Search results
Results from the WOW.Com Content Network
The Highline Trail is a scenic hiking trail in Glacier National Park, Montana, United States. The trail stretches 7.6 miles (12.2 km) from Logan Pass to Granite Park Chalet, and continues another 11.9 miles (19.2 km) from there to Fifty Mountain Campground. The trail follows the Garden Wall ridge
The Garden Wall is a steep alpine area within Glacier National Park well known during the summer months to be heavily covered in dozens of species of flowering plants and shrubs. Located along the west side of the Continental divide and extending northward from Logan Pass , the Garden Wall can be traversed via the popular Highline Trail and for ...
Granite Park Chalet is located in the heart of Glacier National Park in the U.S. state of Montana at an elevation of 6,693 feet above sea level. The chalet was built in 1914 by the Great Northern Railway and is a National Historic Landmark contributing property, being one of five structures in the Great Northern Railway Buildings district.
Highline Trail or High Line Trail may refer to: Highline Trail in Canmore, Alberta, Canada; United States ... Highline Trail (Glacier National Park), in Montana;
The National Park Service announced the incident in a press release Thursday morning, adding that Glacier National Park rangers closed a section of Highline Trail. Officials will keep the closure ...
Glacier National Park is a national park of the United States located in northwestern Montana, on the Canada–United States border.The park encompasses more than 1 million acres (4,100 km 2) and includes parts of two mountain ranges (sub-ranges of the Rocky Mountains), more than 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals.
This is intended to be a complete list of the properties and districts on the National Register of Historic Places in Glacier National Park, United States. The locations of National Register properties and districts for which the latitude and longitude coordinates are included below, may be seen in a Google map.
Like other mountains in Glacier National Park, Haystack Butte Tail is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick, 50 miles (80 km) wide and 160 miles (260 km ...