- published: 02 Jun 2022
- views: 6069
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 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.
The reef knot, or square knot, is an ancient and simple binding knot used to secure a rope or line around an object. It is sometimes also referred to as a Hercules knot. The knot is formed by tying a left-handed overhand knot and then a right-handed overhand knot, or vice versa. A common mnemonic for this procedure is "right over left; left over right", which is often appended with the rhyming suffix "... makes a knot both tidy and tight". Two consecutive overhands of the same handedness will make a granny knot. The working ends of the reef knot must emerge both at the top or both at the bottom, otherwise a thief knot results.
Although the reef knot is often seen used for tying two ropes together, it is not recommended for this purpose because of the potential instability of the knot, and over-use has resulted in many deaths (see #Misuse as a bend).
The reef knot is at least between 4,000 and 9,000 years old. The name "reef knot" dates from at least 1794 and originates from its common use to reef sails, that is to tie part of the sail down to decrease its effective surface area in strong winds. To release the knot a sailor could collapse it with a pull of one hand; the sail's weight would make the collapsed knot come apart. It is specifically this behavior which makes the knot unsafe for connecting two ropes together.
Reef may refer to:
"Lately" may refer to:
"Lately" is a song by Skunk Anansie, released as the third single from their album Post Orgasmic Chill. It was released in August 1999. CD1 came with an interactive element featuring the video and CD2 featured three exclusive Polaroid pictures of the band. As of 2012, it is the band's last major hit, charting at #33 in their native United Kingdom.
The surreal music video was directed by Howard Greenhalgh, who directed the music video for "Goodbye" by Spice Girls, a year earlier. The music video shows the band performing in a small town where all its inhabitants are smiling while a comet (played by Skin) begins to have a collision course with Earth. The video for the single was a homage to Soundgarden's music video for "Black Hole Sun", which was also directed by Greenhalgh in 1994.
Lately is the studio album by the Contemporary Christian and gospel singer Raymond Cilliers.It was released on the label Brettian Productions in 2005.
Outcrop of the day. The Lighthouse epithermal gold quartz vein on Gasado Island South Korea.
Mineralised Quartz vein north of Bacchus Marsh
A brief but comprehensive description of how gold ore bodies form and the differences between placer and hard rock gold deposit. For the latest theories in understandable detail: Gold Bearing Fluids with Prof Stephen Cox: Part 1 https://www.youtube.com/watch?v=co8GG... Part 2: https://www.youtube.com/watch?v=a2iEj...
In this video Catherine describes en-echelon veins in a strike-slip shear zone exposed in Kilve, Somerset Dr. Catherine Mottram, Senior Lecturer University of Portsmouth Interested in finding out more about geology at the University of Portsmouth, see our website and youtube page: https://www.port.ac.uk/study/courses/bsc-hons-geology https://www.youtube.com/channel/UC_l62ESC3_ogxH8ZCE9HfIQ/videos
B Type veins are a unique indicator of the magmatic hydrothermal transition environment where porphyry type copper, gold and molybdenum deposit form. Learning to identify them is a really useful tool in the kit for mineral exploration geologists. They were first identified by Gustafson and Hunt in the El Salvador porphyry copper deposit in Chile: Gustafson, L.B., and Hunt, J.P., 1975, The porphyry copper deposit at El Salvador, Chile: Economic Geology, v. 73, p. 600–607. The full Fieldcraft video series is here: https://geologyupskill.thinkific.com/courses/fieldcraft-for-geologists Many thanks to Dr. Gregg Morrison, Manuel Hernández and the following blog for specimens that appear in this video. https://4.bp.blogspot.com/-LRQkaWLpzvU/XKRy1hv-5gI/AAAAAAAAAJw/9R-WOoAEUrE37pSZggr34JNfNV3nB...
To Buy Geology Material (affiliate link): https://www.ebay.com.au/sch/i.html?_from=R40&_trksid=p2380057.m570.l1313&_nkw=gold+geology&_sacat=0&mkcid;=1&mkrid;=705-53470-19255-0&siteid;=15&campid;=5338809723&customid;=&toolid;=10001&mkevt;=1
International expert Professor Rick Sibson talks about how fluids, faults and earthquakes interact in the crust to form fault-hosted gold deposits. Ken Harris has mined a typical fault-hosted deposit at the Red Robin mine in the Alps of southeast Australia. See more films about gold at http://goo.gl/0mw8Z4
Welcome to Geology Simply Explained. The purpose of these videos is to provide very simple explanations of very complicated geological processes that form mineral deposits so that you may become more familiar with some of the terms and concepts that geologists use to describe their field. In this one we’re going to discuss Porphyry and Epithermal deposits. Often corporate news releases and reports can be very complicated with technical terminology that’s foreign to most of us with only those trained in this field being able to understand. There’s a good reason for this, it’s a very complicated field! Another reason for these videos is to draw awareness to the publicly traded mineral exploration companies that we operate. These are some of the geological models that Eagle Plains Resources ...
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 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.
Oh yeah, alright
Lately, I have not been treated gently by myself
I have been over used, ripped off and abused
Stomping in my shoes, well no more, hey
Think of your family, home is the place to be
Think of your family once more, hey
Think of your family, home is the place to be
Think of your family once more, alright now
Oh yeah, alright, babe
Lately, all my clothes have been so dirty and threadbare
They have been over used, my heart battered and bruised
Thankless for my views, well no more
Think of your family, home is the place to be
Think of your family once more, yeah
Think of your family, home is the place to be
Think of your family once more
1,2,3,4
Been around the world, and there is nothing that I wouldn't do
Just to see the smile upon your face
Been around the world, and there is nothing that I wouldn't do
Just to see the smile upon your face
Think of your family, home is the place to be
Think of your family once more
Think of your family, home is the place to be
Think of your family once more