Difference between revisions of "September 4, 2013"
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<em>image by [mailto:rsackett00@yahoo.com Ross Sackett]</em><br /> | <em>image by [mailto:rsackett00@yahoo.com Ross Sackett]</em><br /> | ||
<br /> | <br /> | ||
| − | Three of the largest volcanic centers on the Moon occur along a visual line in the middle of northern Oceanus Procellarum. At the | + | Three of the largest volcanic centers on the Moon occur along a visual line in the middle of northern Oceanus Procellarum. At the |
| − | northern end (right) is Rümker, the smallest and least conspicuous center. But Rümker is, like the other two volcanic centers, a unique | + | northern end (right) is Rümker, the smallest and least conspicuous center. But Rümker is, like the other two volcanic centers, a unique |
| − | landform, in this case a dome pile, a collection of overlapping volcanic domes. The individual domes are similar in size to stand-along | + | landform, in this case a dome pile, a collection of overlapping volcanic domes. The individual domes are similar in size to stand-along |
| − | domes such as those near Hortensius, but the collection rises about 800 m above the mare. Next in line is perhaps the most unique | + | domes such as those near Hortensius, but the collection rises about 800 m above the mare. Next in line is perhaps the most unique |
| − | structure on the Moon. The Aristarchus Plateau is probably mostly a structurally uplifted feature - like the nearby Harbinger Mountains - | + | structure on the Moon. The Aristarchus Plateau is probably mostly a structurally uplifted feature - like the nearby Harbinger Mountains - |
| − | that is covered by mare lavas and veneered with pyroclastic deposits erupted from the Cobra Head source vent of Schröter's Valley. | + | that is covered by mare lavas and veneered with pyroclastic deposits erupted from the Cobra Head source vent of Schröter's Valley. |
| − | The final unique volcanic center is the Marius Hills (left), another collection of volcanic vents, but this time mostly spread laterally rather | + | The final unique volcanic center is the Marius Hills (left), another collection of volcanic vents, but this time mostly spread laterally rather |
| − | than on top of each other. The 200 plus steep-sided cones rest on and some are partially embayed by a broad elevated area whose | + | than on top of each other. The 200 plus steep-sided cones rest on and some are partially embayed by a broad elevated area whose |
| − | eastern and northern limits are clearly seen here extending past the cones. Back in the late 1960s the colorful planetary scientist | + | eastern and northern limits are clearly seen here extending past the cones. Back in the late 1960s the colorful planetary scientist |
| − | pioneer Hal Marsursky speculated that these three anomalously big and exotic volcanic centers were along the equivalent of a terrestrial | + | pioneer Hal Marsursky speculated that these three anomalously big and exotic volcanic centers were along the equivalent of a terrestrial |
| − | mid-ocean spreading ridge. That would be a fundamental fracture in the lunar crust, and the three volcanic centers could be the | + | mid-ocean spreading ridge. That would be a fundamental fracture in the lunar crust, and the three volcanic centers could be the equivalents of Iceland, a unique volcanic island on Earth because of its formation on a spreading center. Ross' image does show that a series |
| − | + | of mare ridges connect the three volcanic centers, but the likely origin of these ridges is as low angle thrust faults marking rings due | |
| − | of mare ridges connect the three volcanic centers, but the likely origin of these ridges is as low angle thrust faults marking rings due | + | either to the putative Procellarum Impact Basin or an obliquely-formed Imbrium Basin. A basin ring fracture probably extends through the |
| − | either to the putative Procellarum Impact Basin or an obliquely-formed Imbrium Basin. A basin ring fracture probably extends through the | + | depth of the mare that it cuts but not necessarily entirely through the crust to some source of magma. Forty years after Hal's suggestion |
| − | depth of the mare that it cuts but not necessarily entirely through the crust to some source of magma. Forty years after Hal's suggestion | + | we known much more about the Moon, but still don't have a good explanation for the origins of these thrre volcanic centers. |
| − | we known much more about the Moon, but still don't have a good explanation for the origins of these thrre volcanic centers.<br /> | + | <br /> |
<br /> | <br /> | ||
<em>[mailto:tychocrater@yahoo.com Chuck Wood]</em><br /> | <em>[mailto:tychocrater@yahoo.com Chuck Wood]</em><br /> | ||
Latest revision as of 17:44, 14 March 2015
Three Unique Volcanic Centers
image by Ross Sackett
Three of the largest volcanic centers on the Moon occur along a visual line in the middle of northern Oceanus Procellarum. At the
northern end (right) is Rümker, the smallest and least conspicuous center. But Rümker is, like the other two volcanic centers, a unique
landform, in this case a dome pile, a collection of overlapping volcanic domes. The individual domes are similar in size to stand-along
domes such as those near Hortensius, but the collection rises about 800 m above the mare. Next in line is perhaps the most unique
structure on the Moon. The Aristarchus Plateau is probably mostly a structurally uplifted feature - like the nearby Harbinger Mountains -
that is covered by mare lavas and veneered with pyroclastic deposits erupted from the Cobra Head source vent of Schröter's Valley.
The final unique volcanic center is the Marius Hills (left), another collection of volcanic vents, but this time mostly spread laterally rather
than on top of each other. The 200 plus steep-sided cones rest on and some are partially embayed by a broad elevated area whose
eastern and northern limits are clearly seen here extending past the cones. Back in the late 1960s the colorful planetary scientist
pioneer Hal Marsursky speculated that these three anomalously big and exotic volcanic centers were along the equivalent of a terrestrial
mid-ocean spreading ridge. That would be a fundamental fracture in the lunar crust, and the three volcanic centers could be the equivalents of Iceland, a unique volcanic island on Earth because of its formation on a spreading center. Ross' image does show that a series
of mare ridges connect the three volcanic centers, but the likely origin of these ridges is as low angle thrust faults marking rings due
either to the putative Procellarum Impact Basin or an obliquely-formed Imbrium Basin. A basin ring fracture probably extends through the
depth of the mare that it cuts but not necessarily entirely through the crust to some source of magma. Forty years after Hal's suggestion
we known much more about the Moon, but still don't have a good explanation for the origins of these thrre volcanic centers.
Chuck Wood
Technical Details
Sept 1, 2013. 11" Celestron SCT with an ASI120MM camera; mosaic of three images, each a stack of 1000 frames.
Related Links
21st Century Atlas chartS 27 & 28.
Yesterday's LPOD: Too Dazzling for Morning Coffee?
Tomorrow's LPOD: A Russian Corner
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