About: Mercury/Mantle   Sponge Permalink

An Entity of Type : owl:Thing, within Data Space : 134.155.108.49:8890 associated with source dataset(s)

Mantle about 500-700 km thick consisting of Silicates surrounding Mercury's core and beneath its crust. It is thought to not rise and fall in convective patterns like Earth and other larger planets, and so may not have cooled as quickly, enabling volcanism to persist over halfway through its lifespan.

AttributesValues
rdfs:label
  • Mercury/Mantle
rdfs:comment
  • Mantle about 500-700 km thick consisting of Silicates surrounding Mercury's core and beneath its crust. It is thought to not rise and fall in convective patterns like Earth and other larger planets, and so may not have cooled as quickly, enabling volcanism to persist over halfway through its lifespan.
dbkwik:scratch-pad...iPageUsesTemplate
dbkwik:scratchpad/...iPageUsesTemplate
abstract
  • Mantle about 500-700 km thick consisting of Silicates surrounding Mercury's core and beneath its crust. It is thought to not rise and fall in convective patterns like Earth and other larger planets, and so may not have cooled as quickly, enabling volcanism to persist over halfway through its lifespan.
Alternative Linked Data Views: ODE     Raw Data in: CXML | CSV | RDF ( N-Triples N3/Turtle JSON XML ) | OData ( Atom JSON ) | Microdata ( JSON HTML) | JSON-LD    About   
This material is Open Knowledge   W3C Semantic Web Technology [RDF Data] Valid XHTML + RDFa
OpenLink Virtuoso version 07.20.3217, on Linux (x86_64-pc-linux-gnu), Standard Edition
Data on this page belongs to its respective rights holders.
Virtuoso Faceted Browser Copyright © 2009-2012 OpenLink Software