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Granite |
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Granite is a hard, coarse-grained rock
that makes up a large part of every continent. Granite contains
three main minerals - quartz, alkali feldspar, and plagioclase
feldspar. These minerals make granite white, pink, or light grey.
Granite also contains small amounts of dark brown, dark-green, or
black minerals, such as hornblende and biotite mica. The grains of
the minerals in granite are large enough that they can easily be
distinguished.
The minerals in granite are interlocked like the pieces of a jigsaw
puzzle. Consequently, granite is a strong and durable which makes it
useful for construction.
Geologists classify granite as an igneous rock. The slow cooling and
crystallization of molten material called magma forms most granite.
Magma has the same chemical composition as granite. It forms from
rocks that melt 16 to 25 miles (25 to 40 kilometers') below the
surface of the continents. These rocks melt at temperatures between
1200' and 1650' F. (650' and 900' C). As the magma rises, it cools.
Most granite magma cools slowly enough to form coarse crystals and
it solidifies below the earth's surface.
Sometimes granitic magma erupts from volcanoes and cools too quickly
to form large crystals. The resulting rock, called rhyolite, has the
same mineral composition as granite but is fine grained.
Granite 1
A very hard, crystalline, platonic rock (formed far below the
surface of the earth by slowly cooling magmatic bodies) of various
colors consisting of feldspar, quartz (crystalline -2-silica) and
smaller amounts of other minerals. Granite is very hard and more
resistant to damage than marble, making granite more difficult to
harm and correspondingly more difficult to restore than marble. Care
of granite is similar to marble except more work is required,
however the work is required less often. As a practical matter, a
final high gloss finish on granite is generally achieved by using
power driven polishing tools and fine grit diamonds.
Granite 2
Granite is one of the oldest, most durable and most respected of
building materials. Traditionally, it is the material chosen by both
architects and engineers when permanence, enduring color and
texture, and complete freedom from deterioration and maintenance are
prime requirements.
And granite is ageless--always contemporary. Today's leading
architects, knowing its unique qualities, are using it more
extensively than ever before. Many of our most impressive buildings,
commercial as well as institutional and monumental, are being faced
with granite, and it's still unequaled as a material for steps,
terraces, and the pavings of plazas and public spaces.
The granite industry is keeping pace with architectural progress and
changing demands. Technological developments have revolutionized
quarrying and fabrication methods, reducing costs and leading to new
applications. Attractive new finishes, new construction techniques
and new jointing methods have been introduced. For example, granite
is being employed on steel frames to provide preformed wall units
which require no additional masonry back-up.
It is common practice in the industry to to classify architectural
granite as either of two types:
Building Granite : Granite used either structurally or as a veneer
for exterior or interior wall facings, steps, paving, copings or
other building features.
Masonry Granite : Granite used in larger blocks for retaining walls,
bridge piers, abutments, arch stones and similar purposes.
Granite 3
Granite: a coarse-grained rock composed mainly of the minerals
quartz and feldspar, often containing small quantities of mica or
hornblende. Commonly believed to develop as an igneous rock (created
by molten magma under pressure), some researchers now think that
granite is actually metamorphic in nature (created by pressure deep
under the earth's surface). Some beds of granite are among the
world's oldest stone. Granite develops in all parts of the world,
with some of the major granite bed occurring in North America,
Brazil and India.
So, how does granite get from the ground to houses and buildings
around the world?
First, it is mined. Taken from the ground in blocks roughly shaped
like train cars, the granite is sliced into sheets about one inch
thick and polished on one side. Then it is shipped around the world
to distributors, who sell it to the fabrication shops which actually
use up the stone.
Why is granite so popular as a countertop material?
There are several answers to that question:
· First and foremost, looks! Granite comes in some amazing colors,
and is considered to be one of the most beautiful stones in the
world.
· Durability. Granite lasts the lifetime of a person's home without
chipping or scratching, and is impervious to heat. The color and
polished surface of granite do not fade over time.
· Economics. With the new technology available to the miners and
fabricators of granite, the cost of granite has dropped dramatically
in the last few decades. Stone prices are now competitive with
man-made options, and granite lasts longer than any other surface!
· Ecology. Although mining is rough on the environment, other
products are far worse in several ways. Man-made products create
potentially deadly by-products which go straight to our crowded
landfills. Due to granite's durability and timeless beauty it does
not need to be replaced or upgraded, whereas man-made counters are
replaced several times over the life of a building, further adding
waste (both environmentally and financially).
Granite 4
Granite is a very hard crystalline, igneous rock that is available
in a vast range of colour, texture and mineral composition.
Granite is available in the following finishes: polished, honed,
fine rubbed, thermal flame finished, and can take a sandblasted
coarse or fine stippled finish. ASTM C97 - Absorption by weight 0.4%
max.
Granite 5
Granites are intrusive rocks that start out as molten masses deep
within the earth. As the mass cools, the minerals form into crystals
of various sizes and shapes, depending on the conditions at the
time. Large crystals are indicative of a slow cool down while small
crystals are typical of a rapid cooling.
Granites are typically made up of three minerals; quartz, feldspar
and mica. "Gneiss" are a category of granites that have
metamorphosed or changed to a different form. Granites are typically
the hardest of the dimensional stones and withstand the elements
very well. Granites are best for kitchen counters since
They resist scratching are stain and heat resistant. They are also
suitable for flooring or paving, wall cladding, all other types of
counter tops and tombstones. Granite is suitable for either exterior
or interior applications.
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Limestone |
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Limestone
is a type of rock made up mostly of calcite, a mineral form of
calcium carbonate. Most limestone is grey, but all colours of
limestone from white to black have been found.
All limestone are formed when the calcium carbonate crystallises out
of solution. It leaves the solution in many ways, and each way
produces a different kind of limestone.
Limestone can be formed almost completely without the aid of
organisms. This type of limestone is forced out of solution when the
water evaporates.
Evaporation of water in limestone caverns forms another variety of
limestone, called travertine, into stalactites and stalagmites.
Some limestone can be formed by the
work of organisms. Many aquatic organisms draw calcium carbonate out
of the water and use it to make their shells and bones. The oysters,
clams, snails, corals, and sea urchins do this. When the animals die
the shells and bones are broken up by waves into shell and coral
sand and mud.
Limestone makes an excellent building stone because it can be carved
easily. Some factories use limestone to clean waste gases and water
before releasing them into the environment. Limestone is also used
to make lime and to smelt iron ore.
Limestone 1 :
Limestone is typically formed over many years at the bottom of
oceans or lakes from the accumulation of shells, bones and other
calcium rich goods. If this limestone is subjected to intense heat
or pressure and a few millennium, a crystallization will occur and
the limestone will become a "true marble". Chemically they are both
still Calcium Carbonate (TUMS), but the marble will have a
crystalline structure and the limestone will have relatively flat
appearance.
Limestones that will take a polish are considered marbles by most
people, but technically, if there are still shells visible or the
structure is not crystalline, it is still a limestone.
Limestone that have magnesium in them are called"dolomitic
limestones" and are typically much harder and more resistant to
weathering. A typical characteristic of dolomitic limestones are
their capability of taking a flamefinish.
Limestones are typically used for flooring, wall cladding, vanity
tops, furniture, and often times ornate stonework.
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Marble |
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Marble
is a rock widely used in buildings, monuments, and sculptures.
It consists chiefly of calcite or dolomite, or a combination of
these carbonate minerals. Marble is a type of metamorphic rock
formed from limestone. Marble is found in many countries,
including Belgium, France, Great Britain, Greece, India, Italy,
and Spain.
Marble is formed from limestone by heat and pressure in the
earth's crust. These forces cause the limestone to change in
texture and makeup. This process is called recrystallization.
Fossilized materials in the limestone, along with its original
carbonate minerals, recrystallise and form large, coarse grains
of calcite. Impurities present in the limestone during
recrystallization affect the mineral composition of the marble
that forms. The minerals that result from impurities give marble
wide variety of colours. The purest calcite marble is white.
Marble containing hematite has a reddish colour. Marble that has
limonite is yellow, and marble with serpentine is green.
Marble does not split easily into sheets of equal size and must
be mined carefully. The rock may shatter if explosives are used.
Blocks of marble are mined with channeling machines, which cut
grooves and holes in the rock,
Uses. Marble has long been highly valued for its beauty,
strength, and resistance to fire and erosion. The ancient Greeks
used marble in many buildings and statues. The Italian artist
Michaelangelo used marble from Carrara, Italy, in a number of
sculptures.
Extremely pure calcite marble is used for most statues. Large
blocks of coloured marble are, used for columns, floors, and
other parts of buildings. Smaller pieces of such marble are
crushed or finely ground and used as abrasives in soaps and
other products. Crushed or ground marble is also used in paving
roads and in manufacturing roofing materials and soil treatment
products.
Marble 1 :
Marble is limestone that has crystallized naturally over a
period of time. Marble is classified into four groups, Groups A,
B, C, and D. These are broad classifications and relate only to
soundness and working qualities. However, for the purpose of
this maintenance guide marble has been classified as exterior or
interior maintenance of marble. The test used for water
absorption is ASTM C97. Marble is cut into blocks, slabs or tile
in various thickness and sizes. Marble flooring is very
sensitive to acids and alkalis and can be stained if spills are
not wiped up immediately. If marble flooring is installed in an
area where staining liquids are liable to cause problems, then
the flooring should be sealed and finish applied.
Marble 2 :
Marbles are basically metamorphosed limestones. Once limestone
is subjected to heat and pressure, the calcium carbonate re
crystallizes into marble.
Marbles have similar characteristics to limestones and are
typically used on the same applications, though, marbles are
almost always more aesthetically valuable and available in much
wider range of colors.
There are several types of marbles, including calcites (from
calciferous limestones), dolomites (from dolomitic limestone),
serpentines (typically green marbles) and travertines
(sedimentary limestone). Each of these is similar in their
composition, that being predominantly calcium carbonate, and
their capability to take a polish. The stone that is quarried
west of Belen in central New Mexico is a travertine marble.
Many years ago there was a cataclysmic shift in the earth's
crust and the Rio Grande Valley appeared. The Sandia mountains
were pushed up on the east side bringing granite to the surface
and leaving limestone on the top or backside of the mountain.
This limestone was once the floor of a vast ocean that covered
the entire southwest U.S. If you drive along south 14 you can
see the layers of limestone along along the roadside. This same
limestone is used to make cement at the plant in Tijeras, New
Mexico. When the valley was formed, there were openings made in
the earth's crust which allowed volcanoes to form and many hot
springs to appear. These hot spring were present west of Belen,
and as they came to the surface, the water passed through the
limestone beds.
The calcium carbonate in the
limestone went into suspension in the water and once it got to
the surface the water evaporated and it become travertine.
One characteristic of all Travertines is the presence of small
voids that were caused by air bubbles in the hot water. At times
when the springs went cold, onyx was formed. It is not uncommon
to find bands of onyx among travertine beds.
Marbles are suitable for both interior and exterior applications
but it should be noted that with today's environment containing
so many pollutants, if a polish finish is specified on marble,
it will not last.
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Slate |
Slate is a
fine-grained rock that can easily be split into thin, durable
sheets. It consists mainly of grains of mica and quartz, plus
smaller amounts of chlorite, hematite, and other minerals. Most
slate is grey to black in colour, but the rock may be red or purple,
depending on its mineral content.
Slate is a metamorphic rock. Most slate is formed below the earth's
surface by changes in the makeup and appearance of shale, a
sedimentary rock. Shale consists of clay and fine particles of
quartz. Heat from deep in the earth changes some of the clay in
shale into mica and chlorite. Slate results when pressure created
chiefly by mountain-forming movements in the earth's crust squeezes
the mica and other minerals into parallel layers.
The building industry uses slate for roofing and flagstone because
the rock is weatherproof and long lasting. Slate is also used to
trim the fronts and lobbies of buildings.
Slate 1 :
Slate is a split stone and is one of the world's oldest natural
products. Slate is available in various colours. Some shades will
change colour on exterior use; therefore a non-fading shade should
be specified for exterior applications. Water absorption of slate in
accordance with ASTM C121.
Slate 2 :
There are items on the market that can be written on again and
again. These are 'slates', I guess that word is right, that consist
of a layer of transparent film, under this film there is a layer of
magnetic dust or something but I don't know the exact make up of the
materials used. Then one has a pen to go with that with which one
can draw a line over the magnetic part of the board which will be
black. When one wishes to erase the drawing/writing/sketch there is
a little handle on the side connected to an elongated magnet under
the magnetic film. When you move this handle from right to left then
all the magnetic particles get evened out and the screen is blank
again. A year ago I saw this on TV too, but this time as a tool to
be used in offices as a substitute for the 'flip over', this in
order to spare paper.
What you are describing sounds like the 'Etch a Sketch'. If you have
ever tried it, actually writing on it is very difficult. There is a
simple writing device which is a transparent gray film over a slick,
black cardboard background. You write or draw on it with a blunt
stylus. This causes the film to stick to the background, making a
line. When you want to reuse it, you simply pull up one end of the
sheet and it is 'erased'. For temporary drawing or writing, it would
be hard to beat the simplicity of chalk and slate! Also available in
multiple colors! Paper is still important, as it would be the
lowest-tech medium which would have any chance of surviving for a
long period of time. Writing should not be allowed to die out!
Slate 3 :
Slate is basically metamorphosed shale. Shale is made up of slit and
clay that is similar in composition to sandstone except that the
particle size is much smaller. The shale is subject to heat and
pressure and the fine particles are "melted" together to form slate.
Slates are a natural cleft material and are typically used for
flooring or roofing applications. Some slates are available in large
slabs and can be used for counter tops.
Most slates are suitable for exterior and interior applications. Be
careful when specifying green slates as their color may change or
fade with time.
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