Mammoth Hot Springs is a collection of thermal features at the north entrance of Yellowstone National Park. It is best known for the travertine terraces that form from mineral deposits, but there are many other observable geothermal features in this area. The algae living in the pools creates the distinct brownish, reddish colors. Our safari makes a stop here. Your guide will educate you on the historical or geological significance of your stop.

A petrified redwood seems out of place in present day Yellowstone National Park, but millions of years ago, this area looked much different. Petrified trees, such as this are a natural relic of a volcanic past. Our safari makes a stop here. Your guide will educate you on the historical or geological significance of your stop.

This picturesque waterfall in the northern region of Yellowstone National Park is named for the rock pinnacles at the brink of the falls. Years of erosion is actually moving the falls slowly upriver, although not fast enough to see it migrate in your lifetime. Our safari makes a stop here. Your guide will educate you on the historical or geological significance of your stop.

The Yellowstone River originates in the Absaroka Range at the Continental Divide and flows north through Yellowstone National Park and Paradise Valley before heading east across the plains of Montana and eventually flowing into the Missouri River. It is a large-volume river, fed by several tributaries on its journey eastward. The river provides habitat for many species in the Greater Yellowstone Ecosystem and is known for its excellent trout population. Our safari makes a stop here in search of wildlife. Your guide will educate you on the historical or geological significance of your stop.

Slough Creek is a tributary of the Lamar River and originates in the Absaroka Range. The watershed supports a variety of flora and fauna. Our wildlife safari makes multiple stops in the Slough Creek area to track and spot wildlife. Your guide will educate you on the historical or geological significance of your stop.

The Lamar Valley is located in the northeastern region of Yellowstone National Park and is well known for its natural beauty, flora and fauna. Such an abundance of wildlife exists here that it has been dubbed "the Serengeti of North America". Our safari makes several stops here in search of wildlife. Your guide will educate you on the historical or geological significance of your stop.

The Albright Visitor Center, located in the northern region of Yellowstone, is housed in a historic structure that originally served as quarters for cavalry troops charged with protection of the park prior to the creation of the National Park Service. Our safari makes a stop here. Your guide will educate you on the historical or geological significance of your stop.

The Roosevelt Arch, built in 1903, is constructed of hexagonal blocks of columnar basalt and stands 52ft (16m) high. The arch stands at the north entrance to Yellowstone National Park in Gardiner, MT. The original conception was to provide a grand entrance to the world's first National Park but subsequent features were never installed and the official park entrance was relocated south of Gardiner. The arch itself remains standing and is now listed on the National Register of Historic Places. Our safari makes a stop here. Your guide will educate you on the historical or geological significance of your stop.

Yellowstone National Park Entrance Gate - North Entrance

Paradise Valley runs north-south, bordered on the north by the town of Livingston, MT and on the south by Gardiner, MT. The valley lies between the Gallatin Range to the west and the Absaroka Range to the east. It is also a major corridor of the Yellowstone River and is home to diverse flora and fauna as well as geological wonders. Our safari makes a stop here in search of wildlife. Your guide will educate you on the historical or geological significance of your stop.