Weird Science

Sea of Rains, Lunar Mountains, and Craters

Polish ver­sion is here

Our Moon, the only natu­ral satel­lite of Earth, has always exer­ted a pro­fo­und influ­ence on vir­tu­ally all living orga­ni­sms. From a phy­si­cal and bio­lo­gi­cal per­spec­tive, its mass plays a cru­cial role in sta­bi­li­zing Earth’s axis of rota­tion. Without this effect, sud­den and uni­ma­gi­na­bly dra­stic cli­mate chan­ges would likely have pre­ven­ted life from deve­lo­ping at all. Thanks to the Moon’s gra­vi­ta­tio­nal pull, which is cle­arly visi­ble in the tidal phe­no­mena obse­rva­ble to the naked eye, Earth’s rota­tion has gra­du­ally slo­wed to its cur­rent rate. The lunar cycle also serves as a bio­lo­gi­cal rhy­thm regu­la­tor for many orga­ni­sms. For exam­ple, the coral spe­cies Acro­pora pal­mata always spawns at dusk three to four days after the full moon.

For humans, the Moon, being the nea­rest cele­stial body and pos­ses­sing sur­face fea­tu­res visi­ble to the naked eye, has influ­en­ced cul­ture and ima­gi­na­tion for cen­tu­ries. This is evi­dent in tra­di­tio­nal calen­dars used by many reli­gions, as well as in the divi­sion of the Gre­go­rian calen­dar into mon­ths and weeks. The lunar cycle also deter­mi­nes the timing of cer­tain reli­gious holi­days. In the Roman Catho­lic Church, for instance, Easter always falls on the first Sun­day after the first full moon of spring. In popu­lar ima­gi­na­tion, the cre­scent moon is often asso­cia­ted with lovers, while the full moon has long been lin­ked with less ple­a­sant sym­bols such as were­wo­lves and vam­pi­res.

Obse­rving our natu­ral satel­lite is rela­ti­vely sim­ple and highly rewar­ding. No spe­cia­li­zed equ­ip­ment is nee­ded for basic obse­rva­tions. A good pair of bino­cu­lars, a small tele­scope, or a camera with suf­fi­cient zoom is per­fec­tly ade­qu­ate.

Obse­rva­tion

April 2019, aro­und 11:00 PM – Zabo­rze (Poland)
sub­ur­ban con­di­tions, mode­rate light pol­lu­tion

The pho­to­graph below was taken as a so-cal­led one shot, mea­ning it was cap­tu­red without addi­tio­nal ima­ging tech­ni­ques, par­ti­cu­larly without stac­king. As a result, it clo­sely resem­bles what any­one can obse­rve thro­ugh bino­cu­lars. The image shows the nor­thern part of the lunar disk, with direc­tions (N, S, E, W) labe­led from the obse­rver’s per­spec­tive. A wider-field pho­to­graph with labels and descrip­tions can be found here.

The Sea of Rains (A, Mare Imbrium) is the second-lar­gest lunar mare and can easily be seen with the naked eye. To the east lies the smal­ler Sea of Sere­nity (B, Mare Sere­ni­ta­tis), distin­gu­i­shed by its nearly cir­cu­lar shape. This “sea” has a dia­me­ter of about 700 kilo­me­ters. South of these two areas is the Sea of Vapors (C, Mare Vapo­rum), while the Sea of Tra­nqu­i­lity (D, Mare Tra­nqu­il­li­ta­tis) is par­tially out­side the frame. To the north stret­ches the Sea of Cold (E, Mare Fri­go­ris). Simi­lar to maria, tho­ugh usu­ally smal­ler, are the lunar bays and lakes. Exam­ples inc­lude the Bay of Heat (F, Sinus Aestuum), as well as the Lake of Dre­ams (a, Lacus Som­nio­rum) and the Lake of Death (b, Lacus Mor­tis).

Lunar hills and moun­tain ran­ges are ano­ther fasci­na­ting fea­ture of the Moon’s land­scape. The pho­to­graph cle­arly shows the ran­ges sur­ro­un­ding Mare Imbrium. From south to north, these inc­lude the Car­pa­thian Moun­ta­ins (α, Mon­tes Car­pa­tus), the Apen­nine Moun­ta­ins (β, Mon­tes Apen­ni­nus), the Cau­ca­sus Moun­ta­ins (γ, Mon­tes Cau­ca­sus), the Alps (δ, Mon­tes Alpes), and the Jura Moun­ta­ins (ε, Mon­tes Jura). Within the Alps lies Mons Blanc (δ1), which rises to a hei­ght of appro­xi­ma­tely 3.6 kilo­me­ters. Sli­gh­tly to the north is the Alpine Val­ley (δ2, Val­lis Alpes), about 10 kilo­me­ters wide at its cen­tral sec­tion.

Impact cra­ters are also among the Moon’s most pro­mi­nent fea­tu­res. One of the most impres­sive for­ma­tions of this type is Coper­ni­cus (1), loca­ted in the eastern part of the Ocean of Storms (Oce­a­nus Pro­cel­la­rum), mostly out­side the frame. The cra­ter’s floor is about 46 kilo­me­ters in dia­me­ter, with a rim width of appro­xi­ma­tely 22 kilo­me­ters. The outer rim stands just over one kilo­me­ter high, while the inner walls rise to more than three times that hei­ght. The outer slo­pes are gen­tly inc­li­ned. Other labe­led cra­ters inc­lude Gay-Lus­sac (2), Era­to­sthe­nes (3), Archi­me­des (4), Auto­ly­cus (5), Ari­stil­lus (6), Timo­cha­ris (7), Lam­bert (8), Pytheas (9), Plato (10), Ari­sto­te­les (11), and Eudo­xus (12).

The fea­tu­res descri­bed here repre­sent only a small por­tion of the many fasci­na­ting deta­ils that can be obse­rved with com­monly ava­i­la­ble equ­ip­ment. After all, the pho­to­graph shows only a small sec­tion of the Moon’s disk. I enco­u­rage eve­ry­one to look up at our natu­ral satel­lite on a clear night. As a final tip, the easiest time to obse­rve the deta­ils of the Moon’s sur­face is during the cre­scent phase, near the ter­mi­na­tor line. Why? I think you’ll disco­ver the answer your­self.

Photo 1 Para­me­ters:

  • Total expo­sure time: 1/320 second
  • Canon EOS 60D
  • ISO: 500
  • Lens: zoom type (used at fmax = 250mm)
  • A fil­ter was used to reduce the effects of arti­fi­cial light pol­lu­tion and atmo­sphe­ric glow
  • Mount: pho­to­gra­phic tri­pod

Marek Ples

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