Craters of the Moon

La surface est inégale, il y a un état de la surface de la lune, et il y a parfois un chaud terrestre. La Nouvelle-Zélande est riche en géologie, et il est un bon endroit pour la surface de la lune!

Il est allé à 1.5, plus longtemps que d'autres expériences géothermiques dans la région de Liubo. Cependant, il est facile de marcher sur un large pilier de bois. Il y a beaucoup d'aéronefs à vapeur et de plusieurs volcans, dont deux bassins de chauffage. Il y a une route de 120 pas pour faire une tournée car je n'ai pas bien couché. Compte tenu de 8 dollars seulement, c'est très précieux.

A privately operated geothermal park, the taste is relatively large, personal feeling is particularly interested in geomorphology and other geology can be visited, it seems that the general feeling is not too interesting, after all, that is, smoke on the ground, the taste is also particularly strong.

Le paysage est unique ici, le paysage est unique ici

$10NZ entry fee and it’s about 45 minutes to walk around the whole track.

Digu Ring Mountain is one of the most observed Ring Mountains, with a diameter of about 85 kilometers and a depth of about 4850 meters. At the bottom of the crater there are complex central peaks, up to 1600 meters. The Tycho Ring is 51 miles (82 kilometers) in diameter, visible to the naked eye on Earth, but in fact it is the target of many astronomers. In 1968, the U.S. "Surveyor" 7 lunar probe captured some radiation patterns in the Tycho Ring Mountain. There are 12 radiation patterns in the Tycho Ring Mountains. They pass through mountains, moon valleys and the Moon Sea. The longest one is 1800 kilometers long and the widest one is 20 kilometers wide. Most scientists believe that rocks and rock powders are thrown around when volcanic eruptions or large meteorites strike the surface of the moon. Later, these substances gradually fell back to the moon and became radiation lines. Because of their high albedo, they look particularly bright.