Mohorovicic discontinuity (pronounced moh-haw-roh-vuh-chich), more commonly known as the "Moho," is the geological term that describes the boundary zone between Earth's crust and the lower-lying mantle. Its discovery was critical to scientists because it was the first time anyone conceived that...
The Earth is layered below its surface. At the top is the crust. Below that, there's the mantle, and below that, the outer and inner cores. There are other regions, too, like the Moho barrier. Answer and Explanation:1 The Moho barrier, otherwise known as the Mohorovicic Discontinuity, ...
This was the space race’s geological counterpart, the contest to drill the deepest possible hole into the Earth. The US broke ground (both literally and metaphorically) in 1961 with “Project Mohole”, which aimed to collect samples from the Mohorovičić (Moho) discontinuity, the boundary ...
A fault is a planar breakage/discontinuity in the Earth's crust where there is significant/recognizable vertical and/or horizontal movement or displacement of the rock units. Answer and Explanation:1 Horizontal compressive force causes a thrust fault. This is illustrated in the following figure where...
English Definition Moho (aka Mohorovičić discontinuity, the lower boundary of the earth's lithosphere) Simplified Script 莫霍面 Traditional Script Same Pinyin mò huò miàn Effective Pinyin (After Tone Sandhi) Same Zhuyin (Bopomofo) ㄇㄛˋ ㄏㄨㄛˋ ㄇㄧㄢˋ Cantonese (Jyutping) mok6 fok...
The earth's tectonic plates are found in the lithosphere which is an area that incorporates the crust and the uppermost part of the mantle. Between the crust and the mantle is a region called the Mohorovicic Discontinuity, known for short as the Moho. Under the lithosphere is a softer more...
The mantle, which makes up about 84% of Earth's volume, is predominantly solid, but behaves as a very viscous fluid in geological time. The upper mantle, which starts at the "Mohorovicic Discontinuity" (aka. the "Moho" – the base of the crust) extends from a depth of 7 to 35 km ...
This remark seems so obvious that I can't find any description neither analysis about this phase transition. If we look under our feet, there is no problem, we can find the moho' discontinuity at 35km, the gutenberg discontinuity at 2885km, etc... Same if we look over us, there is ...
Here we present an integrated analysis of geophysical and geological data to show how these processes can act contemporaneously and in close proximity to each other, along a lithosphere scale discontinuity that defines the lateral boundary between the Hellenide and Anatolide segments of the Tethyan ...
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