Another minor canyon on Mars that would be a world wonder on Earth
Click for original image.
Cool image time! The picture to the right, rotated, cropped, reduced, and sharpened to post here, was taken on August 6, 2023 by the high resolution camera on Mars Reconnaissance Orbiter (MRO). It shows the steep north canyon wall of one small part of the Martian canyon complex dubbed Noctis Labyrinthus
The elevation drop in this picture is about 8,000 feet, but the canyon’s lowest point is several miles further south and another 7,000 feet lower down. What is most intriguing about the geology here is its age. If you look at the full resolution image, you will see that there are scattered small craters on the smooth slopes that resemble sand that gravity and wind is shaping into those long streaks heading downhill.
Those craters, however tell us that these smooth slopes are very old, and have not changed in a long time. Furthermore, though the material appears to look like soft sand, the craters also tell us it long ago hardened into a kind of rock. If wind is shaping this material, it must be a very slow process.
The light areas on the rim as well as the ridge peaks below the rim suggest the presence of geological variety, which fits with other data that says Noctis Labyrinthus has a wide variety of minerals.
The white dot on the overview map to the right marks the location in Noctis Labyrinthus, east of Mars’ giant volcanoes and near the western beginnings of the 1,500-mile-long Valles Marineris canyon to the east.
Once again the monumental scale of Mars astonishes. This small canyon section of Noctis Labyrinthus is twenty miles wide at this point, with a depth of 15,000 feet or almost three miles. Its length is harder to determine because of the complexity of canyons here, but using the longest option it is about 250 miles long.
You could easily fit two Grand Canyons inside it, with space to spare. Yet it is merely one small canyon section in a maze of canyons almost 600 miles long and 200 miles wide.
Though the origins of Noctis Labyrinthus are as yet not completely understood, the generally accepted theory is that ground here was pushed up by volcanic activity, causing the ground to crack to form the initial canyons. Over time erosion, possibly linked to wind, water, ice, or lava, has widened those canyons.
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In 2020 when the world panicked over COVID I wrote that the panic was unnecessary, that the virus was apparently simply a variation of the flu, that masks were not simply pointless but if worn incorrectly were a health threat, that the lockdowns were a disaster and did nothing to stop the spread of COVID. Only in the past year have some of our so-called experts in the health field have begun to recognize these facts.
Your help allows me to do this kind of intelligent analysis. I take no advertising or sponsors, so my reporting isn't influenced by donations by established space or drug companies. Instead, I rely entirely on donations and subscriptions from my readers, which gives me the freedom to write what I think, unencumbered by outside influences.
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Click for original image.
Cool image time! The picture to the right, rotated, cropped, reduced, and sharpened to post here, was taken on August 6, 2023 by the high resolution camera on Mars Reconnaissance Orbiter (MRO). It shows the steep north canyon wall of one small part of the Martian canyon complex dubbed Noctis Labyrinthus
The elevation drop in this picture is about 8,000 feet, but the canyon’s lowest point is several miles further south and another 7,000 feet lower down. What is most intriguing about the geology here is its age. If you look at the full resolution image, you will see that there are scattered small craters on the smooth slopes that resemble sand that gravity and wind is shaping into those long streaks heading downhill.
Those craters, however tell us that these smooth slopes are very old, and have not changed in a long time. Furthermore, though the material appears to look like soft sand, the craters also tell us it long ago hardened into a kind of rock. If wind is shaping this material, it must be a very slow process.
The light areas on the rim as well as the ridge peaks below the rim suggest the presence of geological variety, which fits with other data that says Noctis Labyrinthus has a wide variety of minerals.
The white dot on the overview map to the right marks the location in Noctis Labyrinthus, east of Mars’ giant volcanoes and near the western beginnings of the 1,500-mile-long Valles Marineris canyon to the east.
Once again the monumental scale of Mars astonishes. This small canyon section of Noctis Labyrinthus is twenty miles wide at this point, with a depth of 15,000 feet or almost three miles. Its length is harder to determine because of the complexity of canyons here, but using the longest option it is about 250 miles long.
You could easily fit two Grand Canyons inside it, with space to spare. Yet it is merely one small canyon section in a maze of canyons almost 600 miles long and 200 miles wide.
Though the origins of Noctis Labyrinthus are as yet not completely understood, the generally accepted theory is that ground here was pushed up by volcanic activity, causing the ground to crack to form the initial canyons. Over time erosion, possibly linked to wind, water, ice, or lava, has widened those canyons.
Readers!
Please consider supporting my work here at Behind the Black. Your support allows me the freedom and ability to analyze objectively the ongoing renaissance in space, as well as the cultural changes -- for good or ill -- that are happening across America. Fourteen years ago I wrote that SLS and Orion were a bad ideas, a waste of money, would be years behind schedule, and better replaced by commercial private enterprise. Only now does it appear that Washington might finally recognize this reality.
In 2020 when the world panicked over COVID I wrote that the panic was unnecessary, that the virus was apparently simply a variation of the flu, that masks were not simply pointless but if worn incorrectly were a health threat, that the lockdowns were a disaster and did nothing to stop the spread of COVID. Only in the past year have some of our so-called experts in the health field have begun to recognize these facts.
Your help allows me to do this kind of intelligent analysis. I take no advertising or sponsors, so my reporting isn't influenced by donations by established space or drug companies. Instead, I rely entirely on donations and subscriptions from my readers, which gives me the freedom to write what I think, unencumbered by outside influences.
You can support me either by giving a one-time contribution or a regular subscription. There are four ways of doing so:
1. Zelle: This is the only internet method that charges no fees. All you have to do is use the Zelle link at your internet bank and give my name and email address (zimmerman at nasw dot org). What you donate is what I get.
2. Patreon: Go to my website there and pick one of five monthly subscription amounts, or by making a one-time donation.
3. A Paypal Donation or subscription:
4. Donate by check, payable to Robert Zimmerman and mailed to
Behind The Black
c/o Robert Zimmerman
P.O.Box 1262
Cortaro, AZ 85652
You can also support me by buying one of my books, as noted in the boxes interspersed throughout the webpage or shown in the menu above.
The crate marks also don’t look to be very deep nor have any side walls to speak of. Is this due to hardened rock -really hard? or a glancing blow or both?
It looks to be compressed ash, thousands of feet of identical texture/marbling, there’s no sediment layers like we see in other locations. Impact Craters hardly make a dent, no obvious erosion taking place in the sidewalls which is unusual. Could have drifting ash from the volcanoes mostly fallen thousands of feet thick in this one area? Mars atmosphere is thin, so the heavier ash will not go far.
I would point out the shadows being cast by the protrusions in the upper wall… You can’t see it from our angle but a shadow that is incredibly long (like Pinocchio‘s nose). An anomaly that may only be possible in low gravity.