WorksheetsGeology Chapter 3
Total questions: 27
Worksheet time: 27mins
understanding the various techniques of stratigraphic correlation
Heliocentric
Geocentric
Geologic Time-
Geochronology
older v. younger- sequential order- The technique of establishing a
chronology of events arranged in relative sequential order.
Events not a specific time only before or after other events
Chemo stratigraphy
Relative age dating-
Lithostratigraphy
Numerical (absolute) age dating-
how much time has passed- ( how long ago it happened) specific ages-the technique of establishing when events occurred according to how much time has elapsed since their occurrence.
Numerical (absolute) age dating
Formation
Relative age dating
Correlation
What age dating is Nicholas Steno’s principles of superposition, original horizontality, and lateral continuity Charles Lyell’s principles of cross-cutting relationships and included fragments William Smith’s principle of biotic succession.
Numerical (absolute) age dating
Relative age dating
Heliocentric
What age dating has these ways to tell -tree rings and coral growth lines counting layers of ice drilled from glaciers, counting sediment layers in ancient lakes, radiometric age dating
how old the earth is
How old the universe is
Geologic time scale
Numerical age
the first astronomical model – the Earth is the fixed center of the universe and everything revolves around it- Ptolemy is the person
Geocentric
Stratigraphy
Heliocentric
Biostratigraphy
Sun is the fixed center of the universe and the earth and other planets revolve around it – Galileo worked on this
Geocentric
Geochronology
Heliocentric
Isotopic excursion
chronology or calendar of the Earth’s history
Heterotrophs
Correlation
Geologic time scale –
Stratigraphy
the study of layers in sediments and sedimentary rocks
Correlation
Sequence stratigraphy-
Biostratigraphy
Stratigraphy
— matching layers from one area to another area
Correlation
Isotopic excursion
Geochronology
Lithostratigraphy
Fossils
Lithostratigraphy
Biostratigraphy
Sequence stratigraphy
Chemo stratigraphy-
chemical isotopes- ratios of chemical isotopes
Lithostratigraphy
Biostratigraphy
Sequence stratigraphy-
Chemo stratigraphy
rock type and composition
Lithostratigraphy-
Biostratigraphy
Sequence stratigraphy
Chemo stratigraphy-
changes in sea level
Lithostratigraphy
Biostratigraphy
Sequence stratigraphy
Chemo stratigraphy-
A Change in the number of isotopes-positive or negative shift in the isotopic ratio of an element recorded through a succession of strati-graphic layers.
Formation
isotopic excursion
Stratigraphy
Heliocentric
it has a distinct top and bottom, and is mappable across geographic space.
Heliocentric
Isotopic excursion
Geocentric
Formation
The amount of time it takes for a quantity of a substance to reduce half it's inital value-radioactive parent isotope to transform, or decay, to a daughter product.
Geochronology
Formation
Half life-
Correlation
in a radioactive decay series. An unstable isotope that decays, or transforms, into a daughter product (isotope)
Geologic Time
Parent isotope-
Half life
Geochronology
A stable isotope formed from the radioactive decay of a parent isotope
Daughter
half life
geocentric
heliocentrid
refers to numerical age
Numerical (absolute) age dating-
Geologic time scale
Relative age dating
Geochronology
How old is the Earth based on Young Earth Theory- Bible theories of Lightfoot and Ussher
10 thousand years
6 thousand years
4.5 Billion years
13.77 billion Years
How old is earth based on Old earth theory- from geology
10 thousand years
6 thousand years
13.77 billion years
4.5Billion years
How old is the universe?
6 thousand years
10 thousand years
4.5 billion years
13.77 billion years
What are the 2 types of Age Dating
carbon dating and geocentric age dating
numerical age dating an gecetric age dating
Relative Age Dating and Numerical Age Dating
geocentric age dating and relative age dating
Sequence of normal and reverse polarity episodes
formation
Magnetic Polarity
isotopic excursion
chemo stratigraphy
Isotopes- radiometric Age Dating
hparent, son, daughter
half life, parent, son
Half life, parent, Daughter
half life, son, daughter
3 types of Isotope decay
Electron, proton, beta
Electron Alpha, Beta
electron, proton, alpha
proton, alpha, beta
