Biodiversity (5)
The variety of life in an area (plants, animals, microbes).
Human actions like pollution, deforestation, and climate change reduce biodiversity.
Food Production (5)
Our ability to grow and harvest food.
Affected by things like soil health, climate, and water access.
Average Global Temperature (5)
Earth’s temperature is rising due to greenhouse gases from burning fossil fuels (like CO₂).
Causes melting ice, sea level rise, and extreme weather.
Human Population (5)
The number of people on Earth keeps growing.
More people = more resource use and more pollution.
Resource Depletion (5)
Using up natural resources faster than they can be replaced (e.g., water, soil, fossil fuels, forests).
Law of Superposition:
In layers of rock/soil, the oldest layers are at the bottom and newer ones are at the top (used for relative dating).
Radioactive Dating:
A method of determining the exact age of an object by measuring radioactive isotopes (used for absolute dating).
Half-Life:
The time it takes for half of a radioactive isotope to decay.
Decay:
When a radioactive atom breaks down over time into a different, more stable element.
Isotope:
Versions of an element that have the same number of protons, but different neutrons.
Proton:
A positively charged particle in the nucleus of an atom.
Neutron:
A neutral particle in the nucleus (no charge).
Electron:
A negatively charged particle that orbits the nucleus.
Radioactive:
An unstable isotope that releases energy/particles (decays).
Nucleus:
The center of the atom where protons and neutrons are located.
Law of Superposition:
deeper = older.
Isotopes of the same element have:
Same number of protons
Different number of neutrons
This changes their mass and sometimes makes them radioactive.
Using the periodic table to find protons and neutrons
Atomic number = # of protons
Mass number (rounded) − atomic number = # of neutrons
The main isotopes of carbon
Carbon-12 (most common, stable)
Carbon-13 (stable, rare)
Carbon-14 (radioactive, used in dating things that were once alive)
How radioactive carbon forms and decays
Carbon-14 forms in the atmosphere → plants absorb it → animals eat plants.
After death, Carbon-14 decays over time → scientists measure how much is left to determine age.
How radiocarbon dating works
Living things have a constant amount of Carbon-14
After death, no new Carbon-14 is taken in
Scientists measure how much Carbon-14 remains and use its half-life (5,730 years) to calculate age.
Using a graph of radioactive decay
The graph shows how much of the isotope is left over time.
You can calculate the age of a sample by matching how much isotope is left to how many half-lives have passed.
How Easter Island’s environment and population changed
Originally had forests and a stable population.
Overused resources (cut trees, overfarmed), which caused:
Soil erosion
Loss of food
Collapse of civilization
Explain how Easter Islanders lived
Built huge stone statues (Moai), farmed, fished, and had a complex society.
Likely had strong spiritual beliefs tied to the statues.