1, Chahan Yan volcano group: 1795, 1820 erupted twice
2, Ga Cong volcano group
3, Gan volcano group
4, sand bald volcano group
5, Kolo volcano group
6, Wudalianchi volcano: the old Montenegro, fire burning for the 1719/1721 eruption
7, Jianshan volcanic group
8, two grams of volcanic groups
9, Yimin River - Moke River Volcanic Group
10, Aershan volcanic group
11, Jiamusi - Shuangyashan volcano group
12, Jixi volcanic group
13, Changbai Mountain volcano: Mount Baishan 1597, 1702, two eruption
14, Longgang volcano group
15, Kuandian volcano group
16, Yitong volcanic group
17, Fan Jiatun volcano group
18, Shuangliao volcano group
19, up to Norr volcanic group
20, Abaga mountain volcano group
21, Ulan Hada volcano group
22, check right before the flag volcano group
23, Datong volcano group
24, the eastern sea volcano: 1916, 1921 erupted twice
25, Datun volcano group
26, Leizhou Peninsula volcano group
27, north of Hainan Island volcano
28, Tengchong volcanic group
29, Caldash volcano: 1951 eruption
Geothermal Resources in China
Volcanoes and Lava
Volcanic cone, after the Pliocene karst, before the Pliocene karst
spa
Intermittent fountain, boiling spring, hot springs, hot springs
Energy is a resource that can provide useful energy for mankind, either directly or through conversion. Nuclear fusion and nuclear fission radioactive sources and planets in the solar system is the world's initial source of all energy. The sun's thermonuclear screenings emit huge amounts of energy, and the sun's radiant energy reaching the Earth's atmosphere reaches 36.02 million tons of standard coal annually, which in turn provides an inexhaustible source of energy for the planet and space, the thermal effects of solar energy In the atmosphere, soil and marine interface between the three generate wind energy, wave energy and ocean kinetic energy. Coal, oil, natural gas and other fossil fuels are indirectly derived from solar energy. Plants absorb solar energy through photosynthesis into biomass, the solar system's planetary tidal energy generation. Geothermal energy in the Earth's bedrock enters the atmosphere and ocean through heat conduction. Volcanic or geothermal geothermal field activities can be through the convection into the surrounding environment.
| Ground temperature and its code | Average Temperature | Maximum ground Temperature |
| China 's eastern region | ||
| ① Songliao Basin | 40~50 | 60~70 |
| ② North China Basin | 40~50 | 60~70 |
| ③ southeast coastal areas | 40~50 | 60~70 |
| ④ Subei Basin | 40~50 | 45~60 |
| ⑤ Taiwan region | 40~50 | 45~60 |
| ⑥ Poyang Lake Basin | 40~50 | 60~70 |
| ⑦ Yunmeng basin | 40~50 | 60~80 |
| ⑧ Nanyang basin | 40~50 | 50~60 |
| Mountain | 25~50 | 50~60 |
| China 's central region | ||
| ⑨ Hulunbeier - Erlian Basin | 35~45 | 50~60 |
| ⑩ Ordos Basin | 35~40 | 50~60 |
| ⑪ Fenwei Basin | 35~45 | 50~60 |
| ⑫ Sichuan Basin | 35~45 | 50~60 |
| ⑬ Baise Basin | 40~45 | 50~60 |
| ⑭ Nanpanjiang Basin | 40~45 | 50~60 |
| ⑮ Kunming - Liupanshui Basin | 40~45 | 40~50 |
| ⑯ Lanzhou - Xining basin | 35~45 | 40~50 |
| Mountain | 25~30 | 40~50 |
| China 's western region | ||
| ⑰ Tibetan Yunnan region | 40~50 | 70~80 |
| ⑱ Qaidam Basin | 35~45 | 50~60 |
| ⑲ Hexi Corridor | 35~40 | 50~60 |
| ⑳ Turpan-Hami Basin | 25~40 | 40~50 |
Comment list ( 0 )
