A plant

Mr.Williamson

A dead animal

the remains or impression of a prehistoric organism preserved in petrified form or as a mold or cast in rock.

Something you eat off of

the ocean

a moving thing

a theory in geology: the lithosphere of the earth is divided into a small number of plates which float on and travel independently over the mantle and much of the earth's seismic activity occurs at the boundaries of these plates.

rock

the ground

a person who studies bones

relating to the study of the earth's physical structure and substance.

toast

the outside of something

the middle of something

A diagram that shows what the inside of something looks like

A core sample is a cylindrical section of a naturally occurring substance

A piece of the grass

an apple core

I DONT EVEN KNOW MAN

large-scale processes affecting the structure of the earth's crust

large-scale processes affecting the strcture of the earth's crust.

large-scale processes affecting te structure of the earth's crust.

large-scale rocesses affecting the structure of the earth's crust.

an extinct small aquatic reptile of the early Permian period, with an elongated body, flattened tail, and a long narrow snout with numerous needlelike teeth.

an extinct small aquatic reptile of the early Permian period, with an elongated body, flattened til, and a long narrow snout with numerous needlelike teeth.

an extinct small aquatic reptile of the early Permian period, with an elongated body, flatteed tail, and a long narrow snout with numerous needlelike teeth.

an extinct small aquatic reptile of the early Permian period, with an elongated body, flttened tail, and a long narrow snout with numerous needlelike teet

In plate tectonics, a convergent boundary, also known as a destructive plate boundary, is a region of active deformation where two or more tectonic plates or fragments of the lithosphere are near the end of their life cycle.

In plat tectonics, a convergent boundary, also known as a destructive plate boundary, is a region of active deformation where two or more tectonic plates or fragments of the lithosphere are near the end of their life cycle.

In plate tectoics, a convergent boundary, also known as a destructive plate boundary, is a region of active deformation where two or more tectonic plates or fragments of the lithosphere are near the end of their life cycle.

In plate tectonics, a cnvergent boundary, also known as a destructive plate boundary, is a region of active deformation where two or more tectonic plates or fragments of the lithosphere are near the end of their life cycle.

In plate tectonics, a divergent boundary or divergentplate boundary (also known as a constructiveboundary or an extensional boundary) is a linear feature that exists between two tectonic plates that are moving away from each other.

In plate tectonics, a divergent boundary or divergentplate boundary (also known as a constructiveboundary o an extensional boundary) is a linear feature that exists between two tectonic plates that are moving away from each other.

In plate tectonics, a divergent boundary or divergentplate boundary (also known as a constructiveboundary or an extensional boundary) is a linear feature that exists between two tectonc plates that are moving away from each other.

In plate tectonics, a divergent boundary or divergentplate boundary (also known as a constructiveboundary or n extensional boundary) is a linear feature that exists between two tectonic plates that are moving away from each other.

Transform fault, in geology and oceanography, a type of fault in which two tectonic plates slide past one another. ... Morgan proposed that opposing plates along an oceanic ridge crest offset by fracture zones are divided by the spreading centres and transformfaults.

Transform fault, in geology and oceanography, a type of fault in which two tectonic plates slide past one another. ... Morgan proposed that opposing plates along an oceanic ridge crest offset by fracture zoes are divided by the spreading centres and transformfaults.

Transform fault, in geology and oceanography, a type of fault in which two tectonic plates sle past one another. ... Morgan proposed that opposing plates along an oceanic ridge crest offset by fracture zones are divided by the spreading centres and transformfaults.

Transform fault, in geology and owdanography, a type of fault in which two tectonic plates slide past one another. ... Morgan proposed that opposing plates along an oceanic ridge crest offset by fracture zones are divided by the spreading centres and transformfaults.

the geological processes, such as tectonic plate movement and volcanic activity, by which mountains are formed.

the geological processes, such as tectonic plate movement and volcanic activity by which mountains are formed.

the geological processes, such as tectonic plate movement and volcanic activity, by which are formed.

the geological processes, such as tectonic plate movement and volcanic activity, by which mounains are formed.

the sideways and downward movement of the edge of a plate of the earth's crust into the mantle beneath another plate.

the sideways and downward move ent of the edge of a plate of the earth's crust into the mantle beneath another plate.

the sideways and downward movement of the edge of a plate of the earth's crust into the mantle eneath another plate.

the sideways and downward movement of the edge of a plate of the earth's crust into he mantle beneath another plate.

volcanic activity or phenomena.

volcanic activity or phenomena

volcanic activity or phenomena

volcanic activity or phenomena

a long, seismically active submarine ridge system situated in the middle of an ocean basin and marking the site of the upwelling of magma associated with seafloor spreading. An example is the Mid-Atlantic Ridge

a long seismically active submarine ridge system situated in the middle of an ocean basin and marking the site of the uwelling of magma associated with seafloor spreading. An example is the Mid-Atlantic Ridge

a long, seismically active submarine ridge system situated in the middle of an ocean basin and markin the site of the upwelling of magma associated with seafloor spreading. An example is the Mid-Atlantic Ridge

a long, seismically active submarine ridge system situated in the middle of an ocean basin and marking the site of the upwelling of magma associated with seaflor spreading. An example is the Mid-Atlantic Ridge

a line that marks the limits of an area; a dividing line.

a line that marks the limits of an area a dviding line.

a line that marks the limits of an area dividing line.

a line that marks the limits of an area, dividing line.

a theory in geology: the lithosphere of the earth is divided into a small number of plates which float on and travel independently over the mantle and much of the earth's seismic activity occurs at the boundaries of these plates.

a theory in geology: the lithosphere of the earth is divided into a small number of plates which float on and travel independently over the mantle and much of the earth'seismic activity occurs at the boundaries of these plates.

a theory in geology: the lithosphere of the earth is divided into a small number of plates which float on and travel independently over the mantle and much of the earth s seismic activity occurs at the boundaries of these plates.

a theory in geology: the lithosphere of the earth is divided into a small number of plates which float hiand travel independently over the mantle and much of the earth's seismic activity occurs at the boundaries of these plates.

An oceanic plate is a tectonic plate at the bottom of the oceans. The Earth's rocky outer layer turned into solid billions of years ago, soon after the Earth formed. ... The Earth's crust lies on top of the plates - the continental crust - the relatively thick part of the earth's crust which forms the large land masses.

An oceanic plate is a tectonic plate at the bottom of the oceans. The Earth's rocky outer layer turned into solid billions of years ago, soon after the Earth forme The Earth's crust lies on top of the plates - the continental crust - the relatively thick part of the earth's crust which forms the large land masses.

An oceanic plate is a tectonic plate at the bottom of the oceans. The Earth's rocky outer layer turned into solid billions of years ago, soon after the Earth formed. ... The Earth's crust lies on top of the plates - the continental cust - the relatively thick part of the earth's crust which forms the large land masses.

An oceani plate is a tectonic plate at the bottom of the oceans. The Earth's rocky outer layer turned into solid billions of years ago, soon after the Earth formed. ... The Earth's crust lies on top of the plates - the continental crust - the relatively thick part of the earth's crust which forms the large land masses.