Geology <strong>of</strong> the Rimae HippalusPhil MorganTHE Mare Humorum (Sea <strong>of</strong> Moisture)is a circular basin roughly 400 kilometresin diameter, dating to the Nectariangeological period <strong>of</strong> <strong>lunar</strong> history, and likethe other circular Maria is a site <strong>of</strong> a positivegravity anomaly. In the late Imbrianera its interior was flooded by mare lavaproducing fine arcuate wrinkle ridges, particularlyaround the eastern half <strong>of</strong> thebasin, probably as a result <strong>of</strong> compressivestress. This compression produced a correspondingzone <strong>of</strong> tension around theperiphery <strong>of</strong> the basin, the results <strong>of</strong> whichwe can see today as a series <strong>of</strong> (mostly)arcuate rille systems, namely the RimaeAgatharchides, Hippalus, Mersenius andDoppelmayer. This article deals with theRimae Hippalus, in particular the regionaround the small crater Agatharchides A.Formed by crustal dilation and tectonicmovement <strong>of</strong> crustal blocks, the RimaeHippalus are a roughly parallel series <strong>of</strong>graben-type rilles that mark the easternboundary <strong>of</strong> the basin spanning a distance<strong>of</strong> some 250 kilometres. Best observed ataround colongitude 35° onwards at sunriseand about colongitude 200° onwards atsunset.Starting at the north at the old floodedcraters Agatharchides and Agatharchides Pas a trio <strong>of</strong> rilles, the Rimae Hippalus IIand III skirt around the crater <strong>of</strong> that name,whilst the Rima Hippalus I slices throughthe centre <strong>of</strong> it in a beautiful concentric arcas it heads towards the south. At this pointthey are joined by the shorter rille RimaHippalus V, and all peter out as they strikesouth towards the crater Vitello.Observationally, most <strong>of</strong> my <strong>studies</strong>have been centered round the small, butinteresting (18 km) crater AgatharchidesA. This crater was named Moore byWilkins, and in 1949 Patrick Moore (nowSir Patrick <strong>of</strong> course) discovered twodusky bands running up the inner west(IAU) wall <strong>of</strong> the crater using a 6-inchrefractor. Since this crater sits directly ontop <strong>of</strong> the Rima Hippalus II and there is nosign <strong>of</strong> the rille cutting through either thecrater floor or its ramparts, we can assumethat the crater is the younger <strong>of</strong> the two(though it’s not always emphatically thecase that that one feature overlying anotheris always the younger!)To the west <strong>of</strong> Agatharchides A the RimaHippalus II shows a considerable displacement.This break is not visible under earlysunrise conditions as it is hidden by thelong shadows striking westwards fromAgatharchides A. Just south <strong>of</strong> this displacementthe rille forks into two and theeastern branch runs northwards into thesouthern outer rampart <strong>of</strong> A. In fact thisarea is the centre <strong>of</strong> a zone <strong>of</strong> fracturingthat is radial to Mare Humorum and iscomplimentary to the more obvious concentricarcuate Hippalus rille system.Another dislocation sits directly underAgatharchides A. As the Rimae HippalusIII heads south it meets the north outerrampart <strong>of</strong> Agatharchides A, passes underthe west (IAU) wall and emerges to thesouth, curving to the west just east <strong>of</strong> theRima Hippalus III dislocation mentionedabove. Lunar maps show the RimaHippalus III continuing on south <strong>of</strong>Agatharchides A, but I believe this section<strong>of</strong> the rille was never connected directly tothe shorter north segment, although visuallyit does appear to do so to the Earthbased observer. Similar fractures can beseen along the Rima Hippalus I insideHippalus itself, and to the north. All aredextral (right handed) in their displace-The Hippalus area, mapped by Walter Goodacre in 1910 (left) and Percy Wilkins in 1946 (right). From the collection <strong>of</strong> Peter Grego.Page 8The New Moon <strong>December</strong> <strong>2008</strong>
ment. Just east <strong>of</strong> Agatharchides A anothershallow rille runs south and is bisected bythe Rima Hippalus IV. This rille is als<strong>of</strong>ractured along its length, herringbonefashion (see Lunar Orbiter image IV-132at right).As the Rima Hippalus III strikes southwardsbeyond Agatharchides A, the rilleskirts a small hill, recorded sometimes ashaving a summit craterlet. Observationallyat least, the rille at this point has a pronouncedbend eastwards. It is interestingto note that this sharp ‘bendaround’ is notconfirmed by the overhead Lunar Orbiterimages, although many observers haverecorded it as such in the past. Rükl alsoshows no great curvature here, though forthe most part he based his charts on theLunar Orbiter photos. This apparent <strong>lunar</strong>illusion is shown well on my drawing <strong>of</strong>2004 March 1 (see p.12). Allowing for thisrille’s position on the <strong>lunar</strong> sphere, some30° west <strong>of</strong> the Moon’s central meridian,and the resultant distortion in its shape(curvature), we would expect the bend <strong>of</strong>the rille around the small hill to appear lessto the Earth bound observer, and not, as isapparently the case, much more. Further<strong>studies</strong> by myself show that a section <strong>of</strong>the eastern half <strong>of</strong> the hill has fallen orslumped into the bottom <strong>of</strong> the rille.Whilst the extra shadow that this fallensection casts eastwards could explain anapparent increased curvature <strong>of</strong> the rille atAbove: Lunar Orbiter photo IV-132, at col. 48.66°. Credit: NASA.Below: Part <strong>of</strong> LAC 93 (featured on p.79-80 <strong>of</strong> The Times Atlas <strong>of</strong> the Moon) showingMare Humorum and Rimae Hippalus. <strong>No</strong>rth is at top. Credit: NASA.The New Moon <strong>December</strong> <strong>2008</strong>Page 9