Tried to find pink wool area and found the yellow wool dungeon. Died in there. Then found the pink wool dungeon again and got my stuff and brought back the pink and blue wools. I only found green because I overshot my home and ended up on the wrong side of a mountain. It all worked out though 12 - Inferno Mines - not started 14 - Waking Up - not started. Going for red and black tonight.
Difficulty has been all over the place so I'm not sure how these 2 areas will play out. I think this was the hardest black and red wool areas I've had so far. Red wasn't too bad until the actual room with the wool in it. Then it got pretty crazy. The black felt hard from the moment I started onto the 2nd part of the dungeon and got harder the farther I went.
Still super excited to be done this one. Definitely not a fan of the continent style but it was an interesting change of map style. Completed June 6th 04 - Kaizo Caverns - completed in about a week May 1st - May 8th 07 - Legendary - not started 08 - Nightmare Realm - not started 09 - Sunburn Islands - not started 10 - Spellbound Caves - not started 11 - Lethamyr - completed June 15th 12 - Inferno Mines - not started 14 - Waking Up - not started I'm still not sure which map to start next.
I've got Legendary, Nightmare Realm and Spellbound caves all ready to play they all have the same suggested version. I kind of wanted to beat those before moving on to Sunburn Islands, Inferno Mines or Waking Up since they require a different version.
Anyone willing to reply here for the first time and suggest a map? Snowchu is Offline. Snowchu Snowdeath Level: ? Do Nightmare's Realm! I watched a LP of it, and man I'm sure you're in a bit of a surprise. I think you'll enjoy it! The starting area seemed safe until nightfall and I had to hide in a very small house I built in a panic.
I did get the white wool and got up to the Victory Monument. I've done a bit of housekeeping stuff but that's all I've managed so far. Completed June 6th 04 - Kaizo Caverns - completed in about a week May 1st - May 8th 07 - Legendary - not started 08 - Nightmare Realm - not started 09 - Sunburn Islands - not started 10 - Spellbound Caves - I've found the orange and magenta wools so far.
I fell in lava and lost all the stuff I had trying to get to the orange wool which sucked. I also died starting into a new area so I grabbed my stuff and ran away and I stopped playing after that. New Thread.
Page Comments. This page has no comments. All Rights Reserved - Total queries executed: Adblocker detected! I'm really looking forward to this It's going to be crazy So, I really badly want to beat all of the Super Hostile maps by Vechs but haven't really had the time or motivation to do it before.
Almost died to spiders so many times 03 - Infernal Sky 2 - not started 04 - Kaizo Caverns - completed in about a week May 1st - May 8th 07 - Legendary - not started 08 - Nightmare Realm - not started 09 - Sunburn Islands - not started 10 - Spellbound Caves - not started 11 - Lethamyr - not started 12 - Inferno Mines - not started 14 - Waking Up - not started 01 - Sea of Flame 2 - Started - found the Victory Monument and white, orange, magenta and light blue on day 1.
Have wood and wheat though so I have a food source 12 - Inferno Mines - not started 14 - Waking Up - not started 1 - Sea of Flame 2 - Completed in 5 days 03 - Infernal Sky 2 - started today May 27th Completed June 6th - Found the blue, brown, green, red and black wool's.
Wool boxes are either placed around the landscape or in a dungeon, depending on the map style. The maps are divided into either Open-World gameplay, where wool boxes are scattered around a large area, or Linear-Branching gameplay, where many branching paths with wool boxes are spread out between several intersections, which progress linearly into each other.
Lethamyr introduced Continental , a map style focusing on exploration and travelling, featuring realistic-scale biomes. In May of , the alpha version of Super Hostile Online was made availible to donors. In terms of gameplay, it functions like an Open-World map with parts reshaped to fit a larger focus on the multiplayer aspect. As you may have guessed by the name and description, these maps are very difficult , some more than others.
They provide a heightened challenge from regular Minecraft , because of the traps, density of monsters, and resource management. If you play Minecraft, and are looking for a challenge and a goal, these are the maps for you. Prospectors had already found rich placers at Bannack and Alder Gulch 70 miles to the south and at Dry Gulch near the present day City of Helena. As the placers were exploited miners located lode deposits, of which the first to be staked was the Asteroid claim in on Butte Hill Rickard, The gold near Butte was impure occurring with a mixture of silver and the veins were also found to contain copper, antimony, arsenic, and manganese.
In , a silver vein was discovered adjoining the Asteroid and was named the Travona. Shortly thereafter, numerous claims were located and Butte was transformed into the leading mining district of Montana Territory. Although metallurgical recovery of the ores proved difficult, miners drudged onward digging shafts to feet and continuing assessment work on the claims which included the Parrott, Original, Gray Eagle and Mountain.
Several years went by with little progress on recovering the refractory silver ores. In the Travona was re-located by William Farlin and in William Clark, a local banker, invested money into the Dexter stamp mill, which turned a profit on the silver ore. Silver mining peaked in with throughput from five mills Rickard, At the foot level a crosscut encountered a large vein 5 feet thick of chalcocite. By , the shaft reached feet and exposed more chalcocite in a vein over 90 feet thick.
Nonetheless, Butte now entered its third phase of mining — the copper industry. All the infrastructural components were in place for Butte just in time for the dawn of the electric age and the requirements for copper wire. During the period of to , Butte miners and mine owners fought over the rights of mining the copper veins.
The geology of Butte was complicated and the trend of ore veins mined underground presented a new difficult situation for those who claimed the right to mine them. Conflicts with this law created serious issues and started the underground wars of Butte which raged in the mines and in the courts.
During these years, no less than 45 companies operated in the Butte district. When all the dust settle it became clear for reasons of efficiency and legalities not to mention economic, one company through consolidation of all others would mine it all — The Anaconda Company Rickard, There were a few terrible disasters during the coming years including the 3,foot shaft fire which was described as a raging inferno killing miners. World War II required increased production from Butte but after the war as economic conditions changed demand dropped.
This allowed for the mining of lower-grade ore and by , when Kelley operations were suspended, over , mt of copper were recovered.
In , the Kelley shaft was deepened to the 4, foot level and ore was produced from the Mountain Con, Steward, and Leonard mines Meyer, Aside from cyclical fluctuations in copper prices, Chuquicamata was taken over by the Chilean government.
This created a financial crisis within Anaconda, and as a result, in underground operations ceased. In the remaining operations were terminated. In , Montana Resources resumed operations on the low-grade Continental pit, formerly the East Berkeley pit.
Acquisition Alice Amy-Silversmith Anselmo Anaconda— great producer of chalcocite-enargite ores Badger — Bornite dominant copper phase Belmont — Bornite dominant copper phase Berkeley pit Black Rock East Colusa — largest concentrations of digenite and covellite Elm Orlu Emma — abundant rhodochrosite, bonanza style veins.
Major mineral specimen producer. Gagnon Gem Goldsmith Leonard — great producer of chalcocite-enargite ores. Lexington - Major mineral specimen producer. Magna Charta Moulton Mountain Con — large veins of chalcopyrite. Red octahedral fluorite. Produced golden barite, bornite and pyrite mineral specimens. Syndicate pit Tramway — great producer of chalcocite-enargite ores Travona — first silver claim.
The ore body has been studied by numerous geologists with the most notable being Reno H. Sales and Weed, R.
Goddard Jr. More recently the Butte copper porphyry has been studied by Rusk, B. H The Butte mining district encompasses an area of approximately 2 by 4 miles which has produced huge commercial quantities of not only copper Although large scale, underground mining has seized in Butte, there is yet a large recoverable reserve at depth.
Montana Resources continues to mine low-grade porphyry ore east of the Berkeley pit. The Butte district Ore Production — Czehura, The Butte copper-molybdenum porphyry deposit is a complex stock work of veins thought to have been mineralized during multiple episodes.
The ore body is a classical example of concentric and distinct zones of mineralization even within veins which cut through the multiple zones. The main intrusive body, the Boulder batholith, was emplaced in a central tectonic block bounded on the north by Precambrian Belt Series rocks and on the south by Archean gneiss, schist and granite Meyer, The Boulder batholith show all the characteristics of an epizonal pluton emplaced in the upper crust with low hydrostatic pressures and multiple phases of volcanic intrusions.
The central tectonic block has been a zone of recurrent subsidence and tensive deformation since Precambrian. The copper porphyry is hosted within the Butte Quartz Monzonite, dated at 76 m.
The magmatic hydrothermal ore deposits are said to be hypogenetic, with supergene enrichment. Ore controls are predominately open tension fissures, fractures and faults within the intrusives Meyer, Butte ore deposition has been characterized in two major episodes: A Pre-Main and Main stage mineralization.
Little was known about the Pre-Main stage in the early years of mining. This stage consisted of small quartz veins containing molybdenite and chalcopyrite at depths in the central part of the district. The veins are bordered by alteration envelopes carrying potash feldspar, biotite, and sericite. The biotite has been dated at 63m.
Rusk et al has studied the fluid inclusions of the pre-Main stage mineralization and has proposed a single parental hydrothermal source from great depth generated the ore bearing fluids. Further, the variations in ore and alteration assemblages were the result of chemical changes of the parental fluid due to wall rock reactions at differing cooling and depressurization as opposed to pulses of fluid with differing compositions. In general, evidence for this exists in the consistency of composition of fluid inclusions throughout the ore body.
About core samples from 10 deep holes drilled from to were used by Rusk and previous researches to study the pre-Main stage mineralization. This information coupled with historical core samples, field mapping and hand sampling from the past years revealed two large internally zoned domes of copper and molybdenum mineralization. Both domes are 2km in diameter. The western dome called the Anaconda and the eastern called the Pittsmont are defined by abundant magnetite-bearing veins and steadily increasing outward molybdenum concentrations.
Main stage veins are above and to the west of the Anaconda dome. Rusk has worked out a hypothetical fluid evolution of the Butte deposit based on a comprehensive fluid inclusion study and he reader is referred to this paper at link. Nearly all the early ore production at Butte came from an east-west striking vein system and more frequent northwest striking veins.
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