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formation
mappable body of rock
contacts
distinct boundaries
outcrops
exposures of bedrock
angular unconformity
nonparallel graphs in rocks above and below the unconformity
nonconformities
separate non bedded, crystalline rocks from younger sedimentary rocks
plutons
bodies of intrusive igneous rock
dikes
thin, tabular intrusions that cut across bedding (discordant)
sills
the other tabular intrusions, are concordant
crater
small depression at the top
calderas
large depression at the top
lava (or pyroclastic) flows
gas charged flows that produce tuff
geologic cross sections
like topographic profiles, but with the subsurface geology shown schematically
line of section
the line along which the cross section will be made
Rule of V’s
where a contact line crosses a valley, it forms a V that points in the direction of the dip of the contact between the two formations