ๆ้ใฏๆๅคใซใ้ ป็นใซ่ตทใใ
Moonquakes Surprisingly Common
ใชใๆ้ใฏใใใชใซๅคใใฎใงใใใใ๏ผใขใใญๆ้ข็้ธๆใซๆใซ่จญ็ฝฎใใใๅฐ้่จใฎๅๆใซใใใจใๆ้ขใใ100ใญใญใกใผใใซไปฅๅ
ใฎๅฐ่กจไป่ฟใง้ฉใใปใฉๅคใใฎๆ้ใ็บ็ใใฆใใใใจใๆใใใซใชใใพใใใๅฎ้ใ1972ๅนดใใ1977ๅนดใฎ้ใซ่จ้ฒใใใใใผใฟใงใฏใ62ๅใฎๆ้ใๆคๅบใใใฆใใพใใใใใใฎๆ้ใฎๅคใใฏใๆ้ขใขใใผใใฎๅฎถๅ
ทใๅใใใปใฉใฎๅผทใใงใใใ ใใงใชใใๆใฎ็กฌใๅฒฉ็ณใฏๅฐ็ใฎๆใใใๅฒฉ็ณใง็บ็ใใๅฐ้ใใใใฏใใใซ้ทใๆฐๅ้ๆฏๅใ็ถใใพใใๆ้ใฎๅๅ ใฏๆชใ ไธๆใงใใใๆๅใชไปฎ่ชฌใฎไธใคใจใใฆใๅฐ็ใใใฎๆฝฎๆฑ้ๅใจๅฐ็ใซใใ็ธๅฏพ็ใชๅ ็ฑใๆใใใใฆใใพใใๅๅ ใไฝใงใใใๅฐๆฅใฎๆ้ขๅฑ
ไฝๆฝ่จญใฏใ้ ป็นใซ็บ็ใใๆ้ใซ่ใใใใใใใซๅปบ่จญใใๅฟ
่ฆใใใใพใใๅ็ใงใฏใใขใใญ11ๅทใฎๅฎๅฎ้ฃ่กๅฃซใใบใปใชใซใใชใณใใๆ่ฟ่จญ็ฝฎใใใๆ้ขๅฐ้่จใฎๆจชใซ็ซใกใๆ็้ธ่นใฎๆนใๆฏใ่ฟใฃใฆใใพใใๅฎๅฎใๆขๆคใใใ๏ผใฉใณใใ APODใธใงใใฌใผใฟใผ
ๅๆ๏ผEnglish๏ผ
Why are there so many moonquakes? Analyses of seismometers left on the moon during the Apollo moon landings reveal a surprising number of moonquakes occurring within 100 kilometers of the surface. In fact, 62 moonquakes were detected in data recorded between 1972 and 1977. Many of these moonquakes are not only strong enough to move furniture in a lunar apartment, but the stiff rock of the moon continues to vibrate for many minutes, significantly longer than the softer rock earthquakes on Earth. The cause of the moonquakes remains unknown, but a leading hypothesis includes tidal gravity from -- and relative heating by -- our Earth. Regardless of the source, future moon dwellings need to be built to withstand the frequent shakings. Pictured here, Apollo 11 astronaut Buzz Aldrin stands beside a recently deployed lunar seismometer, looking back toward the lunar landing module. Explore Your Universe: Random APOD Generator
๏ผผ ใใฎๆๅใๅฎๅฎไปฒ้ใซใทใงใข ๏ผ
ๅฎๅฎใXใงใทใงใข
ยฉ NASA / APOD