Glacier National Park

Established in 1910, Glacier National Park is located in the northern part of the Rocky Mountains, where Montana, USA and British Columbia, Canada meet. The very famous landscape in the park is the third point, which is the meeting point of the various watersheds. The rainfall to the east of the third point will flow from the Gulf of Mexico into the Atlantic Ocean, while the rainfall in the west will flow into the Pacific Ocean, and the rainfall in the north will flow through the Hudson Bay. Arctic Ocean. Due to the greenhouse effect, the glaciers are shrinking greatly, and the small glaciers are gradually disappearing, leaving behind many beautiful mountains and lakes. In addition to the three points, driving along the road of the sun (going-to-the-sunroad) is also a very exciting experience, passing McDonald Lake, Logan Pass and St. Mary Lake along the way, these places The scenery is still breathtaking, and then came to the glaciers (Many Glaciers), surrounded by many glaciers. Glacier National Park is the largest Glacier Glacier in Glacier National Park, covering an area of about 4.8 square kilometers. It is located on the northern slopes of Jackson Mountain and Bradford Mountain at an altitude of 2440 meters. Harrison Glacier and Pumpley Glacier cover the southern slopes. It is also famous for its picturesque peaks. Cleveland Mountain, which is more than 3,000 meters high in the north of the park, is the highest peak. More than 3,000 meters in the park are also Jintra Peak, Xiye Mountain and Siyansen Peak. The ridges here are like sharp knives, and the peaks that have been eroded by glaciers like pyramids, covered with white snow, look particularly enchanting. Ground pressure twists, fractures and tilts the rocks on the peaks, creating an incredible stromatolite geometry. Each rock formation constitutes a platform, often less than 1 meter thick, on which snowflakes accumulate, adorning the entire mountain in black and white stripes.