Based on the information presented in the lecture, students should be able to rank the images of island and volcanic processes from youngest to oldest.Their performance in this task is the assessable product.Additionally, if you would like all of the resources together in a PDF document, that can be accessed as a complete resource here: Dating & Rock Layering [Entire Lesson][PDF].Finally, students may need their Earth Science Reference Tables [ESRT] for parts of the lesson (a document used widely in the New York State Earth Science Regents course) as well.] This is the first, and one of the most important, lessons in the new unit.Some types of relative dating techniques include climate chronology, dendrochronology, ice core sampling, stratigraphy, and seriation.
[Note: For embedded comments, checks for understanding (CFUs), and key additional information on transitions and key parts of the lesson not necessarily included in the below narrative, please go to the comments in the following document: Dating & Rock Layering (Whole Lesson w/comments).
For example, the presence of recycled bricks at an archaeological site indicates the...
ANSWER: Relative dating is used to determine the relative ages of geologic strata, artifacts, historical events, etc.
However, relative methods are , which is that if there are layers of deposits, those laid down first will be on the bottom and those laid down last will be on the top. However, geological strata are not always found to be in a neat chronological order.
Wind and water erode strata and some areas are uplifted or even tilted.