19) In terms of dating of specific rocks, structures, or landscapes, relative age refers to
A) the age of geological features based on isotopic dating techniques.
B) the approximate age of geological features based on the period or epoch in which they
occurred. For instance, noting a feature is from the Cretaceous.
C) the inability to ascertain exact age through isotopic methods and the necessity to provide a
date range for such features.
D) the age of one feature with respect to another within a sequence of events and deduced from
the positions of rock strata above and below one another.
20) In terms of dating of specific rocks, structures, or landscapes, numerical age refers to
A) the age of geological features based on isotopic dating techniques.
B) the approximate age of geological features based on the period or epoch in which they
occurred. For instance, noting a feature is from the Cretaceous.
C) a range of numeric values in which a features was likely formed and based on several lines of
evidence, such as paleoclimatic and paleobotanical reconstructions.
D) the age of one feature with respect to another within a sequence of events and deduced from
the positions of rock strata above and below one another.
21) Scientists have direct evidence of the Earth’s structure to
A) the inner core.
B) the upper mantle (~250 km (155 mi)).
C) about 2 km (1.2 mi) from the surface.
D) 10 km (6 mi) from the surface, based on the deepest well shaft.