不超过13人的精品小团 | 旧金山+黄石国家公园+大提顿国家公园+纪念碑谷+羚羊彩穴+拉斯维加斯 7日游Small Group of No More Than 13 Guests | 7-Day Tour across San Francisco, Yellowstone National Park, Grand Teton National Park, Monument Valley, Antelope Canyon and Las Vegas

The California State Capitol Museum consists of a museum in and grounds around the California State Capitol in Sacramento, California, United States. The building has been the home of the California State Legislature since 1869. The State Capitol Museum has been a property in the California State Parks system since 1982.

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.

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 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.

Located in the eastern part of Yellowstone National Park, not far from the northern part of Yellowstone Lake. Most of the fountains here do not spray water, but mud, and every time they erupt, the ground shakes. Next to the mud volcano, there are colorful grasses that look extremely tender and gorgeous.

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.

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.

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.

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.

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.

Canyonlands National Park is an American national park located in southeastern Utah near the town of Moab. The park preserves a colorful landscape eroded into numerous canyons, mesas, and buttes by the Colorado River, the Green River, and their respective tributaries. While these areas share a primitive desert atmosphere, each retains its own character. The Island in the Sky mesa rests on sheer sandstone cliffs towering over 1,000 feet (304 m) above the surrounding terrain. Every overlook offers a different perspective on Canyonlands' spectacular landscape. Island in the Sky is the easiest area of Canyonlands to visit in a short period of time, offering many pullouts with spectacular views along the paved scenic drive.

Arches National Park is located near the town of Moab in Utah, USA. It covers an area of 309 square kilometers and preserves more than 2,000 natural rock arches. About 300 million years ago, this salt layer was an ocean. Millions of years after the sea disappeared, the salt layer was covered by air and water debris, and squeezed into rock with other debris. Later, after the crust uplifted and natural weathering, it became the arches of today. The park not only has arches, but also numerous large and small spires, pedestals, balancing stones and other unique geological features; all the stones have textures with very strong color contrasts.

Monument Valley is a region of the Colorado Plateau characterized by a cluster of vast sandstone buttes, the largest reaching 1,000 ft above the valley floor. It is located on the Arizona–Utah state line, near the Four Corners area. Monument Valley has been featured in many forms of media since the 1930s. Director John Ford used the location for a number of his best-known films and thus, in the words of critic Keith Phipps, "its five square miles [13 square kilometers] have defined what decades of moviegoers think of when they imagine the American West."

Horseshoe Bend – One of the top ten best photography spots in the United States selected by National Geographic Magazine! The dense aquatic plants on the Colorado River bed make the river water appear fluorescent green in the sun. The river turns 360 degrees in the reddish-brown canyon here, cutting out a horseshoe-shaped canyon, hence the name Horseshoe Bend. Standing on the edge of the cliff, you will be intoxicated by the breathtaking beauty of the blue water, blue sky and red rocks.

The Lower Antelope Canyon is located in the north of Arizona, USA. It is formed by soft sandstone after millions of years of various erosion forces. Flash floods often flow into the canyon during the monsoon season. Due to the sudden increase in rainfall, the flow rate of the flash flood is quite fast. In addition, the narrow channel narrows the river channel, so the vertical erosion force is relatively large, forming the corridor at the bottom of the Lower Antelope Canyon and the hard and smooth edges on the valley wall that look like flowing water. There is no artificial lighting in the Lower Antelope Canyon. All visible light comes from the cracks at the top of the canyon. These lights are repeatedly refracted by the rock texture and enter the valley bottom, producing a dreamy and irregular color change. These colors are from deep to light, colorful and beautiful.