Chalk has such large NON WEIGHT that it may be defined in terms of -x gravity or as levels in the other side of gravity progression, for example
our Sun as a G type star as the 5th type of star may have -5 gravity.
The observations of the core of the sun or any other star will not be visable by using gravity detection, rather ,the core will have states of lite weight related to
chalk and it's lite weight values. By making comparisons with the CHALK on the Moon as some specific gravity as 1/3 of the Earth's gravity , the Moon
core of gravity may be defined as being -1/3 gravity.
The Earth as the measure of the gravity = 1 gravity measure may be defined as having the -1 gravity core of it's CHALK STATE.This equated
equivalence may be defined by the MANTLE of the Plasma states as they define the change from the surface and the layers of Mantle and Plasma core as
between the intervals of gravity interactions as
1 gravity surface = the chalk gravity core as the change of the force between the layers as the radius of 1 unit gravity of chalk as chalk has some fragmentation of it as
being finer grained and able to reduce it's molecular size without being altered when the displacement radius taking it to the core where it changes by temperature and friction that creates electricity or ionic heat increases.
So 1 gravity / radius =1 unit of surface chalk weight per unit measure of the 1m cubed.
These functions are related to the core of the milky way galaxy by the
1) barbers pole of spirals of red and white chalk shifts and the ring that continues to displace the spirals in their red and white chalk shifts.
2) the molecular measure of the ideal states of chalk as the cubic volume usable application by experiments to see how chalk from
Earth behaves in Moon gravity or on Mars as well as on Neptune or on Alpha Centaurii or on the Sirius star system or on the Andromeda galaxy and
all it's planets and stars including our own galaxy .
3) the measure of displacement of the Chalk as displaced beyond , by the way that it relates to the comparative of Moon chalk on Earth
or as Moon Chalk on Mars and any other planet in the milky way galaxy or other galaxies, so that this ability to SIFT CHALK through
FUNNELS indicates the reduction of flow reductions where the chalk reaches the FUNNEL LIMIT DIAMETER and as such the ability of
it to start to PLASMIFY at the limits of the FUNNEL width where the electricty of the friction may be controlled by using the diameter mechanism ,(shown below),
so that it acts like a switch of the universes chalk force.
our Sun as a G type star as the 5th type of star may have -5 gravity.
The observations of the core of the sun or any other star will not be visable by using gravity detection, rather ,the core will have states of lite weight related to
chalk and it's lite weight values. By making comparisons with the CHALK on the Moon as some specific gravity as 1/3 of the Earth's gravity , the Moon
core of gravity may be defined as being -1/3 gravity.
The Earth as the measure of the gravity = 1 gravity measure may be defined as having the -1 gravity core of it's CHALK STATE.This equated
equivalence may be defined by the MANTLE of the Plasma states as they define the change from the surface and the layers of Mantle and Plasma core as
between the intervals of gravity interactions as
1 gravity surface = the chalk gravity core as the change of the force between the layers as the radius of 1 unit gravity of chalk as chalk has some fragmentation of it as
being finer grained and able to reduce it's molecular size without being altered when the displacement radius taking it to the core where it changes by temperature and friction that creates electricity or ionic heat increases.
So 1 gravity / radius =1 unit of surface chalk weight per unit measure of the 1m cubed.
These functions are related to the core of the milky way galaxy by the
1) barbers pole of spirals of red and white chalk shifts and the ring that continues to displace the spirals in their red and white chalk shifts.
2) the molecular measure of the ideal states of chalk as the cubic volume usable application by experiments to see how chalk from
Earth behaves in Moon gravity or on Mars as well as on Neptune or on Alpha Centaurii or on the Sirius star system or on the Andromeda galaxy and
all it's planets and stars including our own galaxy .
3) the measure of displacement of the Chalk as displaced beyond , by the way that it relates to the comparative of Moon chalk on Earth
or as Moon Chalk on Mars and any other planet in the milky way galaxy or other galaxies, so that this ability to SIFT CHALK through
FUNNELS indicates the reduction of flow reductions where the chalk reaches the FUNNEL LIMIT DIAMETER and as such the ability of
it to start to PLASMIFY at the limits of the FUNNEL width where the electricty of the friction may be controlled by using the diameter mechanism ,(shown below),
so that it acts like a switch of the universes chalk force.
calcium carbonate has some basic crystallinity
from Wikipedia
date 2017, oct 05.
Aragonite is a carbonate mineral, one of the two most common, naturally occurring, crystal forms of calcium carbonate, CaCO3 (the other forms being the minerals calcite and vaterite). It is formed by biological and physical processes, including precipitation from marine and freshwater environments.
Aragonite's crystal lattice differs from that of calcite, resulting in a different crystal shape, an orthorhombic crystal system with acicular crystal. Repeated twinning results in pseudo-hexagonal forms. Aragonite may be columnar or fibrous, occasionally in branching stalactitic forms called flos-ferri ("flowers of iron") from their association with the ores at the Carinthian iron mines.
Vaterite is a mineral, a polymorph of calcium carbonate (CaCO3). It was named after the German mineralogist Heinrich Vater. It is also known as mu-calcium carbonate (μ-CaCO3) and has a JCPDS number of 13-192. Vaterite belongs to the hexagonal crystal system, whereas calcite is trigonal and aragonite is orthorhombic.
Vaterite, like aragonite, is a metastable phase of calcium carbonate at ambient conditions at the surface of the earth. As it is less stable than either calcite or aragonite, vaterite has a higher solubility than either of these phases. Therefore, once vaterite is exposed to water, it converts to calcite (at low temperature) or aragonite (at high temperature: ~60 °C). At 37 °C for example a solution-mediated transition from vaterite to calcite occurs, where the latter one dissolves and subsequently precipitates as calcite assisted by an Ostwald ripeningprocess.[4]
Here's VAterine
Here's Argonite
Both the Argonite and Vaterine have crystal functions that indicate the BRANCHING of CRYSTALLINITY and the shape of the crystals as being made of regular cubic shapes such as squares or pentagons or hexagons.
It may be that this crystalline development of the branching being derived from the zoom on it as the smaller Vaterine and zooming in more closely into the CHALK. So how does something as loose as Chalk remain solid. Well it's the action of gravity on the chalk that keeps it solid with the VATERINE and then the Argonite which branch the gravity to keep the CHALK solid with GRAVITY. That the Gravity of bodies in space are verged into a smaller angle may be indicated by the Argonite. and that the particles that do the gravity warping are the VATERINE that define crystals and their conductivity of gravity so that the chalk does the fragmentations of the source of gravity having this fine grain but in as many positions as the branches of Argonite have.
So then, the zoom in on the Argonite results in Varerine and zooming in more closely on Vaterine shows the Chalk powder. So that even when observing the forst cause of the chals it's deveopment in the core of the planets and stars will displace outwards by stages of the chalk to Vaterine to Argonite.
In this way then, the structure of the zoom in = the same structural change as each component taken together as each of them define the combined stages from the core chalk to the interval of VAterine to the outer Argomite.
So they are gravity interactive by creating the vectors of gravity in any direction of observation, be it zooming in or taking the whole as 3 units or 1 unit of gravity development as in stages or as together..
So that the above examples of the SIFTING and SPIRAL rotation of CHALK may be applied to the red as heat of chalk = the Vaterine or the
rotation of the whole as the Aronite stage and the chalk as the conductive and compressed state which also may rotate.
It may be that this crystalline development of the branching being derived from the zoom on it as the smaller Vaterine and zooming in more closely into the CHALK. So how does something as loose as Chalk remain solid. Well it's the action of gravity on the chalk that keeps it solid with the VATERINE and then the Argonite which branch the gravity to keep the CHALK solid with GRAVITY. That the Gravity of bodies in space are verged into a smaller angle may be indicated by the Argonite. and that the particles that do the gravity warping are the VATERINE that define crystals and their conductivity of gravity so that the chalk does the fragmentations of the source of gravity having this fine grain but in as many positions as the branches of Argonite have.
So then, the zoom in on the Argonite results in Varerine and zooming in more closely on Vaterine shows the Chalk powder. So that even when observing the forst cause of the chals it's deveopment in the core of the planets and stars will displace outwards by stages of the chalk to Vaterine to Argonite.
In this way then, the structure of the zoom in = the same structural change as each component taken together as each of them define the combined stages from the core chalk to the interval of VAterine to the outer Argomite.
So they are gravity interactive by creating the vectors of gravity in any direction of observation, be it zooming in or taking the whole as 3 units or 1 unit of gravity development as in stages or as together..
So that the above examples of the SIFTING and SPIRAL rotation of CHALK may be applied to the red as heat of chalk = the Vaterine or the
rotation of the whole as the Aronite stage and the chalk as the conductive and compressed state which also may rotate.