Inactive Lava Zone

This seems new This article contains information that is updated for the latest Experimental Version of Subnautica. Players using stable mode may find this information inaccurate.

This article is about the Inactive Lava Zone Corridor. You may be looking for the Inactive Lava Zone, the Lava Lakes, or the Lava Castle.

<infobox layout="stacked">

 <title source="title1">
   <default>Inactive Lava Zone</default>
 </title>
 <image source="image1">

</image> <label>Tab</label> <label>Type</label> <label>Biome</label> <label>Depth Range</label> <label>Temperature Range</label> <label>Biome ID</label> <label>Harvesting Nodes</label> <label>goto ID</label> <label>Coordinates</label> <label>Base ID</label> <group> <label>Point of Interest</label> <label>Music</label> </group> </infobox>The Inactive Lava Zone Corridor is a mini-biome which links the Lost River and Inactive Lava Zone together.

Description

The Inactive Lava Zone Corridors are characterized by large cavernous corridors of hardened lava. Veins of active lava can be found regularly, sometimes ejecting molten boulders. The Corridors continue well below all other biomes and converge into a central chamber. Resources such as Kyanite and Aluminum Oxide Crystals are frequent in this biome which come in useful in Survival.

This Corridor leads to the Inactive Lava Zone, so it serves as the entrance to that particular Biome.

<tabber> Resources=

• Aluminum Oxide Crystal
• Deep Shroom Spore
• Diamond
• Kyanite
• Sulphur

|-| Fauna=

• Lava Larva
• Lava Lizard
• Magmarang
• Red Eyeye
• Warper

|-| Flora=

• Deep Shroom

</tabber>

Gallery

• 

  The Lost River Corridor

• 

  The Inactive Lava Zone Corridor's Resources

• 

  A Lava Fall

• 

  Some Deep Shrooms

• 

  Some Kyanite and other resources

Trivia

• There was once a Corridor that lead to the Deep Grand Reef, this has since been removed in the Infected Update.
• There was once a Corridor that led to the Crash Zone, this has since been removed in Experimental Mode.