This HTML5 document contains 59 embedded RDF statements represented using HTML+Microdata notation.

The embedded RDF content will be recognized by any processor of HTML5 Microdata.

PrefixNamespace IRI
n38http://dbkwik.webdatacommons.org/resource/J5-aVCD79FNUsLY8S3DjeQ==
n15http://dbkwik.webdatacommons.org/resource/ov7UKRnkZWbKXGlddstZzQ==
n42http://dbkwik.webdatacommons.org/resource/R7qU8SMZULyjmkvidmZ1yg==
n16http://dbkwik.webdatacommons.org/resource/B_FjH-VLyjNx9RPbEhSUgg==
n48http://dbkwik.webdatacommons.org/resource/m5268hoCy0FopVdhvAYd7w==
n18http://dbkwik.webdatacommons.org/resource/HJzPLWyKTechISKYVIh_ZA==
n2http://dbkwik.webdatacommons.org/resource/qXX_bnHOZ2RAwy7_8MgOrg==
n20http://dbkwik.webdatacommons.org/resource/7QQcqg3Hg4hLsOzWWO_Xjg==
dbrhttp://dbpedia.org/resource/
n35http://dbkwik.webdatacommons.org/resource/2acBgv9hkUj7heA0YhbHdA==
n54http://dbkwik.webdatacommons.org/resource/eTU4Xy1rek9hOR678WurhA==
n55http://dbkwik.webdatacommons.org/resource/RiaMY-W7ua567zJeXjY1LA==
n4http://dbkwik.webdatacommons.org/resource/uvpcfT5twfAIP0WSgVeODg==
n31http://dbkwik.webdatacommons.org/resource/qS_zVwQXFa9YsRmyHyezhA==
n62http://dbkwik.webdatacommons.org/resource/_pHy4oewCgdneP8Pd0hgeQ==
n27http://dbkwik.webdatacommons.org/resource/yTb5WbS7dBCN1CYbxmA27w==
dctermshttp://purl.org/dc/terms/
n30http://dbkwik.webdatacommons.org/resource/Qw1V5ppuvWt6-AdL0n12-Q==
n9http://dbkwik.webdatacommons.org/resource/PR16ZSZL47RfBrMJnCPw6Q==
rdfshttp://www.w3.org/2000/01/rdf-schema#
n36http://dbkwik.webdatacommons.org/geology/property/
rdfhttp://www.w3.org/1999/02/22-rdf-syntax-ns#
n57http://dbkwik.webdatacommons.org/resource/mN1SPtSK6DqXcZx381QGPQ==
n24http://dbkwik.webdatacommons.org/resource/CxVKfr_uKBHotfvF571miw==
n5http://dbkwik.webdatacommons.org/resource/7l2jiPBKM7FSLkH3AhLZiw==
n3http://dbkwik.webdatacommons.org/resource/kGLB5oAXCnudmK16Q3kgnA==
n41http://dbkwik.webdatacommons.org/resource/ye2csl6OrlP9Jv1gSBDBvw==
n59http://dbkwik.webdatacommons.org/resource/SCO-PvFACrSZEUu1vXtb9w==
xsdhhttp://www.w3.org/2001/XMLSchema#
n45http://dbkwik.webdatacommons.org/resource/UCOSFpu38MzM65kylQCJLQ==
n46http://dbkwik.webdatacommons.org/resource/t_PO8SEQhpu5C43j_wJ8Ow==
n32http://dbkwik.webdatacommons.org/resource/AikZagFu0XuAr6tTphXaeg==
n22http://dbkwik.webdatacommons.org/resource/o0QGxuwHGIzmTuMiX5jhSA==
n52http://dbkwik.webdatacommons.org/resource/OdZnbUFuZqFi6hJHeMKmiw==
n7http://dbkwik.webdatacommons.org/resource/g7aBJoUn1dtvJLr0ipYsgA==
n58http://dbkwik.webdatacommons.org/resource/Ugq9y4OzuvJW3qa0sXdAjg==
n19http://dbkwik.webdatacommons.org/resource/Z3AsUmmuUdVU6xja1FC2zA==
n60http://dbkwik.webdatacommons.org/eq2/property/
n29http://dbkwik.webdatacommons.org/ja.eq2/property/
n51http://dbkwik.webdatacommons.org/resource/1gzr2Qu5Mo2gAvRfNOP4SQ==
n40http://dbkwik.webdatacommons.org/resource/rcW8RJQMm4AFuHfV_LXqcA==
n47http://dbkwik.webdatacommons.org/resource/_Zpr0NJbPFuMcGO3_iLzxg==
n14http://dbkwik.webdatacommons.org/finalfantasy/property/
n21http://dbkwik.webdatacommons.org/final-fantasy/property/
n50http://dbkwik.webdatacommons.org/resource/vZse_IigyJgkSmuIhBTNwg==
n49http://dbkwik.webdatacommons.org/resource/bH7J6fZVC9ddIDf-QvtirQ==
n39http://dbkwik.webdatacommons.org/resource/_6MG8QrAr5QWoD_fM2eGbw==
n37http://dbkwik.webdatacommons.org/resource/XT6LQEmK8k32kN-BS-1rAA==
n6http://dbkwik.webdatacommons.org/halo/property/
n25http://dbkwik.webdatacommons.org/resource/bX9Sb6V8_vJvZdB80A-lDw==
n28http://dbkwik.webdatacommons.org/resource/q55-wklRaQDyQq0ldXMXlw==
n26http://dbkwik.webdatacommons.org/ontology/
n43http://dbkwik.webdatacommons.org/resource/OKMIXeFNj1OOwECmZZu0ag==
n53http://dbkwik.webdatacommons.org/resource/1w9PK0RDjZhVDEpNfzFxSA==
n10http://dbkwik.webdatacommons.org/resource/5KL52omCwczaQOGlAZ6i2w==
n44http://dbkwik.webdatacommons.org/resource/LUf46SzJumcvGk0eDDv9ig==
n34http://dbkwik.webdatacommons.org/resource/yx2QN92pkGHjx_HDHs38CQ==
n11http://dbkwik.webdatacommons.org/resource/XJ6XkZDjJ7QifEra07eAsQ==
n23http://dbkwik.webdatacommons.org/volcanoes/property/
n33http://dbkwik.webdatacommons.org/resource/Ijyilhce4egGntreF_8dUQ==
n56http://dbkwik.webdatacommons.org/resource/Ue7i4hkEjreGPzOrgN7aBA==
n61http://dbkwik.webdatacommons.org/resource/se9wCJ8F6iQerysbA3ucCg==
owlhttp://www.w3.org/2002/07/owl#
Subject Item
n2:
rdf:type
n57:
rdfs:label
Pumice Pumice
rdfs:comment
|} It is commonly, but not exclusively composed of silicic or felsic materials or otherwise intermediate in composition (e.g. rhyolitic, dacitic, andesite, pantellerite, phonolite, trachyte), but occurrences of basaltic and other compositions are known. Pumice is commonly pale in color, ranging from white, cream or gray, but can be green brown or black. It forms when gases exsolving from viscous magma nucleate bubbles which cannot readily decouple from the viscous magma prior to chilling to glass. Pumice is a common product of explosive eruptions (plinian and ignimbrite-forming) and commonly forms zones in upper parts of silicic lavas. Pumice has an average porosity of 90%, and initially floats on water. Pumice is a textural term for a volcanic rock that is a solidified frothy lava composed of highly microvesicular glass pyroclastic with very thin, translucent bubble walls of extrusive igneous rock. It is commonly, but not exclusively of silicic or felsic to intermediate in composition (e.g. rhyolitic, dacitic, andesite, pantellerite, phonolite, trachyte), but occurrences of basaltic and other compositions are known. Pumice is commonly pale in color, ranging from white, cream, blue or grey, but can be green brown or black. It forms when gases exsolving from viscous magma nucleate bubbles which cannot readily decouple from the viscous magma prior to chilling to glass. Pumice is a common product of explosive eruptions (plinian and ignimbrite-forming) and commonly forms zones in upper parts o |} Pumice is an igneous rock. It is the only known rock that can float on water, due to large airpockets in its core. It is mainly used as a grinding stone, to polish jewelery or sharp objects such as knives. Pumice is also used in making cinder blocks.
owl:sameAs
dbr:Pumice
n47:
51
dcterms:subject
n18: n20: n32: n59:
n53:
n54:
n10:
n11:
n5:
ランブラー
n44:
Pumice..jpg
n43:
51
n52:
Crushing
n9:
-490
n56:
Yes
n39:
魔法生物
n62:
Slashing Blades
n3:
ネームド
n28:
▲ ヒロイック
n31:
ラヴァストーム
n46:
Pumice
n41:
51
n34:
^
n60:wikiPageUsesTemplate
n61:
n21:wikiPageUsesTemplate
n22: n45:
n14:wikiPageUsesTemplate
n15: n19:
n6:wikiPageUsesTemplate
n7: n33: n35: n51:
n29:wikiPageUsesTemplate
n30:
n48:
Pumice
n55:
Igneous
n36:wikiPageUsesTemplate
n37:
n23:wikiPageUsesTemplate
n24:
n58:
Heroic
n50:
Rock
n16:
No
n25:
Pew-Miss or Puhm-Iss
n38:
Lavastorm
n42:
Rumbler
n40:
32074
n27:
Roams The Wounds
n4:
はい
n49:
Lava
n26:abstract
|} It is commonly, but not exclusively composed of silicic or felsic materials or otherwise intermediate in composition (e.g. rhyolitic, dacitic, andesite, pantellerite, phonolite, trachyte), but occurrences of basaltic and other compositions are known. Pumice is commonly pale in color, ranging from white, cream or gray, but can be green brown or black. It forms when gases exsolving from viscous magma nucleate bubbles which cannot readily decouple from the viscous magma prior to chilling to glass. Pumice is a common product of explosive eruptions (plinian and ignimbrite-forming) and commonly forms zones in upper parts of silicic lavas. Pumice has an average porosity of 90%, and initially floats on water. Much of the surface of the UEG colony world Tribute was blanketed in frost-covered pumice. Pumice is a textural term for a volcanic rock that is a solidified frothy lava composed of highly microvesicular glass pyroclastic with very thin, translucent bubble walls of extrusive igneous rock. It is commonly, but not exclusively of silicic or felsic to intermediate in composition (e.g. rhyolitic, dacitic, andesite, pantellerite, phonolite, trachyte), but occurrences of basaltic and other compositions are known. Pumice is commonly pale in color, ranging from white, cream, blue or grey, but can be green brown or black. It forms when gases exsolving from viscous magma nucleate bubbles which cannot readily decouple from the viscous magma prior to chilling to glass. Pumice is a common product of explosive eruptions (plinian and ignimbrite-forming) and commonly forms zones in upper parts of silicic lavas. Pumice has an average porosity of 90%, and initially floats on water. This article is a . You can help My English Wiki by expanding it. |} Pumice is an igneous rock. It is the only known rock that can float on water, due to large airpockets in its core. It is mainly used as a grinding stone, to polish jewelery or sharp objects such as knives. Pumice is also used in making cinder blocks.