就是精品 || 不超过13人小团 | 盐湖城进出+杰克逊+大提顿国家公园+黄石国家公园+大盐湖 5日游Juicy Premium || Small Group (Maximum 13 People) | 5-Day Tour of Salt Lake City, Jackson, Grand Teton National Park, Yellowstone National Park, and the Great Salt Lake

A 10-minute ride on the Jackson Hole Sky Tramway takes you to a height of 4,139 feet, a journey like a journey through the clouds. Upon reaching the summit, you'll enjoy breathtaking 360-degree views of the Teton Range, Jackson Hole Valley, and the surrounding mountains. As the ride continues, the scenery becomes more breathtaking with each second. Once you reach the summit, you'll feel like you're on top of the world!

The park is not big, but there are giant arches made of deer antlers in the four directions of east, west, south and north. The antlers are all sharp, but they are not obtained by hunting. Every winter, a large number of elk come from the mountains to the "National Elk Refuge" in Jackson to spend the winter. In the spring, the antlers fall off naturally and are replaced. After the elk leave, countless treasures are left everywhere.

Grand Teton National Park was established on February 26, 1929. There are 300 kilometers of trails in Grand Teton National Park. There are many lakes in the park, including Jackson Lake and Jenny Lake. Most of the area of Grand Teton National Park is located in the Rocky Mountains, and the natural scenery is very magnificent. In addition, Grand Teton National Park also has extremely rich biological resources, including American bison, grizzly bears, black bears, moose, etc.

Jenny Lake is located in Grand Teton National Park, Wyoming, USA. The lake was formed approximately 12,000 years ago when glaciers pushed rock debris into the Cascades Canyon during the Last Glacial Maximum, creating the terminal moraine that now blocks the lake. The lake is estimated to be 256 feet deep and covers 1,191 acres. Jenny Lake is one of the most visited areas in Grand Teton National Park. Nestled at the foot of the Teton Mountains, it is the heart of the park. From its east shore, visitors can overlook Mount Tevinot, Mount St. John, and the Cascades Canyon. From its west shore, visitors can gaze back across the lake towards the Jackson Hole Valley.

Jackson Lake is a 400-foot-deep natural lake with a dam built on top. The original woodpile dam, built in 1906-07, failed in 1910. In 1916, the Bureau of Reclamation built a concrete dam, raising the lake level by 39 feet. The rising waters flooded the surrounding forest, killing many trees. During the Great Depression, young men from the Civilian Conservation Corps helped clear the shores of Jackson Lake and burn the woodpile. Today, you can enjoy beautiful views of Jackson Lake from the Jackson Lake Dam Overlook.

Located in the Rocky Mountains, known as the "backbone of America", it is located on the lava plateau between the Northern Rockies and the Central Rockies in the western United States. The geothermal wonders are its hallmark, a primitive landscape of the earth forged by water and fire. The natural landscape in the park is divided into five major areas, namely the Mammoth Area, the Roosevelt Area, the Canyon Area, the Geyser Area and the Lake Area, each with its own characteristics. It exceeds the limits of human art and is the most wonderful and spectacular scenery on the surface of the earth.

The West Thumb Geyser Basin, located on the edge of Yellowstone Lake, was formed 150,000 years ago by the collapse of the earth's crust. The combination of hot springs and lake water has created a wonderful misty landscape: the misty area is the steam of hot springs, and the green waves are the water of Yellowstone Lake, which complements the blue sky and white clouds in the background, forming a landscape different from other hot spring areas in Yellowstone. This area is equivalent to the bay of Yellowstone Lake, where many geysers gather. The colors of the water outlets vary, some are transparent green, and some are dark black like cement. Many water outlets present a beautiful fantasy.

Hayden Valley is located on the edge of the Yellowstone crater. It is an open grassland with relatively little geothermal activity. Because of the river passing through it, the grass and water are lush, so it is one of the areas with more wild animals in Yellowstone Park. The main animals are bison, elk, black bears, brown bears and coyotes. Wild ducks, pelicans and other birds can often be seen in the Yellowstone River. There are viewing points on the roadside, and many tourists often use binoculars to watch animals.

Located in the Rocky Mountains, known as the "backbone of America", it is located on the lava plateau between the Northern Rockies and the Central Rockies in the western United States. The geothermal wonders are its hallmark, a primitive landscape of the earth forged by water and fire. The natural landscape in the park is divided into five major areas, namely the Mammoth Area, the Roosevelt Area, the Canyon Area, the Geyser Area and the Lake Area, each with its own characteristics. It exceeds the limits of human art and is the most wonderful and spectacular scenery on the surface of the earth.

The Upper Falls is located 400 meters upstream of the larger Yellowstone Falls. The waterfall falls vertically along the volcanic cliff with a drop of 33 meters. The originally uneven volcanic rocks below the waterfall have been eroded by the waterfall for hundreds of years and have become very smooth.

No other destination in Yellowstone gives you a greater opportunity to see wild bison than Lamar Valley. The Lamar River feeds a wide grassy valley, drawing the massive grazers to the northeast corner of Yellowstone National Park. In addition to bison, Lamar Valley is also renown for its gray wolf population. These crafty creatures are harder to spot than the big bison, but you’ll have a better chance of spotting one around sunrise and sunset.In addition to bison and wolves, you can see elk, pronghorns, and even grizzlies in Lamar Valley. Fishing in the Lamar River is another popular activity in Lamar Valley. 

There were originally several hot springs flowing down the hillside, and the hillside was dyed colorful by the microorganisms in the spring water, forming a colorful large staircase. However, due to a crustal movement in 2002, most of the hot springs here are no longer active. The microorganisms turned into grayish white powder after death, which remained on the dry large staircase, reflecting the dazzling sunlight, turning this place into a solemn and barren land. With the movement of the crust, a place that was once very active may suddenly become quiet; a place that was originally unknown may also become a sensation.

The Palette Geyser is a mud spring, a type of acidic hot spring containing limited water. Underground acidic gases and microorganisms break down the rocks surrounding the pores into clay and volcanic mud. Like boiling water bubbling mud, the thicker the mud, the higher the steam pressure underneath, and the greater the eruption. The Palette Geyser displays colors such as pale pink, milky white, and cyan due to the different minerals released from the rocks, and its bubbling appearance is further enhanced by geothermal activity. Its circumference is approximately 20 meters, and it is surrounded by railings to prevent visitors from getting too close and potentially causing danger.

Also known as the Seven Color Pool, it is the largest hot spring in the United States and the third largest in the world. It is 75-91 meters wide and 49 meters deep, and it gushes out about 2,000 liters of 71-degree hot water every minute. The amazing thing about the Grand Prismatic Spring is that the color of the lake changes with the seasons. In spring, the lake changes from emerald green to golden orange-red, which is due to the algae and pigment-containing bacteria and other microorganisms living in the mineral-rich water. In midsummer, the chlorophyll content is relatively low, so the lake water appears brilliant orange, red or yellow. But in the cold winter, due to the lack of light, these microorganisms will produce more chlorophyll to suppress the color of carotenoids, so the water will appear deep dark green.

Old Faithful geyser is named for its consistent and regular eruption. Currently, it erupts approximately every 60 to 110 minutes, and each eruption lasts four to five minutes. The water column is more than 40 meters high, which is spectacular and never stops. The Old Faithful Visitor Center will display the eruption schedule in advance, so you can check the eruption time in advance before visiting with confidence.

Located in the Rocky Mountains, known as the "backbone of America", it is located on the lava plateau between the Northern Rockies and the Central Rockies in the western United States. The geothermal wonders are its hallmark, a primitive landscape of the earth forged by water and fire. The natural landscape in the park is divided into five major areas, namely the Mammoth Area, the Roosevelt Area, the Canyon Area, the Geyser Area and the Lake Area, each with its own characteristics. It exceeds the limits of human art and is the most wonderful and spectacular scenery on the surface of the earth.

Norris Geyser Basin, named after an early Yellowstone Superintendent, may be the hottest geyser basin in Yellowstone. The stark, barren landscape of Porcelain Basin is the result of the acidic environment. Due to the hostile condition plants, algae and bacteria have difficulty in establishing themselves. Instead, the basin derives its colors from mineral oxides, in spectrums of pink, red, orange (iron oxides) and yellow (sulfur and iron sulfates). The largest geyser in the world is located here. Steamboat Geyser has long periods of dormancy, but when it does erupt it sends jets of water nearly 380 feet high in a spectacular display.

The Morning Glory Pond exhibits a variety of colors due to the thermophilic bacteria living within it. Decades ago, the pond displayed a unique blue hue. However, as tourists frequently tossed coins into the pond for good luck, debris clogged the spring's source, lowering the water temperature and leading to the proliferation of various bacteria and algae. Currently, the central part of the pond is green, surrounded by a yellow hue. The water is emerald green, crystal clear, and edged with orange-yellow rims. The spring water contains various metal ions, which, under low-angle light, make the clear water appear even more azure, and the golden-yellow outer edge even more vibrant, resembling a blooming morning glory flower. Hence, it is named the Morning Glory Pond.

Yellowstone Park Bear World is located in Rexburg, Idaho. It was built in 1998 and is the only wildlife sanctuary in Greater Yellowstone that can be driven through. The park offers rare animals for visitors to see, such as grizzly bears, black bears, gray wolves and other precious North American animals. It is said that there are nearly 100 grizzly bears. There are also shops, tour guides and performances such as feeding bears and other small animals.

The Utah State Capitol is the house of government for the U.S. state of Utah. The building houses the chambers and offices of the Utah State Legislature, the offices of the Governor, Lieutenant Governor, Attorney General, the State Auditor and their staffs. The capital is the main building of the Utah State Capitol Complex, which is located on Capitol Hill, overlooking downtown Salt Lake City. The Neoclassical revival, Corinthian style building was designed by architect Richard K.A. Kletting and built between 1912 and 1916. The building was added to the National Register of Historic Places in 1978.

Temple Square is a 10-acre (4.0 ha) complex, owned by The Church of Jesus Christ of Latter-day Saints (LDS Church), in the center of Salt Lake City. Contained within Temple Square are the Salt Lake Temple, Salt Lake Tabernacle, Salt Lake Assembly Hall, the Seagull Monument, and two visitors' centers. The square was designated a National Historic Landmark District in 1964, recognizing the Mormon achievement in the settlement of Utah.

Great Salt Lake, lake in northern Utah, U.S., the largest inland body of salt water in the Western Hemisphere and one of the most saline inland bodies of water in the world. The lake is fed by the Bear, Weber, and Jordan rivers and has no outlet. The lake has fluctuated greatly in size, depending on the rates of evaporation and the flow of the rivers that feed it. Like the Dead Sea, the Great Salt Lake exists within an arid environment and has chemical characteristics like that of the oceans. However, it has a much greater salinity than the oceans, since natural evaporation exceeds the supply of water from the rivers feeding the lake.