![]() ![]() I designed the functionality of Blacksmith to be identical to that of ARchive_neXt. ![]() The repo will stay online and will not be deleted.īlacksmith tries to serve as a successor to ARchive_neXt, since development has seemingly ceased, and it does not support the two latest Assassin's Creed games nor Steep. However, the readme, changelog, and Releases page will still be updated. ![]() I have migrated away from GitHub due to the amount of effort and time I have put into development. Access to the source code is now a donation perk. I will no longer be updating the repo with the source code of 1.7 and later. Join the Discord server to engage with other fans of Assassin's Creed (and other supported games), and for quick support.Ĭheck the Current Support section to see what is supported. The program assumes that you have access to the games' files. Note 2: Blacksmith supports ALL VERSIONS (past and latest) of each game It CANNOT MODIFY, INJECT, NOR REPLACE files. The laterites were subsequently buried, folded, faulted, and intruded, but the mineralogy, structure, and texture of the ores were essentially unchanged during these events.Blacksmith is a tool for viewing, extracting, and converting textures, 3D models, and sounds from Assassin's Creed: Odyssey, Assassin's Creed: Origins, Assassin's Creed: Valhalla, and Steep. The hard hematite ore was derived from the primary magnetite-banded oxide facies of iron formation which underlies the ore at the Cliff-Shaft mine, and the hard goethite ore was derived from the primary pyrite facies at the Caland or Steep Rock mines. This indicates that both deposits were formed as laterites resulting from the oxidation and leaching of primary iron formation by meteoric solutions. Both ore deposits have a prefolding remanence that differs in age from any of the associated rock units. Geologists have proposed several theories to explain the genesis of these iron deposits of direct-shipping grade. Alternating-current demagnetization and other standard paleomagnetic procedures were used. A paleomagnetic study was made on 67 samples from the ore horizons and associated rocks of these deposits. Hard hematite ore is mined at the Cliff-Shaft mine, Marquette Range, Michigan, and hard goethite ore is mined at the Caland and Steep Rock mines. ![]()
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