The Norris Geyser Basin is the most active and longest active geothermal region in North America, and has been around for about115000 years. This is the hottest area in all geothermal resources in Yellowstone, located at the intersection of three fault lines, including the fault line in the Norris-Mammoth corridor and the Hebgen Lake fault line (the fault line from the northwest of Huangshi Town to Norris in Congxi). Studies have shown that temperatures in the Norris area have reached 237 degrees Celsius 300 meters underground. In 2003, the area was also briefly closed due to rising rock temperatures in the surrounding area. Unlike other geyser basins in Yellowstone, geysers in the Norris region are acidic (geysers in other regions are basically alkaline), and different pH values between the springs produce different types of microorganisms, resulting in different surroundings and color of the springs. In addition, the geothermal landscape here will vary with the season. The browsing of the Norris area is mainly divided into two parts, Porcelain Basin and Back Basin. Most tourists will choose the former for browsing, because the distance is relatively short, and the walk down the plank road is only about 1 mile/1.6 kilometers. The Porcelain basin is the hottest place in Yellowstone, and although the water vapor after condensation makes it difficult for me to see the appearance of most geysers, it is easy to tell by sound that some springs are rolling. As I said, Porcelain Basin is the main area for visitors to visit Norris Geyser Basin. But today, most tourists seem to have lost interest in it, and there are only a few people on the boardwalk. Think about it, in such weather, people can see only the layers of water vapor floating, nothing else. Back Basin is more quiet than Porcelain Basin. The full-named about 2 miles/3 kilometers of browsing plank road may be a reason many people give up here, after all, the vast majority of tourists in Yellowstone stay more limited. Back Basin is located in a forest, and in order to see the whole attraction, I still walked the whole journey of Back Basin browsing the plank road in such a weather that is not suitable for browsing the geothermal landscape. After all, it is not easy to come here, and I have time. The geysers in the Back Basin area are mostly “quiet,” but this is only temporary. The Steamboat geysers in the area are the world’s tallest and still active geysers. Unlike the famous Old Faithful Geysers, which erupt frequently, the interval between two large-scale eruptions of Steamboat Geysers is usually long. According to the data, the longest large-scale eruption interval of Steamboat Geysers can be up to 50 years. Once erupting, the geyser can emit water columns up to 90 meters. In the interval between two large eruptions, Steamboat geysers usually have small eruptions, and their water columns can reach about 12 meters. In addition, Echinus Geyser within Back Basin is Yellowstone's largest acid geyser, which used to be very active and erupts every few hours, so it also attracted a lot of tourists. But in recent years, it has been much quieter. To be honest, I had great expectations for the Norris Geyser Basin before I came to Yellowstone, but maybe it was the weather, maybe it was Norris that was visually average here. Although I spent about two and a half hours on the Norris boardwalk, in the end there was too little memory left for me...