definisi
marl iku sawijining rock sedimentary unconsolidated dumadi saka lempung lan jeruk
tuff jinis rock digawe saka awu vulkanik luwar saka ngeculake sajrone eruption vulkanik
panemu
William Smith
Ora dingerteni
Etimologi
saka lawas marle french, saka pungkasan marglia latin
saka tembung latin tophous banjur ing tufo italian lan pungkasanipun tuff
kelas
rocks sedimentary
batuan beku
sub-kelas
awet rock, rock alus
awet rock, medium atose rock
kategori liyane
rock grained nggoleki, rock opaque
rock grained nggoleki, rock opaque
tektur
earthy
clastic, pyroclastic
werna
ibas, coklat, ijo, grey, putih
coklat, grey, kuning
katon
atos lan kurang
kurang, vesicular lan foilated
Efesus interior
aggregates hiasan, kothak lantai
aggregates hiasan, entryways, jogan, homes, interior
Efesus njaba
minangka watu bangunan, kothak gendheng
minangka watu bangunan, minangka madhep watu, Taman hiasan, bangunan kantor, mapeng watu
Efesus arsitektur liyane
curbing
curbing
industri construction
Pabrik semen, kanthi jumlah ongko construction, kanggo dalan kanthi jumlah ongko, nggawe semen alam, mentahan materi kanggo Pabrik mortir
omah bangunan utawa tembok, kanthi jumlah ongko construction
Efesus jaman
artefak, perhiasan, reca, figurines cilik
artefak, monumen, reca, figurines cilik
komersial
nggawe kriya, kondisioner lemah
nggawe kriya
jinis
lempung marl, marl biru, marl abang, dhuwur marl bank, Nihan lapisan marl, ing lapisan Nihan marl, marl wedhi, marl ijo, marl werna abu-abu lan marl clayey
gandheng tuff, tuff rhyolitic, basaltic tuff, trachyte tuff, tuff andesitic lan ignimbrite.
fitur
umume atos kanggo tutul, iku salah siji saka rock tuwa, splintery, rock grained banget nggoleki
tansah ditemokake minangka pipo vulkanik liwat lemah ndhuwur Continental jero
monumen misuwur
-
pulo Paskah ing segitiga Polinesia, pacific segara
tatanan
Wangun marl nalika partikel lempung banget nggoleki-grained sing setor ing banyu kang settles ing ngisor banyu badan lan compacted dening overlying endhepan; banyu meres metu lan Empu mbentuk rock marl.
tuff wis kawangun nalika massa gedhe saka awu lan wedhi kang lagi pipis karo gas panas sing luwar dening gunung mbledhos lan longsor kanthi cepet mudhun lereng sawijining.
isi Mineral
kalsit, lempung, dolomite, gypsum, micas, pyrite, quartz
kalsit, chlorite
senyawa isi
aluminium oxide, NaCl, cao, wesi (iii) oxide, silikon dioksida
hidrogen sulfida, belerang dioxide
jinis metamorphism
-
metamorphism kakubur, metamorphism cataclastic, kontak metamorphism, hidrotermal metamorphism, impact metamorphism, metamorphism regional
jinis udan
udan biologi, udan kimia
udan biologi, udan kimia, udan mechanical
jinis erosi
erosi kimia, erosi gisik, banyu erosi, angin erosi
erosi kimia, erosi gisik, erosi Glacier, erosi segara, banyu erosi, angin erosi
ukuran gandum
banget nggoleki-grained
grained nggoleki
rengat
conchoidal
ora rata
porosity
Highly keropos
Highly keropos
luster
kurang
vitreous kanggo kurang
tartamtu gravitasi
2.2-2.8
2.73
Kapadhetan
2.4-2.8 g / cm 3
1-1.8 g / cm 3
resistance
tahan panas, impact tahan
tahan panas, impact tahan, meksa tahan, nyandhang tahan
celengan ing bawana wétan
asia
India, Pakistan, Russia
Afghanistan, Armenia, Azerbaijan, Burma, Cambodia, China, India, Indonesia, Iran, Japan, Malaysia, Mongolia, Nepal, North Korea, Pakistan, Saudi Arabia, Syria, Taiwan, Thailand, Turkey, Vietnam, Yemen
africa
Ethiopia, Kenya, Morocco, South Africa
Cameroon, Cape Verde, Eritrea, Ethiopia, Kenya, Libya, Madagascar, Nigeria, Rwanda, South Africa, Sudan, Uganda
europe
austria, france, germany, greece, italy, romania, Scotland, spain, Swiss
france, georgia, germany, greece, iceland, italy, Aku tresna sampeyan;, Poland, portugal, spain, united kingdom
wong
-
Antartika, pulo hawaii
celengan ing bawana kulon
lor amerika
USA
Canada, Costa Rica, Panama, USA
kidul amerika
Colombia, Ecuador, Peru
Argentina, Bolivia, Brazil, Chile, Ecuador, Paraguay
celengan ing Oseania bawana
australia
New South Wales, Victoria, Western Australia
Central Australia, Western Australia