INSIGHT LANDING MISSION will arrive at Mars by about 3 days from today, 23 of November 2018.
POSSIBLE
MARS ,EARTH and it's GEOLOGY similarities,
comparative method
by Henryk Szubinski
The core values of the temperature inside the MARS core =
The core is about 1500 degrees Kelvin, or 1230 Celsius. This may not be too hot compared to the cores of most celestial bodies, but it is hot enough at strong enough pressure for the iron, nickel and sulfur core of mars to melt.
While the EARTH core is 3 times larger or as the planet size itself, the temperature would be the EARTH CORE TEMPERATURE divided by 3
=
10,800 F
A team of scientists has measured the melting point of iron at high precision in a laboratory, and then drew from that result to calculate the temperature at the boundary of Earth's inner and outer core — now estimated at 6,000 C (about 10,800 F). That's as hot as the surface of the sun
as 6000 C/3 = 2000 C which in relationship to the core temperature of MARS as 1230 C. Meaning the difference of the :
2000-1230=770 C
So in relation to the true size of the MARS and EARTH, the 770 C may define more activity inside MARS that displaces from
the inner core to the layers between the surface.
What types of HARD ROCKS are = 770 C
Here are the EARTH type rocks that are shaped at 770 degrees celcius ,approximate because it will move from the GEOLOGICAL LAYERS
of MARS.
The article on them as from the HIMALAYAN BELT is :
from NASA,
/www.science.gov/topicpages/c/calc-silicate+metamorphic+rocks
date 2018
November 23
Titanite-bearing calc-silicate rocks constrain timing, duration and magnitude of metamorphic CO2 degassing in the Himalayan belt
NASA Astrophysics Data System (ADS)
Rapa, Giulia; Groppo, Chiara; Rolfo, Franco; Petrelli, Maurizio; Mosca, Pietro; Perugini, Diego
2017-11-01
The pressure, temperature, and timing (P-T-t) conditions at which CO2 was produced during the Himalayan prograde metamorphism have been constrained, focusing on the most abundant calc-silicate rock type in the Himalaya. A detailed petrological modeling of a clinopyroxene + scapolite + K-feldspar + plagioclase + quartz ± calcite calc-silicate rockallowed the identification and full characterization - for the first time - of different metamorphic reactions leading to the simultaneous growth of titanite and CO2 production. The results of thermometric determinations (Zr-in-Ttn thermometry) and U-Pb geochronological analyses suggest that, in the studied lithology, most titanite grains grew during two nearly consecutive episodes of titanite formation: a near-peak event at 730-740 °C, 10 kbar, 30-26 Ma, and a peak event at 740-765 °C, 10.5 kbar, 25-20 Ma. Both episodes of titanite growth are correlated with specific CO2-producing reactions and constrain the timing, duration and P-T conditions of the main CO2-producing events, as well as the amounts of CO2 produced (1.4-1.8 wt% of CO2). A first-order extrapolation of such CO2 amounts to the orogen scale provides metamorphic CO2 fluxes ranging between 1.4 and 19.4 Mt/yr; these values are of the same order of magnitude as the present-day CO2 fluxes degassed from spring waters located along the Main Central Thrust. We suggest that these metamorphicCO2 fluxes should be considered in any future attempts of estimating the global budget of non-volcanic carbon fluxes from the lithosphere.
Basically the height of TIBET and the MOUNTAINS, there, have the top surface position by an extension of the 8000 meters approximately, for the highest point being Mt EVEREST at 8,848 m as compared to the type of ROCK that FLOATS up on the HIMALAYAN BELT , so it would make sense that the MARS radius inwards by 8000 meters or 8 8 8 48 meters would be the position of this rock type.
MARS RADIUS =3,390 km
So then, the resulting INNER MARS reference to the HIMALAYAN BELT=
3 390 km -8.848
=3381.152 km
this is almost the ,
3 389 km to the SURFACE of MARS shown on the image of MARS CORE.
So this would be where the +- 8 848 meters that defines the SURFACE TOPOGRAPHY
as HIGH and LOW surface of MARS.
credit,
Nature.
POSSIBLE
MARS ,EARTH and it's GEOLOGY similarities,
comparative method
by Henryk Szubinski
The core values of the temperature inside the MARS core =
The core is about 1500 degrees Kelvin, or 1230 Celsius. This may not be too hot compared to the cores of most celestial bodies, but it is hot enough at strong enough pressure for the iron, nickel and sulfur core of mars to melt.
While the EARTH core is 3 times larger or as the planet size itself, the temperature would be the EARTH CORE TEMPERATURE divided by 3
=
10,800 F
A team of scientists has measured the melting point of iron at high precision in a laboratory, and then drew from that result to calculate the temperature at the boundary of Earth's inner and outer core — now estimated at 6,000 C (about 10,800 F). That's as hot as the surface of the sun
as 6000 C/3 = 2000 C which in relationship to the core temperature of MARS as 1230 C. Meaning the difference of the :
2000-1230=770 C
So in relation to the true size of the MARS and EARTH, the 770 C may define more activity inside MARS that displaces from
the inner core to the layers between the surface.
What types of HARD ROCKS are = 770 C
Here are the EARTH type rocks that are shaped at 770 degrees celcius ,approximate because it will move from the GEOLOGICAL LAYERS
of MARS.
The article on them as from the HIMALAYAN BELT is :
from NASA,
/www.science.gov/topicpages/c/calc-silicate+metamorphic+rocks
date 2018
November 23
Titanite-bearing calc-silicate rocks constrain timing, duration and magnitude of metamorphic CO2 degassing in the Himalayan belt
NASA Astrophysics Data System (ADS)
Rapa, Giulia; Groppo, Chiara; Rolfo, Franco; Petrelli, Maurizio; Mosca, Pietro; Perugini, Diego
2017-11-01
The pressure, temperature, and timing (P-T-t) conditions at which CO2 was produced during the Himalayan prograde metamorphism have been constrained, focusing on the most abundant calc-silicate rock type in the Himalaya. A detailed petrological modeling of a clinopyroxene + scapolite + K-feldspar + plagioclase + quartz ± calcite calc-silicate rockallowed the identification and full characterization - for the first time - of different metamorphic reactions leading to the simultaneous growth of titanite and CO2 production. The results of thermometric determinations (Zr-in-Ttn thermometry) and U-Pb geochronological analyses suggest that, in the studied lithology, most titanite grains grew during two nearly consecutive episodes of titanite formation: a near-peak event at 730-740 °C, 10 kbar, 30-26 Ma, and a peak event at 740-765 °C, 10.5 kbar, 25-20 Ma. Both episodes of titanite growth are correlated with specific CO2-producing reactions and constrain the timing, duration and P-T conditions of the main CO2-producing events, as well as the amounts of CO2 produced (1.4-1.8 wt% of CO2). A first-order extrapolation of such CO2 amounts to the orogen scale provides metamorphic CO2 fluxes ranging between 1.4 and 19.4 Mt/yr; these values are of the same order of magnitude as the present-day CO2 fluxes degassed from spring waters located along the Main Central Thrust. We suggest that these metamorphicCO2 fluxes should be considered in any future attempts of estimating the global budget of non-volcanic carbon fluxes from the lithosphere.
Basically the height of TIBET and the MOUNTAINS, there, have the top surface position by an extension of the 8000 meters approximately, for the highest point being Mt EVEREST at 8,848 m as compared to the type of ROCK that FLOATS up on the HIMALAYAN BELT , so it would make sense that the MARS radius inwards by 8000 meters or 8 8 8 48 meters would be the position of this rock type.
MARS RADIUS =3,390 km
So then, the resulting INNER MARS reference to the HIMALAYAN BELT=
3 390 km -8.848
=3381.152 km
this is almost the ,
3 389 km to the SURFACE of MARS shown on the image of MARS CORE.
So this would be where the +- 8 848 meters that defines the SURFACE TOPOGRAPHY
as HIGH and LOW surface of MARS.
credit,
Nature.
Lets define what is in the EARTH CORE at the radius of
3389 km
Need for addition.
3389 km
Need for addition.
64 km + 2980 km
=3044 km
Next addition layer
3044 km+ 725 km
=3769 km
This is beyond the MARS 3389 km
by about : 3769 km - 3389 km
=380 km from the ASTHENOSPHERE of EARTH as the COMPARISON with where MARS is positioned in reference to the RADIUS of MARS.
What is the ASTHENOSPHERE :
credit
Wikipedia
date 2018
November 23
The asthenosphere (from Greek ἀσθενής asthenḗs 'weak' + "sphere") is the highly viscous, mechanically weak[1] and ductilely deforming region of the upper mantle of the Earth. It lies below the lithosphere, at depths between approximately 80 and 200 km (50 and 120 miles) below the surface. The Lithosphere-Asthenosphere boundary is usually referred to as LAB.[2][3] The asthenosphere is almost solid, although some of its regions could be molten (e.g., below mid-ocean ridges). The lower boundary of the asthenosphere is not well defined. The thickness of the asthenosphere depends mainly on the temperature. However, the rheology of the asthenosphere also depends on the rate of deformation,[4]which suggests that the asthenosphere could be also formed as a result of a high rate of deformation. In some regions the asthenosphere could extend as deep as 700 km (430 mi). It is considered the source region of mid-ocean ridge basalt (MORB).[5]
=3044 km
Next addition layer
3044 km+ 725 km
=3769 km
This is beyond the MARS 3389 km
by about : 3769 km - 3389 km
=380 km from the ASTHENOSPHERE of EARTH as the COMPARISON with where MARS is positioned in reference to the RADIUS of MARS.
What is the ASTHENOSPHERE :
credit
Wikipedia
date 2018
November 23
The asthenosphere (from Greek ἀσθενής asthenḗs 'weak' + "sphere") is the highly viscous, mechanically weak[1] and ductilely deforming region of the upper mantle of the Earth. It lies below the lithosphere, at depths between approximately 80 and 200 km (50 and 120 miles) below the surface. The Lithosphere-Asthenosphere boundary is usually referred to as LAB.[2][3] The asthenosphere is almost solid, although some of its regions could be molten (e.g., below mid-ocean ridges). The lower boundary of the asthenosphere is not well defined. The thickness of the asthenosphere depends mainly on the temperature. However, the rheology of the asthenosphere also depends on the rate of deformation,[4]which suggests that the asthenosphere could be also formed as a result of a high rate of deformation. In some regions the asthenosphere could extend as deep as 700 km (430 mi). It is considered the source region of mid-ocean ridge basalt (MORB).[5]
INSIGHTS.
MARS Asthenosphere would be cooler than the Earth's Asthenosphere. This would account for the HIMALAYAN BELT INFLUENCE of the ROCKS higher up being cooled faster than the inner rock samples.
Made my own rule:
The rule : No inner planet core may decrease beyond the temperature of the surface topography as related to the COOLER TEMPERATURE of SPACE outside it.
So that CAMBRIAN VOLCANISM may have occurred previously in MARS history by way of the motion of Asthenosphere lava displaced to the surface and up
into the OPEN ATMOSPHERE that is colder and then cooled the lava into the resulting CONTINENTAL CRUST of MARS.
The PROTO TETHYAN OCEAN of MARS would have been pulled upwards with the VOLCANISM on it's surface and then evaporated as part of the cooling of the
Asthenosphere molten lava that made it to the surface.
There are some vectors that water would take in cases of large evaporation of the oceans that were on MARS.
This would have occurred by the motion of the OCEANIC CRUST that is closest to the ASTHENOSPHERE
and will define H2O displacement in the UP direction giving the feel that water is LIFTING or is taking part in the
negative gravity of the planet MARS at this stage in it's development.
Just like the DYKES on Earth, the water reaches very high temperatures and are very hot gaseous state of H2O.
So this gaseous state of the OCEANIC CRUST is actually LIFTING the MARS LITHOSPHERIC MANTLE together with
the GEOLOGICAL ACTIVITY of the other layers such as the LITHOSPHERIC MANTLE.
The thing being that the GASEOUS COOLING of the : theorem
OCEANIC / LITHOSPHERIC = LITHOSPHERIC / DYKES
The dyke is the closest to the separation of the MANTLE as the SEPARATION of the LITHOSPHERE 1 and the LITHOSPHERE 2.
The thing separating them being the OCEAN CRUST as it DIVES DEEPEST into MARS as the layer between the LITHOSPHERES 1 and 2
as 1/2=0.5 as the mean +- H2O of the OCEAN CRUST that hangs along as gaseous water.
Just basic GEOMETRY of the thing being divided and the thing doing the division.
Because the gravity of Mars is 1/3 rd that of Earth, the effect on the H2O as the gaseous temperature state might be higher , meaning that it could
be displacing with Mars along the motion of MARS DYKES ad their INERTIA. effect as along the incline angle of the DYKES to the Mars surface.
image credit
news.mthai.com
You may observe the SECTIONING of the HARD ROCK by LAVA as the water around it evaporates and the conditions for the DYKE SECTION through the MID SECTION of the HARD ROCK.
This is what happens in relation to MINIM EVENTS of the creation of the
LITHOSPHERE 1 left side of the hard rock and the right side as the LITHOSPHERE 2 while the OCEANIC CRUST MATTER is created to displace between them on the side closest to the gaseous temperature of the water.
These rocks will, depending on the gravity , fall at different velocities through the water to the ocean floor. On Earth they fall regularly while on MARS the gravity 1/3 of Earth's will make them fall slower, so the lava has time to interact with the lower levels of the ocean crust.
So in case Mars had an ocean environment, these molten CLOVEN ROCKS would have interacted with the LITHOSPHERIC LAYERS and the DYKES by moving upwards due to the lower gravity of MARS as compared to it's BUOYANCY LEVEL of the water being lower than that of Earth's oceans and being similar to negative gravity.
As such they would have displaced or floated upwards and then cooled on the MARS surface.
image credit
Mars.NASA.gov.
These small spherules on the Martian surface are near Fram Crater, visited by NASA's Mars Exploration Rover Opportunity during April 2004. The area shown is 1.2 inches (3 centimeters) across....
This is what happens in relation to MINIM EVENTS of the creation of the
LITHOSPHERE 1 left side of the hard rock and the right side as the LITHOSPHERE 2 while the OCEANIC CRUST MATTER is created to displace between them on the side closest to the gaseous temperature of the water.
These rocks will, depending on the gravity , fall at different velocities through the water to the ocean floor. On Earth they fall regularly while on MARS the gravity 1/3 of Earth's will make them fall slower, so the lava has time to interact with the lower levels of the ocean crust.
So in case Mars had an ocean environment, these molten CLOVEN ROCKS would have interacted with the LITHOSPHERIC LAYERS and the DYKES by moving upwards due to the lower gravity of MARS as compared to it's BUOYANCY LEVEL of the water being lower than that of Earth's oceans and being similar to negative gravity.
As such they would have displaced or floated upwards and then cooled on the MARS surface.
image credit
Mars.NASA.gov.
These small spherules on the Martian surface are near Fram Crater, visited by NASA's Mars Exploration Rover Opportunity during April 2004. The area shown is 1.2 inches (3 centimeters) across....
image credit
Pintrest.
Mars SAND DOMES
Pintrest.
Mars SAND DOMES
SAND DOME EROSION into DUNES.
image credit
HIRISE
image credit
HIRISE
That the WAY UP for the HARD ROCKS and their way to float upwards in the PROTO OCEAN of MARS means that as they LIFTED by the GASEOUS WATER , like balloons to the ocean surface that they then mixed with oxygen and became the BLUE OXIDE of the BLUE ROCK TYPES.Meaning that the BUBBLEs of H2O gaseous particles lifted upwards the rocks but also lifted the heavier metals to the surface.
Cobalt blue is a blue pigment made by sintering cobalt(II) oxide with alumina at 1200 °C. Chemically, cobalt blue pigment is cobalt(II) oxide-aluminium oxide, or cobalt(II) aluminate, CoAl2O4. Cobalt blue is lighter and less intense than the (iron-cyanide based) pigment Prussian blue. It is extremely stable and has historically been used as a coloring agent in ceramics (especially Chinese porcelain), jewelry, and paint. Transparent glasses are tinted with the silica-based cobalt pigment smalt.
image credit
Seeker.
With the water acting as the floaters for every type of mineral and metal , Mars must have those elements floating around on the surface and mixed with water in various states of solid, fluid ,gaseous and plasma.
Here is an image that might indicate the presence of MERCURY floating about on the MARS surface.
image credit
Sciencealert.com
Here is an image that might indicate the presence of MERCURY floating about on the MARS surface.
image credit
Sciencealert.com
The colder temperatures on MARS could be freezing some of the elements and metals but also other metals such as copper, nickel ,and Galiuim that melts at room temperature.
Even the MINERALS such as QUARTZ could be pulverised and mixed with the water on Mars ,giving the TRANSPARENCY EFFECT.
You think that walking on Mars might be easy, but it's possible you would be walking in a QUARTZ LAKE.
image credit
Pintrest
Mercury ripple.
Very similar to the features seen on MARS.
Even the MINERALS such as QUARTZ could be pulverised and mixed with the water on Mars ,giving the TRANSPARENCY EFFECT.
You think that walking on Mars might be easy, but it's possible you would be walking in a QUARTZ LAKE.
image credit
Pintrest
Mercury ripple.
Very similar to the features seen on MARS.
image credit,
The Awesomedaily.com
on another note:
What you are observing is the fluid type ocean on the right as the light effect that displaces into it from the left side of the image where there is a higher level HILL . The light play is the same as when you observe the ripples on water and observe them as on the floor of a shallow ocean floor. To be so deep in the reflection onto the floor , the fluid has to be very clear and could possibly be avoiding detection by the satellites because it is either metallic or mineral matter mixed into new types of water MIXES that are as yet unknown of on Earth.
Imagine diving into this ocean of infinite clarity and eternal peace of mind and calm resolve.
the image is of the TLEILAX DUNES or ALIEN FLUIDITY of the DUNE SCAPE that has water on it's right side.
The light reflections not as varied as the image of Earth water (shown below) This means that the fluidity seen
above,on MARS , must be denser than the fluidity of water in the state shown below.
Had you been an astronaut and dived into this FLUID OCEAN you would be floating around like in zero gravity.
But in fact you might be floating around because the fluidity is as real as water, we just haven't been able to
identify it as the same .
We have gone from STONE AGE TIMES as getting it right by GUESSING the evolutionary step and then using
statistics to place our feet on the Moon. But why do we still search?.Don't we know that it is because water that
we made the right guess. In any case we are getting it right. We have found water on most of the planets in the solar system
and other star systems and even other galaxies. So the point should be clear that , to follow water , is to get to the
right place. So we have to recognize the presence of water in TOTALLY NEW ENVIRONMENTS such as i have
set out for , in this theory , that water may have different buoyancy depending on the planet gravity and this
gravity makes water float in different MIX STATES of the elements of metals and minerals. So there must be
infinite and eternal amounts of this POSSIBLE MIX RESULTS and the way we may observe them as real when
we discover that we are on MARS and in some places that we are floating around in it's THICK LIQUIDS where
the LIGHT EFFECTS of the SUN are the only thing we need to identify this SPECIAL FLUIDITY that places us in
the circumstances of light, ripples , reflections and slow motion interaction where we become the CENTER of our
birth on other planets.
credit
Pintrest
The Awesomedaily.com
on another note:
What you are observing is the fluid type ocean on the right as the light effect that displaces into it from the left side of the image where there is a higher level HILL . The light play is the same as when you observe the ripples on water and observe them as on the floor of a shallow ocean floor. To be so deep in the reflection onto the floor , the fluid has to be very clear and could possibly be avoiding detection by the satellites because it is either metallic or mineral matter mixed into new types of water MIXES that are as yet unknown of on Earth.
Imagine diving into this ocean of infinite clarity and eternal peace of mind and calm resolve.
the image is of the TLEILAX DUNES or ALIEN FLUIDITY of the DUNE SCAPE that has water on it's right side.
The light reflections not as varied as the image of Earth water (shown below) This means that the fluidity seen
above,on MARS , must be denser than the fluidity of water in the state shown below.
Had you been an astronaut and dived into this FLUID OCEAN you would be floating around like in zero gravity.
But in fact you might be floating around because the fluidity is as real as water, we just haven't been able to
identify it as the same .
We have gone from STONE AGE TIMES as getting it right by GUESSING the evolutionary step and then using
statistics to place our feet on the Moon. But why do we still search?.Don't we know that it is because water that
we made the right guess. In any case we are getting it right. We have found water on most of the planets in the solar system
and other star systems and even other galaxies. So the point should be clear that , to follow water , is to get to the
right place. So we have to recognize the presence of water in TOTALLY NEW ENVIRONMENTS such as i have
set out for , in this theory , that water may have different buoyancy depending on the planet gravity and this
gravity makes water float in different MIX STATES of the elements of metals and minerals. So there must be
infinite and eternal amounts of this POSSIBLE MIX RESULTS and the way we may observe them as real when
we discover that we are on MARS and in some places that we are floating around in it's THICK LIQUIDS where
the LIGHT EFFECTS of the SUN are the only thing we need to identify this SPECIAL FLUIDITY that places us in
the circumstances of light, ripples , reflections and slow motion interaction where we become the CENTER of our
birth on other planets.
credit
Pintrest