GOJIRA - Magma

About Magma by GOJIRA Album

Magma is the sixth studio album from French metal band Gojira. The album was recorded at the band's studio in New York City, and was produced by Joe Duplantier, mixed by Johann Meyer, and mastered by Ted Jensen. The album sold almost 17,000 copies in its first week of release in the United States, charting at number 24 on the Billboard 200, making Magma the band's highest sales and chart debut to date. The album has been noted as a stylistic departure from the band's previous albums, featuring a more accessible atmospheric sound and more prominent use of clean vocals. Magma was inspired in part by the death of Joe and drummer Mario Duplantier’s mother, who passed away during the LP’s recording sessions. “The songs were half-written while she was sick,” Joe told Rolling Stone in an in-depth interview. “After she died, I still had to finish them. So one song was like, ‘You’re going to make it,’ but the second verse is ‘You didn’t make it.'” “When you read Joe’s lyrics, for me, I cry right away,” Mario said. “They’re very deep and to the point. No bullshit. We recycle our sadness and depression in the music.”

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Magma (GOJIRA) Album Songs

NoSong TitleTime
1.The Shooting Star 5:42
2.Silvera 3:32
3.The Cell 3:17
4.Stranded 4:29
5.Yellow Stone 1:19
6.Magma 6:42
7.Pray 5:13
8.Only Pain 3:59
9.Low Lands 6:03
10.Liberation 3:35

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Magma [GOJIRA] Album Reviews

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Magma Wiki

Magma (from Ancient Greek μάγμα (mágma) 'thick unguent') is the molten or semi-molten natural material from which all igneous rocks are formed. Magma (sometimes colloquially but incorrectly referred to as lava by laypeople) is found beneath the surface of the Earth, and evidence of magmatism has also been discovered on other terrestrial planets and some natural satellites. Besides molten rock, magma may also contain suspended crystals and gas bubbles. Magma is produced by melting of the mantle or the crust in various tectonic settings, which on Earth include subduction zones, continental rift zones, mid-ocean ridges and hotspots. Mantle and crustal melts migrate upwards through the crust where they are thought to be stored in magma chambers or trans-crustal crystal-rich mush zones. During magma's storage in the crust, its composition may be modified by fractional crystallization, contamination with crustal melts, magma mixing, and degassing. Following its ascent through the crust, magma may feed a volcano and be extruded as lava, or it may solidify underground to form an intrusion, such as a dike, a sill, a laccolith, a pluton, or a batholith. While the study of magma has relied on observing magma after its transition into a lava flow, magma has been encountered in situ three times during geothermal drilling projects, twice in Iceland (see Use in energy production) and once in Hawaii.

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