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Difference between revisions of "v0.31:Sedimentary layer"
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(In real world geology, sedimentary {{L|stone}} is formed by sediment. The sediment collects in constantly growing heaps and the pressure at the bottom eventually forms the sediment into stone.) | (In real world geology, sedimentary {{L|stone}} is formed by sediment. The sediment collects in constantly growing heaps and the pressure at the bottom eventually forms the sediment into stone.) | ||
− | == | + | ==Sedimentary layers== |
− | {{ | + | {{makelist|cv:Inorganic stone layer|type=INORGANIC|reqtagtype=SEDIMENTARY|capturetagtype=STATE_NAME_ADJ|capturetagoffset=2|delimiter=\9 |
− | == | + | \9 |
− | {{ | + | |decoration=* <span style="text-transform: capitalize">{{lb}}{{NAMESPACE}}:\1{{!}}\1]]</span> |
− | + | }} | |
− | |||
− | {{ | ||
− | |||
− | {{ | ||
− | == | + | ==Stone specific to sedimentary layers== |
− | {{ | + | {{makelist|cv:Inorganic stone mineral|type=INORGANIC|reqtagtype=ENVIRONMENT|reqtagoffset=1|reqtagentry=SEDIMENTARY|capturetagtype=STATE_NAME_ADJ|capturetagoffset=2|delimiter=\9 |
+ | \9 | ||
+ | |decoration=* <span style="text-transform: capitalize">{{lb}}{{NAMESPACE}}:\1{{!}}\1]]</span> | ||
+ | }} | ||
+ | ==Gems specific to sedimentary layers== | ||
+ | {{makelist|cv:Inorganic stone gem|type=INORGANIC|reqtagtype=ENVIRONMENT|reqtagoffset=1|reqtagentry=SEDIMENTARY|capturetagtype=IS_GEM|capturetagoffset=1|delimiter=\9 | ||
+ | \9 | ||
+ | |decoration=* <span style="text-transform: capitalize">{{lb}}{{NAMESPACE}}:\1{{!}}\1]]</span> | ||
+ | }} | ||
{{Category|Stone Layers}} | {{Category|Stone Layers}} |
Revision as of 01:28, 30 April 2010
This article is about an older version of DF. |
This is the only layer you will find Template:L and Template:L which are needed for coke, for furnaces. They also contain large amounts of ore such as iron.
Sedimentary stone layers contain Template:L, Template:L, Template:L, Template:L, Template:L, Template:L, and Template:L.
Template:L*, Template:L, Template:L, Template:L, Template:L*, Template:L*, Template:L, Template:L, Template:L, Template:L and Template:L layers are sedimentary.
- (* These also function as Template:L.)
The name of a sedimentary layer appears white on the embark menu.
Sedimentary layers are, on average, the most economically valuable of the four mineral layers. They are your only source of Template:L and Template:L, vital for fueling non-Template:L forges and for the Template:L Template:L-making requires (especially if you lack Template:Ls). They are much richer in Template:L Template:Ls than other rock formations. Several sedimentary rocks - Template:L, Template:L, and Template:L - are Template:Les, required for Template:L-making and also being twice as valuable as normal stone, making them useful for Template:L or Template:L.
(In real world geology, sedimentary Template:L is formed by sediment. The sediment collects in constantly growing heaps and the pressure at the bottom eventually forms the sediment into stone.)