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Sand and red sand are in the same article, and this block is basically the same as sandstone, including all the crafting recipes. Would it be better to merge it with the sandstone article? --KnightMiner (t|c) 14:33, 6 August 2014 (UTC)
The result of the discussion was do not merge.
Both share the same ID, and they are therefor technically the same block. All the recipes are also the same, so I believe that the two articles should be merged. Clone200 (talk)
The result of the discussion was merge with Sandstone.
This page should be merged with sandstone. The following sections would be easily combined:
This covers most of the article. Why everyone opposed makes no sense at all.71.212.10.80 03:12, 14 May 2015 (UTC)
The colours of sandstones arise, not so much from that of the quartz, which is commonly white or grey, as from the film or crust which often coats the grains and holds them together as a cement. Iron, the great colouring ingredient of rocks, gives rise to red, brown, yellow, and green hues, according to its degree of oxidation and hydration. Like conglomerates, sandstones differ in the nature of their component grains, and in that of the cementing matrix. Though consisting for the most part of siliceous grains, they include others of clay, felspar, mica, or other mineral; and these may increase in number so as to give a special character to the rock. Thus sandstones may be argillaceous, felspathic, micaceous, calcereous, &c. By an increase in the argillaceous constiuents, a sandstone may pass into one of the clay-rocks, just as modern sand on the sea-floor shades imperceptibly into mud. On the other hand, by an augmentation in the size of the grains, a sandstone may become a grit, or a pebbly or or conglomerate, so that the difference between the two rocks is little more than one of relative size of particles. The cementing material of sandstones may be ferruginous, as in most ordinary red and yellow sandstones, where the anhydrous or hydrous iron oxide is mixed with clay or other impurity-in red sandstones the grains are held together by a haematitic, in yellow sandstones by a limonitic cement; argillaceous, where the grains are united by a base of clay, recognizable by the earthy smell when breathed upon; calcareous, when carbonate of lime occurs either as an amorphous paste or as a crystalline cement between the grains; siliceous, where the component particles are bound together by a flinty substance, as in the exposed blocks of eocene sandstone known as "grey-weathers" in Wiltshire, and which occur also over the North of France towards the Ardennes
BDJP007301 had quickly closed the new discussion, even after I replied with my changed decision. He thinks that given there is a consensus against already, no new arguments, like that real-life factor, will be at all applicable. I would also say that consensus must be based on applicable arguments (which also have their weight), not a number of users voting for/against, and thus closing of the original discussion wrong. — 👁 Image
NickTheRed37 (talk|contributions) 15:48, 14 May 2015 (UTC)
I think that in merge/split discussions we shouldn’t rely on block characteristics alone. We should analyze the blocks from a player’s prospective, as this gives more info and, in result, more accurate statistics that will affect the resulting decision in a right way. Most users participating in these discussions don’t know that just yet. I know, this may not apply to sandstones, but I feel like this place is appropriate to say that. — 👁 Image
NickTheRed37 (talk|contributions) 14:02, 30 May 2015 (UTC)