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Atomic Structure
An atom consists of three main subatomic particles:
Density Formula
Density is the amount of mass in a given volume, calculated as:
Density = \frac{mass}{volume}
Newton's First Law of Motion
Also known as the Law of Inertia, it states that an object at rest stays at rest, and an object in motion stays in motion unless acted upon by an unbalanced force.
Newton's Second Law of Motion
The acceleration of an object depends on the mass of the object and the amount of force applied:
F = m \times a
Cell Theory
Photosynthesis Equation
The process by which plants convert light energy into chemical energy:
6CO{2} + 6H{2}O + light \rightarrow C{6}H{12}O{6} + 6O{2}
Law of Conservation of Mass
Mass is neither created nor destroyed in a chemical reaction; the mass of the reactants must equal the mass of the products.
Plate Tectonics
The theory that Earth's outer shell is divided into several plates that glide over the mantle, causing earthquakes, volcanoes, and continental drift.
Potential vs. Kinetic Energy
Genotype vs. Phenotype
Atomic Structure
An atom consists of three main subatomic particles:
Density Formula
Density is the amount of mass in a given volume, calculated as:
Density = \frac{mass}{volume}
Newton's First Law of Motion
Also known as the Law of Inertia, it states that an object at rest stays at rest, and an object in motion stays in motion unless acted upon by an unbalanced force.
Newton's Second Law of Motion
The acceleration of an object depends on the mass of the object and the amount of force applied:
F = m \times a
Cell Theory
Photosynthesis Equation
The process by which plants convert light energy into chemical energy:
6CO{2} + 6H{2}O + light \rightarrow C{6}H{12}O{6} + 6O{2}
Law of Conservation of Mass
Mass is neither created nor destroyed in a chemical reaction; the mass of the reactants must equal the mass of the products.
Plate Tectonics
The theory that Earth's outer shell is divided into several plates that glide over the mantle, causing earthquakes, volcanoes, and continental drift.
Potential vs. Kinetic Energy
Genotype vs. Phenotype
Newton's Third Law of Motion
For every action, there is an equal and opposite reaction.
Physical vs. Chemical Changes
Layers of the Earth
Speed Formula
The rate at which an object covers distance:
Speed = \frac{distance}{time}
The Rock Cycle
The continuous process by which one type of rock changes into another (igneous, sedimentary, and metamorphic) through geological processes like melting, cooling, weathering, and pressure.