Panginten kieu ngabentenkeunana teh, ieu mah ceuk pamadegan abdi.
Upami vulkanik biasana sok aya kaitanana sareng tektonik, maksadna sok dibarengan oge sareng gempa tektonik. Tapi tektonik teu acan tangtos vulkanik. Gempa vulkanik biasana sok ngaluarkeun anu aya dina jero gunung contohna asap atanapi gas. Sareng deuih gempa vulkanik henteu sasering dibandingkeun sareng tektonik.
Gempa bumi pan biasana timbul di daerah anu caket sareng gunung berapi atanapi di sakitar caket lautan. Ngantisipasi gempa tiasa oge merhatoskeun disabudeureunana teras upami tos aya tanda2 diharepkeun ngajauhan tong sina caket. Kumargi saurna jalmi2 anu netep di sakitar wilayah eta kedah tiasa oge merhatoskeun lingkunganana.Contohna biasana gejala2/tanda2 anu bakal timbul ayana gempa nyaeta salah sawiosna tumbuhan disakitar gunung layu, suhu sakitar kawah naik, sumber cai disakitar gunung janten kering, sering aya gempa2 alit, teras sok aya migrasi atanapi sato2 anu pararindah. Salangkungna panginten nya ku alat teknologi, Richter atanapi seismograf tea.
Mangga sakitu heula, bilih aya anu nambihan atanapi anu ngalereskeun. Kanu ahlina panginten langkung terang.
Neng Iva
Kang Maman <[EMAIL PROTECTED]> wrote:
Kang Maman <[EMAIL PROTECTED]> wrote:
Hatur nuhun, neng iva mojank akank...
Naha kumaha ngabentenkeunnana... pan teu katingal
gerak sareng geserna nu di jero taneuh, moal kitu
pahili mana anu tektonik mana nu pulkanik?.
palangsiang tektonik tektonik...ari kanyataanana
geuning vulkanik, nyaeta lava nu ngageleser di joro
taneuh !.
Ujug-ujug jleghur weh...
kamana lumpat...kamana lumpat ...
:)
--- iva wanti <[EMAIL PROTECTED]> wrote:
>
> Upami henteu lepat bentena tektonik sareng vulkanik
> nyaeta ari tektonik mah gempa anu disebabkeun ku
> lapisan kerak bumi anu keras jadi genting (lunak)
> anu ahirna janten gerak. Lapisan eta bergerak sacara
> lalaunan sampai kapecah-pecah anu ahirna silih
> tabrakan.
> Upami gempa vulkanik nyaeta gempa anu disebabkeun ku
> ayana letusan gunung berapi anu langkung dahsyat.
> Waktu gunung berapi meletus eta getaran sareng
> goncanganna tiasa karaos dugika 20 mil.
> Upami henteu lepat saurna anu kamari gempa di pulau
> jawa teh kalebet gempa vulkanik da sababna aya
> kaitanana sareng aktifitas gunung sareng kajadianana
> di sakitar wilayah gunung.
>
>
>
> Neng Iva
>
> Kang Maman <[EMAIL PROTECTED]> wrote:
> Haturan baraya...
>
> Sok emut kapungkur sateuacana gunung galunggun bitu,
> aya lini di bandung; kasauran ti lembaga anu
> berwenang
> nyebatkeun yen sumber lini teh ayana di lautan.
>
> Dina usum kemarau (katiga ?), beu... eta gunung
> ujug-ujug ngabeledug, kacipta eta debu dugi kabawa
> angin kamana-mana duga nyampai ka rorompok sim
> kuring
> di buahbatu. Anu matak "kesel" naha hujan teu
> turun-turun; atuh kebul kamana mendi; masker baham
> janten pajeng pisan.
>
> Moal kitu dina usum katiga gunung-gunung bakal
> bararitu ?
> bentenna vulkanik sareng tektonik naon ?
>
> :)
>
>
>
>
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