The island may be only a few meters in height, it represents the first reference to the surrounding layers around it that are also separated by some depth of a lower height than the island. The fact that the first beach would always be there from the start is an impossibility. There has to be some first reference where the water weight pushes down on the soil and erodes it gradually over hundreds of years, for such a sized crater as "yezero".
So the first beach would be the layer indicated to the left or right as, where they match., in a position where the diagonal to the same level makes a full vector and the circumference may be the first beach at some height lower than the ,using an example of a few meters, meaning the lake is a smaller type of lake but the sea level would have to be higher, around the other side of the circumference and the time it takes for the water to fall to the lake level ,by an intake current will still be left as erosion. So the pressure of the larger mars oceans may be defined and the pressure reference to the flow of the ducts on the sides of yezero crater may be computed as their flow rate and the first water deposits. Or it could have collected by atmosphere moisture in which case the amounts may be found in the erosion and the rock hard values computed.
So the first beach would be the layer indicated to the left or right as, where they match., in a position where the diagonal to the same level makes a full vector and the circumference may be the first beach at some height lower than the ,using an example of a few meters, meaning the lake is a smaller type of lake but the sea level would have to be higher, around the other side of the circumference and the time it takes for the water to fall to the lake level ,by an intake current will still be left as erosion. So the pressure of the larger mars oceans may be defined and the pressure reference to the flow of the ducts on the sides of yezero crater may be computed as their flow rate and the first water deposits. Or it could have collected by atmosphere moisture in which case the amounts may be found in the erosion and the rock hard values computed.
from wikipedia
date 2019 15,07 The Mars ocean hypothesis states that nearly a third of the surface of Mars was covered by an ocean of liquid water early in the planet’s geologic history.[2][3][4] This primordial ocean, dubbed Paleo-Ocean[1] and Oceanus Borealis,[5] would have filled the basin Vastitas Borealis in the northern hemisphere, a region which lies 4–5 km (2.5–3 miles) below the mean planetary elevation, at a time period of approximately 4.1–3.8 billion years ago. Evidence for this ocean includes geographic features resembling ancient shorelines, and the chemical properties of the Martian soil and atmosphere.[6][7][8] Early Mars would have required a denser atmosphere and warmer climate to allow liquid water to remain at the surface.[9][10][11][12] |
When the launch window difference of an astronaut is related to the timing of the position, speed, displacement , the facts may be increased in reference to the first position of the relay of data back to ground base nasa.
basically, the wave effect of the launch window, could work out the water functions on Mars as it once was due to the fastest way that water covered Mars long ago and the wave effect of the remaining rotation that is not in the launch window angle and time = the remaining data on the re-entry window as using the "non re-entry angles and time" so that when dividing the two, the water multiple could be found as with the true angle and time as 3 variables of H2O. The H2O function could be defined as the "launch window" equated to the sling shoot and the change of buoyancy.
the distance to a planet when the Earth is in a minimal distance away from Earth and that position gives the spaceship going to Mars the curvature to make it to Mars with minimal wastage of fuel and also a chance to hop on the "sling shoot effect around the Sun" so that the spaceship accelerates around it and gains velocity by the Sun's gravity pull at a minimal angle that accelerates the spaceship that is moving faster ,the closer it gets to the Sun and faster as it displaces away from the gravity pull+ the rotational inertia of the Sun as it rotates in the same direction as the spaceship and increases the missing gravity as propulsion.
Mars launch window : by Wikipedia
date 2019, 15,07
basically, the wave effect of the launch window, could work out the water functions on Mars as it once was due to the fastest way that water covered Mars long ago and the wave effect of the remaining rotation that is not in the launch window angle and time = the remaining data on the re-entry window as using the "non re-entry angles and time" so that when dividing the two, the water multiple could be found as with the true angle and time as 3 variables of H2O. The H2O function could be defined as the "launch window" equated to the sling shoot and the change of buoyancy.
the distance to a planet when the Earth is in a minimal distance away from Earth and that position gives the spaceship going to Mars the curvature to make it to Mars with minimal wastage of fuel and also a chance to hop on the "sling shoot effect around the Sun" so that the spaceship accelerates around it and gains velocity by the Sun's gravity pull at a minimal angle that accelerates the spaceship that is moving faster ,the closer it gets to the Sun and faster as it displaces away from the gravity pull+ the rotational inertia of the Sun as it rotates in the same direction as the spaceship and increases the missing gravity as propulsion.
Mars launch window : by Wikipedia
date 2019, 15,07