- 33.4.1: How do nematode and annelid body plans differ?
- 33.4.2: Describe two adaptations that have enabled insects to thrive on land.
- 33.4.3: MAKE CONNECTIONS Historically, annelids and arthropods were viewed ...
Solutions for Chapter 33.4: Ecdysozoans are the most species-rich animal group
Full solutions for Campbell Biology | 10th Edition
Adiabatic temperature change
Cooling or warming of air caused when air is allowed to expand or is compressed, not because heat is added or subtracted.
The place in the orbit of a planet where the planet is farthest from the Sun.
An imaginary hollow sphere upon which the ancients believed the stars were hung and carried around Earth.
A volcano composed of both lava flows and pyroclastic material.
The transfer of heat through matter by molecular activity. Energy is transferred through collisions from one molecule to another.
The gently sloping surface at the base of the continental slope.
A type of volcanism that results from the eruption of magmas derived from the partial melting of ice.
The formation and growth of a crystalline solid from a liquid or gas.
An imaginary line that separates the drainage of two streams; often found along a ridge.
An organism whose genetic material is enclosed in a nucleus; plants, animals, and fungi are eukaryotes.
The flat, low-lying portion of a stream valley subject to periodic inundation.
A fountain of hot water ejected periodically.
The fine structure visible on the solar surface caused by convective cells below.
A general term referring to water vapor in the air but not to liquid droplets of fog, cloud, or rain.
The movement of surface water into rock or soil through cracks and pore spaces.
An isolated mountain remnant characteristic of the late stage of erosion in an arid region.
A chemical bond present in all metals that may be characterized as an extreme type of electron sharing in which the electrons move freely from atom to atom.
A theory that is held with a very high degree of confidence and is comprehensive in scope.
A system of streams running in all directions away from a central elevated structure, such as a volcano.
The downward slipping of a mass of rock or unconsolidated material moving as a unit along a curved surface.