagett Butte is an isolated summit 1.9 miles west of Mammoth Hot Springs between Clematis Creek and Snow Pass. The Snow Pass trail passes approximately .33 miles south of the butte. Clagett Butte was named in 1926 by park photographer Jack Ellis Haynes and then superintendent Horace Albright to honor William H. Clagettthe Montana Territorial Delegate who put forth the Act of Dedication bill in Congress to create Yellowstone National Park. Prior to 1926, the butte had several different names. In 1885, park guide G. L. Henderson called it Temple Mountain. That was the accepted local name for many years. In 1887, members of the Arnold Hague geological survey called it Sentinel Butte and later in 1897, Signal Butte but these names never became official.

Norris Geyser Basin Museum

The Norris Geyser Basin Museum, also known as Norris Museum or Norris Comfort Station, is one of a series of "trailside museums" in Yellowstone National Park designed by architect Herbert Maier in a style that has become known as National Park Service Rustic. It is listed on the National Register of Historic Places, and is one of three parts of a National Historic Landmark, the Norris, Madison, and Fishing Bridge Museums, which were funded by Laura Spelman Rockefellers grant of $118,000. Built 1929 1930, the Norris Museum is sited on a hill between the Porcelain Basin and the Back Basin of Norris Geyser Basin. Its central breezeway frames a view of the Porcelain Basin for arriving visitors. The 94-foot by 20-foot museum consists of two rectangular sections divided by the breezeway, which is roofed by a prominent jerkinhead gable., framed in massive logs. The pavilions to either side are of shingle-coveredframe construction on a massive stone base. A stone and concrete terrace surrounds the building. A nearby comfort station or toilet is included in the National Register nomination. It was probably built in the 1930s. With the construction of a modern facility the one story log structure is now used as a bookstore operated by the Yellowstone Association. The museum exhibits focus on geothermal geology, features of Norris Geyser and plant and animal life in thermal areas.

Amethyst Mountain

Amethyst Mountain, el. 9,609 feet is the highest peak and central part of a northwest – southeast trending ridge that lies between the Lamar River to the northeast and Deep Creek to the southwest within Park County, Wyoming. From northwest to southeast, this ridge consists of Specimen Ridge, Amethyst Mountain, and the Mirror Plateau in Yellowstone National Park. The nearest town is Silver Gate, Montana, which is 19.2 miles away. In 1872, it was named Amethyst Mountain by the United States Geological Survey for amethysts found on its summit. This mountain is known for its abundance of amethyst, opal and exposures of well known and visited petrified forests. The summit of Amethyst Mountain is traversed by Specimen Ridge Trail, which also traverses the south side of Specimen Ridge between Tower Junction and Soda Butte Creek and through the Yellowstone Petrified Forest.

Francs Peak

Francs Peak is the highest point in the Absaroka Range which extends from north central Wyoming into south central Montana, in the United States. It is located in the Washakie Wilderness of Shoshone National Forest, and the peak is also the highest point in Park County, Wyoming, which includes much of Yellowstone National Park. It was named after Otto Franc, a cattle baron and homesteader in the Big Horn Basin.

Mystic Falls

Mystic Falls is a 70-foot cascade type waterfall on the Little Firehole River, a tributary of the Firehole River. Originally named Little Firehole Falls by members of the 1872 Hayden Geologic Survey, the name was changed to Mystic Falls by members of the Arnold Hague Geological Survey in 1885 for unknown reasons. Mystic Falls is reached via the 1.2 miles Mystic Falls Trail which starts at Biscuit Basin in the Upper Geyser Basin.

Tower Fall

Tower Fall is a waterfall on Tower Creek in the northeastern region of Yellowstone National Park, in the U.S. state of Wyoming. Approximately 1,000 yards upstream from the creeks confluence with the Yellowstone River, the fall plunges 132 feet . Its name comes from the rock pinnacles at the top of the fall. Tower Creek and Tower Falls are located approximately three miles south of Roosevelt Junction on the Tower-Canyon road.

Union Falls

Union Falls ht. 250 feet is a waterfall on Mountain Ash Creek, a tributary of the Fall River in the Cascade Corner of Yellowstone National Park. It is the second highest waterfall in Yellowstone exceeded in height only by the lower Yellowstone Falls. The falls got its name from members of the Arnold Hague Geological Surveys sometime between 1884-86. Geologist J.P. Iddings claims the name derives from the fact that a tributary of Mountain Ash Creek joins at the very brink of the falls, thus Union Falls. Access to the falls is via the Mountain Ash Creek trail and the Grassy Lake Road.

Old Faithful Inn

The Old Faithful Inn is a hotel located in Yellowstone National Park, Wyoming, United States, with a clear view of the renowned Old Faithful Geyser. The Inn features a multi-story log lobby, flanked by long frame wings containing guest rooms. With its spectacular log and limb lobby and massive stone fireplace, the inn is a prime example of the "Golden Age" of rustic resort architecture, a style which is also known as National Park Service Rustic. It is also unique in that it is one of the few log hotels still standing in the United States. It was the first of the great park lodges of the American west. Initial construction was carried out over the winter of 1903-1904, largely using locally obtained materials including lodgepole pine and rhyolite stone. When the Old Faithful Inn first opened in the spring of 1904, it boasted electric lights and steam heat. The structure is the largest log hotel in the world; possibly even the largest log building in the world. In 2007 the American Institute of Architects conducted a survey to determine the 150 favorite buildings in America; the Old Faithful Inn ranked 36. The Inn, which was designated a National Historic Landmark in 1987, is itself part of the Old Faithful Historic District. Old Faithful Inn is a member of Historic Hotels of America, the official program of the National Trust for Historic Preservation.

Isa Lake

Isa Lake is located in Yellowstone National Park, in the U.S. state of Wyoming. The lake straddles the continental divide at Craig Pass and was first discovered in 1891 by Hiram M. Chittenden, who was exploring the best routes for a road to connect Old Faithful and West Thumb geyser basins. Chittenden named the lake after Miss Isabel Jelke, from Cincinnati, though it is not clear why. Isa Lake is believed to be the only natural lake in the world which drains to two different oceans backwards. The east side of the lake drains by way of the Lewis River to the Pacific Ocean and the west side of the lake drains by way of the Firehole River to the Atlantic Ocean. This is the opposite of what one would expect since the Atlantic Ocean is east of the lake and the Pacific Ocean is to the west. The lake is easy to visit as it is adjacent to the road that now connects the Old Faithful and West Thumb geysers basins, on what is known as the "lower loop" of the figure-eight roadway which traverses through Yellowstone.

Shoshone Lake

Shoshone Lake is a backcountry lake with the area of 8,050 acres elevated at 7,795 feet in the southwest section of Yellowstone National Park, Wyoming, US. It lies at the headwaters of the Lewis River a tributary of the Snake River. The U.S. Fish and Wildlife Service believes that Shoshone Lake is the largest backcountry lake in the lower 48 states that cannot be reached by a road.

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Top Attractions in Yellowstone National Park

Upper Geyser Basin

Lower Geyser Basin

Midway Geyser Basin

Grand Canyon of the Yellowstone

Norris Geyser Basin

Lake Fish Hatchery Historic District

Old Faithful Historic District

Old Faithful

Grand Prismatic Spring

Castle Geyser

Chromatic Spring

Giant Geyser

Steamboat Geyser

Overhanging Cliff

Mammoth Hot Springs

Yellowstone Lake

Fishing Bridge Museum

Madison Museum

Specimen Ridge

Yellowstone Caldera

Clagett Butte

Norris Geyser Basin Museum

Amethyst Mountain

Francs Peak

Mystic Falls

Tower Fall

Union Falls

Old Faithful Inn

Isa Lake

Shoshone Lake

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