Chapter 13 - Geologic time Flashcards
principle of superposition
in sedimentary rocks the oldest layer is on the bottom and youngest layer is on the top
principle of original horizontality
sedimentary rocks originally formed parallel to the surface of earth
principle of original lateral continuity
faulting, severe folding, and erosion may separate originally continuous strata
principle of cross-cutting relationships
rocks that cut across other layers of rock are younger than the rock that they cut across
principle of inclusions
any existing rock that is incorporated into a sedimentary layer or igneous intrusion is older than the layer or intrusion which it is incorporated within
principle of unconformities
unconformities develop when erosion or non-deposition interrupts the continuity of the geologic record
principle of fossil succession
plants and animals change throughout time and the rock layers record the change
unconformity
when a sedimentary layer is on top of an eroded igneous layer
disconformity
when a sedimentary layer is on top of an eroded sedimentary layer
alpha decay
an atom emits an alpha particle consisting of 2 protons, 2 neutrons
beta decay
an atom emits a negative particle which changes a neutron into a proton
electron capture
an atom loses one proton and becomes lighter