GEOLOGY on Mars and future manned missions to Mars.
by Henryk Szubinski
The mission with 2 000 000 names on it where I'm included.
That sand as the matter of small crystals is not so interesting to the research missions to Mars
surface because sand exists everywhere. We can observe sand on our own planet Earth with the same characteristics as on
Mars. So why go to Mars?.
Because there are places on it that have hard rocks and these are needed for samples taken from it's surface by astronauts.
So what happens when an astronaut walks on Mars?.
He or She would experience the sand as the alpha value of the expansion of the HARD geology beneath the sand layer.
In this way there are inclines of HARD matter beneath the Sand and we are able to use these lower rocks to compute the
angles to which they displace to the surface where hard rocks are visually identifiable so that Astronauts know where to go.
In this way any position may be known as related to the SOLID UNDER SURFACE of these places that are thicker, geologically
and on which astronauts may walk safely while taking rocks with them back to Earth.
The reference to the SOLID PLACES of MARS may extend into the Core by way of the inner mantle as the ability to know the
topographical HIGH PLACES and the approach to Mars by the Insight mission as the reference to the depth and releif of the
variables of the types of sonic interactions with geology on Mars by the geological sound motion of earthquakes as they are
pressure indicative of their motion as the many variables of the responses around Mars, back and forth.
The change of the under surface hardness and its displaced projection to HARD surfaces on mars may be defined by the NEWTONIAN
INCLINE theory.
So then this defines the advantage of using water to compute the variability of depth of the lower "easy" surface and the "hard" surface
and the incline between them as the HARDNESS of the environment and the indication for the fluidity as = space. Meaning that space also is
"everywhere" because we could easily measure it around Earth. So the advantage is not about space, it's about the planetary alternative
use of the mapping of inclines and depth of hardness as action reaction, based. So that action reaction of the HARD= beta may become
delta dense.
These delta densities are then,related to their own topography by the ability to measure height in terms of the atmosphere and the
variations of the geological depth where there is hardness.
So then the forwards motion of astronauts need not make repeat missions depending on how fast the manned missions to Mars take as in time and the
knowledge of where to go by way of the map of the whole of the geology and the projections to future missions.
So the crystal structure of Mars would be valuable when samples of crystal are located and taken back to Earth as they have the data related to this
hard surface as the HARDEST SAMPLES to FIND.
The facts of the solidity on Mars, may be defined by the place on it where there are DENSE MATTER EVIDENCE by way of the vies from above Mars as having
CRYSTAL STRUCTURE.
The place :Antioniadi.
article from:
agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2011JE004038
date 2018
June 4
time, 11:40
Abstract[1] The only area on Mars where crystalline quartz has been identified from orbit is near Antoniadi Crater, on the northern edge of the Syrtis Major shield volcano. However, the method of quartz formation has remained unknown. In this study, we use high‐resolution satellite imagery as well as thermal and near‐infrared spectroscopy to construct a geologic history of these deposits and their local context. We find that the quartz‐bearing deposits are consistently co‐located with hydrated silica. This spatial coherence suggests that the quartz formed as a diagenetic product of amorphous silica, rather than as a primary igneous mineral. Diagenetic quartz is a mature alteration product of hydrated amorphous silica, and indicates more persistent water and/or higher temperatures at this site. Beneath the silica‐bearing rocks, we also find spectral evidence for smectites in the lowermost exposed Noachian‐aged breccia. A similar stratigraphic sequence — smectite‐bearing breccias beneath deposits containing minerals suggesting a greater degree of alteration — has also been found at nearby exposures at Nili Fossae and Toro Crater, suggesting a widespread sequence of alteration. By merging the mineral detections of thermal infrared (quartz, feldspar) and near‐infrared spectroscopy (hydrated silica, smectite clays) we are able to construct a more complete geologic history from orbit.
more on my theory.
The Newtonian theory of the inclination of Hard rocks beneath the surface of Mars as on an incline towards the surface protrusions where the samples may be taken by astronauts on their way home.
So the HARDNESS is INVERTED because the SURFACE of MARS facing the Sun will usually face the side opposite to Earth as opposite to Mars because Mars is mainly
observable in the night sky.
As spacial coherence:
from:
wiki.metropolia.fi/display/Physics/Spatial+and+Temporal+coherence
date 2018
June 4
time, 11:50
Spatial and Temporal coherenceSpatial coherence is a concept of wave disturbance describing the correlation between periodic transmitted energy (wave signals) from one point to another,it can also be said that it is a mutual interdependence or connection of variable wave quantities of two different points in a given instant of time,the coherence is presented as a function of distance and mapped as correlation against an absolute distance between points in question.
While spatial coherence is concerned with the phase correlation of waves in different observation points, temporal coherence entails the phase correlation of waves at a given point in space at two different instances of time,it is the measure of the average correlation between the value of a wave and itself delayed by a certain period of time depicting the characteristics of how well a wave can create an interference with itself.The delay on which the correlation effect is emphatically low is denoted by the degree of Tc (coherence time)[3], a state at which there is a significant shift in amplitude.