Anatomy Flashcards

1
Q

Linear elevation of enamel found at the mesial and distal borders of the occlusal surface of posterior teeth

A

Marginal Ridges

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2
Q

Ridges which descend from the tips of cusps of posterior teeth toward the central area of the occlusal surface

A

Triangular Ridges

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3
Q

The combination of 2 triangular ridges, which transversely cross the occlusal surface on a posterior tooth to merge with each other.

A

Transverse Ridge

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4
Q

The ridge that is found only on maxillary molars.

A

Oblique Ridge

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5
Q

It crosses the occlusal surface of maxillary molars in an oblique direction from the triangular ridge of distobuccal cusp to a ridge of mesiolingual cusp.

A

Oblique Ridge

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6
Q

Form the shape of a four-sided somewhat rounded pyramid.

A

Cusp Ridges

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7
Q

The mesial and distal cusp ridges are also known as

A

Cusp Slopes

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8
Q

Found on molars and premolars on the occlusal surfaces of mesial or distal to marginal ridges

A

Triangular Fossae

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9
Q

Major, sharply defined narrow, linear depressions formed during tooth development and usually separating the lobes or major portions of a tooth

A

Developmental Groove

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10
Q

This is less distinct, also a shallow linear depression on the surface of a tooth, but is supplemental to a developmental groove and does not mark the junction of primary parts

A

Supplemental Groove

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11
Q

This is located in the buccolingual center of the tooth and runs mesiodistally

A

Central Groove

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12
Q

A long depression or valley in the surface of a tooth between ridges and cusps, the inclines of which meet at an angle

A

Sulcus

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13
Q

A very narrow cleft or crevice at the depth of any groove, caused by the incomplete fusion of enamel during tooth development

A

Fissure

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14
Q

Small pinpoint depressions located at the junction of developmental grooves or at terminals of those grooves

A

Pits

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15
Q

A term used to describe a landmark in the central fossa of molars where developmental grooves join

A

Central Pit

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16
Q

Is an irregular depression or concavity

A

Fossa

17
Q

They are formed by the convergence of ridges terminating at a central point in the bottom of the depression where there is a junction of grooves.

A

Fossa

18
Q
A