Unit 1 Exam Flashcards
Scientific Basics, Geologic Dating and Time Scale, Earths Structure, Plate Tectonics (45 cards)
Hypothesis
(Scientific basics)
possible explanations for our observations
theory
(Scientific basics)
well tested and widely accepted view that the scientific community generally agrees upon
scientific methods
(Scientific basics)
careful observation, construct hypothesis, test hypothesis
basic assumptions
(Scientific basics)
-the world is understandable
-scientific ideas are subject to change
-scientific knowledge is durable
-science cannot provide complete answers to all questions
original horizontally
(relative dating)
rock layers typically form a nearly horizontal position
superposition
(relative dating)
rock layers become younger from bottom to top
lateral continuity
(relative dating)
rock layers are assumed to have originally extended laterally in all direction unless they are observed to pinch out or terminate
cross cutting relationship
(relative dating)
any geologic feature that cuts across another the younger of the two layers(faults)
inclusion
(relative dating)
where fragments of one rock type is contained within rocks of another type, rock included is older
oldest to youngest
(relative dating)
EGLCHMDJANKBF
numeric dating
geologic clock, occurs at a constant rate, radioactive decay
radioactive decay
(numeric dating)
measuring the quantity of unstable atoms left in a rock and compare into the quantity of stable daughter atoms in the rock
phanerozoic
(geologic time scale)
-eon
-visible life
-hard bodied fossils
cenozoic
(geologic time scale)
-era
-recent life
-mammals
mesozoic
(geologic time scale)
-era
-middle life
-reptiles and dinosaurs
paleozoic
(geologic time scale)
-era
-ancient life
-intervertebral, fish, amphibians
Jurassic
(geologic time scale)
-period
-Mesozoic era
Cambrian
(geologic time scale)
-period
-Paleozoic era
how do we know what is inside the earth
(earths structure)
ultrasonography
-we measure earthquake waves, which have a low frequency but a lot of energy
inner core
(earths structure)
composed of iron
high density
high pressure
outer core
(earths structure)
high density
high pressure
liquid
mantle
(earths structure)
composed of iron rich silicate rocks
solid but able to flow over long timescales
astheosphere
(earths structure)
relatively weak and plastic zone
upper mantle
flows with time
lithosphere
(earths structure)
cool and rigid outer surface of the earth
uppermost mantle and crust