WorksheetsESB -U2Q1: Earth's Layers Pulse Check - 2025
Total questions: 30
Worksheet time: 23mins
The process by which a homogeneous (uniform) Earth separated into layers of differing density, with heavier materials sinking to the center, is known as:
Accretion
Differentiation
Volcanic Outgassing
Nebular Theory
The "Iron Catastrophe" describes the time when molten iron sank to form Earth's core. The primary cause of this event was:
The slow cooling of the Earth over billions of years.
The planet's temperature reaching iron's melting point due to bombardment, allowing liquid iron to sink by gravity.
Tidal forces from the early Moon pulling the liquid core into place.
The initial accretion of planetesimals containing only iron.
Which two sources are primarily responsible for the water that formed Earth's oceans?
Water vapor released by volcanic outgassing and bombardment by comets
Water captured from an icy ring system around the early Earth
Gravitational capture of atmospheric gases from space
Photosynthesis by early bacteria
The outermost mechanical layer of Earth, which is rigid and broken into large pieces called tectonic plates, is the:
Asthenosphere
Mesosphere
Lithosphere
Outer Core
The Asthenosphere is described as plastic because:
The rock within it flows slowly due to immense heat and pressure.
It is composed primarily of silicon, oxygen, and aluminum.
It is the boundary between the crust and the mantle.
It is a transitional zone where S-waves are absorbed.
Earth's average density is 5.54 g/cm³. Given that the crust has a density of 2.2-3.4 g/cm³, this information implies that:
The oceans must be denser than the crust.
The Mantle must have a lower density than the crust.
Material deep inside Earth (the core) must have a density much greater than 5.54 g/cm³
The Mesosphere is the layer that generates the magnetic field.
Earth's magnetosphere is created and sustained by the:
Extreme heat from the Inner Core.
Interactions and churning flow of liquid iron and nickel in the Outer Core (Dynamo Theory).
Convection currents in the Asthenosphere.
Gravitational pull of the Moon on the Inner Core.
How can we describe an oblate spheroid?
Equatorial Diameter is shorter than the Polar Diameter
Polar Diameter is shorter than the Equatorial Diameter
Polar and Equatorial Diameter are equal
