In the
history of lunar exploration, the mysterious association of craters
and rilles has provoked a number of mutually contradictory
hypotheses, none of which is sufficient to explain things seen in
high-resolution pictures of the Moon.
In our previous looks at the lunar craters
Tycho
and Aristarchus, we observed that the popular
“explanation” (the impact hypothesis) is contradicted by features
that, in close-up photographs, invariably leap out at the critical
observer.
Similarly, when we consider details of the
“sinuous rilles”
Schroeter’s Valley and
Hadley, we
discover that common teachings require things that are not
there while ignoring things that are there.
The message conveyed by these prominent lunar
features carries broad implications for our understanding of the
lunar surface at all scales of observation. Our claim has been that
theoretical assumptions in planetary science—including the most
popular teachings in lunar geology—cannot withstand a critical
review.
Yet there is a vantage point from which the
accumulated anomalies and contradictions disappear. The electric
hypothesis does not arbitrarily separate issues of crater formation
from issues of rille formation. In one instance after another, we
see that craters and rilles stand in a partnership that is far too
pervasive to be accidental. And this convergence is
predictable under the electric hypothesis.
Dominating craters on the Moon are surrounded
by non-radial crater chains, irregular concentrations of smaller
craters, sinuous or filamentary channels, and deep gashes—the very
features seen in electrical arcing experiments and in electrical
discharge machining in industrial applications. To underscore these
surface patterns on the Moon, we have placed two large images of the
Euler Crater region
here and
here. (The files are
large—1.5mb and 1.8mb respectively—but they are worth the look).
The pictures show innumerable small crater
concentrations, crater chains, and gashes, one form merging with
another in every imaginable way. A modest number of the gashes might
be mistaken for impacts at oblique angles, were it not for the
repeated instances in which the gashes are constituted
of overlapping craters, or are too long, or change
direction—attributes that exclude “explanation-by-impact”. In this
sense, an unbending adherence to the impact theory can only
encourage theorists to ignore these defining features on the lunar
surface.
The standard picture only grows more
incoherent when we consider the numerous rilles and enigmatic
channels that are conventionally “explained” as lava erosion. Why do
they exhibit craters and crater chains
of a sort never found in association with known
remains of flowing lava? Look at the higher-resolution image we
presented earlier of the Aristarchus region
here. In the
lower left of the picture is a rille that divides into twin
channels, both of which end in large craters. Could this anomalous
channel have been formed by flowing liquid of any kind? It is
simultaneously a crater chain and a rille, confirming the point made
repeatedly by the electrical theorist Wallace Thornhill: The same
force that produces crater chains produces rilles.
Rilles often exhibit craters deeper or wider
than the channels on which they are centered. For a good example,
consider the picture of Rima Hyginus
here. In many instances
the larger craters centered on a rille appear at the “joints” of a
meandering channel. Could they be “collapsed lava tubes,” a
once-popular hypothesis? It is only necessary to look closely to see
that these formations never reveal rubble from
a collapsed “roof”.
Not infrequently, we also observe a secondary
stream of smaller craters meandering down the rille, as we saw along
the floor of Schroeter’s Valley. The electrical theorists point to
analogs in both laboratory arcs and in lightning-excavated
trenches. On the moon, a fascinating example is Vallis Alpes, a
spectacular channel that extends some 166 kilometers, cutting across
the mountain range Montes Alpes. Clearly, it was not cut by flowing
liquid! See pictures
here and
here. Along its mid
section it is about 10 kilometers wide. Meandering down the center
of the flat valley floor is a narrow rille punctuated by
circular craters.
Inexplicable gashes emerging from craters or
converging with crater chains are ubiquitous on the lunar surface.
Our picture of Hadley Rille above, recently taken by the ESA
SMART-1, shows an “inexplicable” gash on the far left. The long and
deep gash emerges from the narrow end of a balloon-like crater to
cut across Hadley. It certainly has no explanation in standard
theory, and most lunar scientists simply address it as a “gash” and
go on to something they “understand”.
To put all of this in perspective, we must remember that the craters,
rilles, crater chains, and gashes on the Moon can now be
systematically compared to analogs on other bodies to see whether
scientists have been able to forge a coherent interpretation. We
find that, as the quality of the pictures has improved, the
interpretations have grown increasingly fragmented and bizarre. For
a telling comparison of the lunar enigmas to those presented on
another body, look at the so-called “collapse pits”
on the Martian “volcano”
Arsia Mons. All of the lunar enigmas are
there in one place—craters, crater chains, gashes, and rilles—except
that here the stunning clarity of the pictures gives common sense a
distinct advantage. Are these formations the result of “surface
collapse”, or has material been cleanly removed from
the surface by a force unknown to planetary scientists? In a
contest with the inertia of prior belief, common sense will surely
win out in the end.
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