Vein (album)

Vein is the thirteenth album by Japanese experimental band Boris. The album was released on vinyl on October 2006 through Important Records and was limited to 1500 copies only. Vein became somewhat controversial for the long delays prior to the release but most importantly for presenting two different albums under the album's title. As the label in charge of the release explained, "Every aspect of this beautiful release was planned and designed by Boris and they have stated that it has very special meaning for them".

In 2013, the band announced that the album would be released as a 2-CD set but that this was not a reissue of the album, but rather a re-arrangement of both albums combined. The label in charge of this release explained that this release sounds different from the previous versions. The album was packaged in two 3" CDs with the same printed outer edge as the vinyl release to make them appear to be traditional 5" CDs.

Part of track A7 of the hardcore vinyl version is used in the untitled final track of Smile. It is present unadulterated, but as an alternate, bass-heavy mix, on the Southern Lord US vinyl pressing of Smile as "VEIN;" it is thus removed from the untitled song. The 2013 CD pressing of Vein moves this to track 11 and is yet another mix, this one even incorporating the backwards guitar melody from the untitled Smile track. This creates a circle of sampling that intermingles the two albums.

! (album)

! is an album by The Dismemberment Plan. It was released on October 2, 1995, on DeSoto Records. The band's original drummer, Steve Cummings, played on this album but left shortly after its release.

Track listing

Personnel

The following people were involved in the making of !:

References

Album

Albums of recorded music were developed in the early 20th century, first as books of individual 78rpm records, then from 1948 as vinyl LP records played at 33 ¹⁄₃ rpm. Vinyl LPs are still issued, though in the 21st century albums sales have mostly focused on compact disc (CD) and MP3 formats. The audio cassette was a format used in the late 1970s through to the 1990s alongside vinyl.

An album may be recorded in a recording studio (fixed or mobile), in a concert venue, at home, in the field, or a mix of places. Recording may take a few hours to several years to complete, usually in several takes with different parts recorded separately, and then brought or "mixed" together. Recordings that are done in one take without overdubbing are termed "live", even when done in a studio. Studios are built to absorb sound, eliminating reverberation, so as to assist in mixing different takes; other locations, such as concert venues and some "live rooms", allow for reverberation, which creates a "live" sound. The majority of studio recordings contain an abundance of editing, sound effects, voice adjustments, etc. With modern recording technology, musicians can be recorded in separate rooms or at separate times while listening to the other parts using headphones; with each part recorded as a separate track.

+ (disambiguation)

+ (the plus sign) is a binary operator that indicates addition, with 43 in ASCII.

+ may also refer to:

See also

Vein (geology)

In geology, a vein is a distinct sheetlike body of crystallized minerals within a rock. Veins form when mineral constituents carried by an aqueous solution within the rock mass are deposited through precipitation. The hydraulic flow involved is usually due to hydrothermal circulation.

Veins are classically thought of as being the result of growth of crystals on the walls of planar fractures in rocks, with the crystal growth occurring normal to the walls of the cavity, and the crystal protruding into open space. This certainly is the method for the formation of some veins. However, it is rare in geology for significant open space to remain open in large volumes of rock, especially several kilometers below the surface. Thus, there are two main mechanisms considered likely for the formation of veins: open-space filling and crack-seal growth.

Open space filling

Open space filling is the hallmark of epithermal vein systems, such as a stockwork, in greisens or in certain skarn environments. For open space filling to take effect, the confining pressure is generally considered to be below 0.5 GPa, or less than 3-5 kilometers. Veins formed in this way may exhibit a colloform, agate-like habit, of sequential selvages of minerals which radiate out from nucleation points on the vein walls and appear to fill up the available open space. Often evidence of fluid boiling is present. Vugs, cavities and geodes are all examples of open-space filling phenomena in hydrothermal systems.

Veining (metallurgy)

In metallurgy a veining (or finning) is the occurrence of a sheet like casting defect, produced by molten metal penetration into a sand casting mould.

a defect on the surface of a casting appearing as fins, veins or wrinkles and associated with excessive thermal movement of the sand, especially core sand

Description

Veining occurs as 'vein' like projections from a casting, usually at right angles to the casting's surface; the phenonoma can occur in any alloy, and is commonly seen in ferrous or copper based castings.

Veining has been attributed to temperature differences at distance from the molten metal resulting in differential thermal expansion in the sand leading to strain in, and failure of the sand mould. Research has shown that a main cause of veining is thermal expansion of the silica sand in combination with reduction in sand volume above 573C (after the alpha to beta silica phase transformation) due to softening/sintering and/or melting of sand grains, which results in cracking/voids.

Leaf

A leaf is an organ of a vascular plant and is the principal lateral appendage of the stem. The leaves and stem together form the shoot.Foliage is a mass noun that refers to leaves collectively.

Typically a leaf is a thin, dorsiventrally flattened organ, borne above ground and specialized for photosynthesis. Most leaves have distinctive upper (adaxial) and lower (abaxial) surfaces that differ in colour, hairiness, the number of stomata (pores that intake and output gases) and other features. In most plant species, leaves are broad and flat. Such species are referred to as broad-leaved plants. Many gymnosperm species have thin needle-like leaves that can be advantageous in cold climates frequented by snow and frost. Leaves can also have other shapes and forms such as the scales in certain species of conifers. Some leaves are not above ground (such as bulb scales). Succulent plants often have thick juicy leaves, but some leaves are without major photosynthetic function and may be dead at maturity, as in some cataphylls, and spines). Furthermore, several kinds of leaf-like structures found in vascular plants are not totally homologous with them. Examples include flattened plant stems (called phylloclades and cladodes), and phyllodes (flattened leaf stems), both of which differ from leaves in their structure and origin. Many structures of non-vascular plants, and even of some lichens, which are not plants at all (in the sense of being members of the kingdom Plantae), look and function much like leaves. The primary site of photosynthesis in most leaves (palisade mesophyll) almost always occurs on the upper side of the blade or lamina of the leaf but in some species, including the mature foliage of Eucalyptus palisade occurs on both sides and the leaves are said to be isobilateral.