Fixed Download Vein Miner

Mine a single ore to break the full vein of the same ore! Veinminer is a common feature in various modpacks or survival pvp game modes like UHC to speed up breaking whole veins. Now you can you this feature as a datapack too!

The Veinminer effect can be limited to certain pickaxes to balance the usage (default active for every pickaxe). Additionally, a hunger effect can be applied to veinminers to compensate the hunger debuff on mining multiple blocks. You can define an extra cooldown to limit the usage even more!

Download Vein Miner

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It is the only ability without this command, and it is going to get my killed. Because of how the controls are set up, there is no way to just hold a button and use vein miner (unlike every other ability). You must first select vein miner, and then use it. The issue comes from if I recently used something like Dash (with its own dedicated hotkey), and then I go to vein mine using the ability button, I will dash instead. I guarantee I will die to this, probably a lot. I've already had many close calls in the Nether, nearly dashing off a cliff into the lava below.

I thought I would be clever and set the "Select Vein Miner" and "Use Ability" to the same hot key, and it works! Kind of. The new issue arises that, for some reason, doing this will turn vein miner into a permanent toggle (always vein mining) unless you deselect it with another ability.

Vein Miner Mod (1.12.2, 1.11.2) is a mod to help mine veins of ores by mining blocks of the same type in a chain reaction, giving you the blocks at the end. It is inspired by Connected Destruction by Bspkrs.

You do not have to craft any items to have benefit from the veinminer mod. On most modpacks the veinminer ability is, by default, set to the crouch or Shift key. Upon any item you can break with your hand ex. dirt, wood, sand, etc. will not require you to have a tool in hand, but an item (nothing specific) will have to be in your hand. Respectively veinmining stone, cobblestone, ores, etc. will require a pickaxe. Also (on most modpacks) by default veinmining will depreciate your hunger and the durability of the tool,if a tool is used.

To use Veinminer, you need to have Veinminer installed on the server (for single player games the client and the server are the same). You do not need to have Veinminer installed on the client, however it will provide reduced functionality to the clients that do not have it installed.

In order to get the most out of Veinminer, you shold edit the VeinMiner.cfg config file. Add the ids of the blocks to the different block lists to that you wish to be able to mine using Veinminer. Add any tools that you want to be able to use to use with Veinminer. The IDs should be changed on the server.

I did the /stop and restarted the server which was supposed to make vein miner in the server but it doesn't work. I used some of the commands and they go through showing that it is installed but when i sneak and break a block nothing happens

The Miner power-ups are ore vein miner, automatically smelt ores and haste I when mining. These all cost 10 coins each to unlock. The Miner superpower is haste II and speed I when mining. This will be unlocked when you reach level 100 of the Miner job.

Vein Miner is a custom enchantment for pickaxes that will mine an ore vein. The amount dug depends on the level. Fortune still works on all the ores. If other ores are connected to the initial vein, it will dig up those too.Vein MinerItemsPickaxeCursedNoMaximum levelsStable formXIUnstable formXXAvailabilityEnchantment tableYesTreasureYesVillagersYes

Did you know we have veinminer?PrerequisitesWelcomeLevelGetting StartedRewards4 ChestsQuest progressionPreviousNextWelcomeScanningThis quest is meant to teach the player about the Ore Excavation mod. To use the Ore Excavation function, hold anything in your hand in-game, hold down the "Excavate" key (which is set to backslash by default), and mine a block. Blocks of the same type that are connected to that block will all be destroyed, up to a certain number of blocks (limit of 512 blocks, range of 24 blocks). Try this out by holding an item in your hand, holding down the excavate key, and punching a tree. If all goes well, the whole tree should break. Do this enough times to collect sixteen logs, and you will receive four chests for your troubles.

Vein miner is a custom enchantment for pickaxes that will mine an ore vein. The amount dug depends on the level. Fortune still works on all the ores. If other ores are connected to the initial vein, it will dig up those too.

Huh, that would be nice. But seriously, it's kind of insane to me that there seems to be absolutely NO veinminer mod for this game of any sort. It's been around in various forms for half a decade now. The first Veinminer mod for Minecraft was made in 2013, just four years after the early days in 2009. And this game seems just as moddable, if not incredibly more so. Still just seems bizarre. Maybe it's from the Grind culture that seems to have been a thing around this game since the start.

Leaf-mining Stilbosis quadricustatella larvae are distributed non-randomly within leaves of their host plants, sand live oak (Quercus geminata) and water oak (Q. nigra), in north Florida. Fewer mines are found together on the same side of the mid-vein than separated, on opposite sides of the mid-vein. Larvae do not normally cross the mid-vein but create small blotch-like mines along subsidiary veins. Investigations of the usual mortality factors acting on these leaf-miner populations, including competition, parasitism, and predation, revealed no significant differences in these factors between mines separated by the mid-vein and those on the same side of the leaf. However, early leaf abscission, which kills the larvae present in the leaf, occurs significantly more frequently in cases where larvae are clustered on one leaf side. The reasons for this differential leaf abscission are not yet clear.

N2 - Introduction: The planetesimal collision is one of the most important processes in the solar system evolution. Shock veins in meteorites were formed through such process. High-pressure pol-ymorphs of silicates, oxides, and phosphate have been reported from ordinary [e.g., 1], carbonaceous [2], and differentiated me-teorites [e.g., 3, 4, 5], in relation with shock veins. These miner-als provide constraints on the conditions of collisional process in the solar system. On the other hand, no high-pressure phases have been yet reported from enstatite chondrites. Although Kimura et al. [6] systematically studied silica polymorphs in EH and EL chondrites, no high-pressure phases were encountered. Recently, a shock vein was observed in an EH chondrite, Asuka 10164 (A10164) [7]. Here we present our preliminary results on this chondrite, focusing on the shock vein. Petrography: Although A10164 is shocked, the sample in-cludes abundant chondrules, which mostly consist of clinoensta-tite and glassy mesostasis, with olivine, diopside, and a silica mineral. Opaque minerals in the host are Fe-Ni metal, schreiber-site, perryite, troilite, niningerite, and daubreelite, which are typi-cal of EH chondrites [8]. All these observations support the clas-sification of A10164 as EH3 chondrite. The shock degree is S4, after the criteria by [9]. Shock vein: A shock vein, ~0.3mm in width, crosscuts the sample, and comprises fragments of fine-grained silicates, opaque minerals, and chondrule fragments. In the vein, we found coesite, identified by the characteristic Raman peaks at 521 and 268 cm-1. All silica minerals in the vein are coesite. This is the first discovery of a high-pressure phase in E chondrites. Other high-pressure polymorphs of silicates were not observed in the shock vein, but further investigation is planned. On the other hand, the host does not contain any high-pressure phase. Chon-drules include cristobalite, which is consistent with [6]. The occurrence of coesite indicates that A10164, as well as the other meteorites, experienced high-pressure condition during shock event. However, the stability of coesite indicates that the pressure condition for A10164 might have been lower than in other meteorites containing high-pressure polymorphs, such as ringwoodite and majorite. At any rate, our results suggest that all major chondrite groups contain high-pressure polymorphs. Therefore, heavy shock events commonly took place in the solar system.

AB - Introduction: The planetesimal collision is one of the most important processes in the solar system evolution. Shock veins in meteorites were formed through such process. High-pressure pol-ymorphs of silicates, oxides, and phosphate have been reported from ordinary [e.g., 1], carbonaceous [2], and differentiated me-teorites [e.g., 3, 4, 5], in relation with shock veins. These miner-als provide constraints on the conditions of collisional process in the solar system. On the other hand, no high-pressure phases have been yet reported from enstatite chondrites. Although Kimura et al. [6] systematically studied silica polymorphs in EH and EL chondrites, no high-pressure phases were encountered. Recently, a shock vein was observed in an EH chondrite, Asuka 10164 (A10164) [7]. Here we present our preliminary results on this chondrite, focusing on the shock vein. Petrography: Although A10164 is shocked, the sample in-cludes abundant chondrules, which mostly consist of clinoensta-tite and glassy mesostasis, with olivine, diopside, and a silica mineral. Opaque minerals in the host are Fe-Ni metal, schreiber-site, perryite, troilite, niningerite, and daubreelite, which are typi-cal of EH chondrites [8]. All these observations support the clas-sification of A10164 as EH3 chondrite. The shock degree is S4, after the criteria by [9]. Shock vein: A shock vein, ~0.3mm in width, crosscuts the sample, and comprises fragments of fine-grained silicates, opaque minerals, and chondrule fragments. In the vein, we found coesite, identified by the characteristic Raman peaks at 521 and 268 cm-1. All silica minerals in the vein are coesite. This is the first discovery of a high-pressure phase in E chondrites. Other high-pressure polymorphs of silicates were not observed in the shock vein, but further investigation is planned. On the other hand, the host does not contain any high-pressure phase. Chon-drules include cristobalite, which is consistent with [6]. The occurrence of coesite indicates that A10164, as well as the other meteorites, experienced high-pressure condition during shock event. However, the stability of coesite indicates that the pressure condition for A10164 might have been lower than in other meteorites containing high-pressure polymorphs, such as ringwoodite and majorite. At any rate, our results suggest that all major chondrite groups contain high-pressure polymorphs. Therefore, heavy shock events commonly took place in the solar system. ff782bc1db