クレイターズ・オブ・ザ・ムーン

地表の凹凸のある地面は、本当に月の表面の穴のような状態があり、時地熱が出ます。ニュージーランドは地質地形が豊富で、月の地表の撮影にいいところです。

彼は1.5の距離を歩いて、タウポの他の地熱経験よりも少し長いです。それでも、広い木製の歩道を歩くのは簡単です。 2つの泥プールを含む多くの蒸気通気口といくつかのクレーターがあります。膝が悪いので、120歩歩く円の回路があります。チケットは8ドルしかないので、とても価値があります。

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.

ここの景色はこちらがいいです。ここの景色はこちらがいいです。

$10NZ入場料とトラック全体を歩くのに約45分かかります。

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.