Now, when I examined the star- stone, the optical effects indicated the dextral situation.

Those with right-lateral motion are also known as dextral faults.

It may be classified as a dextral intra-arc transform fault.

The shell is dextral, and it has 5 whorls.

With a dextral snail this all happens fairly easily.

A maximum dextral offset of 3.5 m was recorded.

In life the shell was carried upside down with the aperture on the right, and this makes it appear to be dextral.

The shell of this species is dextral (right-handed) in coiling.

These rather featureless dextral shells are characterized by a low spire and their yellow to brown color.

The more common form of this shell is known as "left-turning" in a religious context, although scientists would call it "dextral".

Geologically speaking, the line serves as a huge dextral strike-slip fault.

This is the only dextral species in the subgenus Syndromus.

However, the shell is dextral in coiling and has an operculum.

The small, white shell shows a glassy minute apparently dextral nucleus and about six whorls.

This suggests dextral offset along a strike-slip fault.

The dextral shell is conic and solid.

The focal mechanism shows mainly dextral (right lateral) strike-slip faulting.

The mechanism of this earthquake was of dextral strike-slip faulting.

The sinistral and dextral specimens form "clear" populations but can by found sympatrically as well.

That is, when looked at from above (with the spire pointing up), most shells are "dextral," spiraling in a clockwise direction.

The main tectonic pressure was from the south or south-east, and may have resulted in dextral strike-slip faulting.

The shell is dextral, decollate, rather large, more or less fusiform, solid, dark brown, not translucent.

This image "flipping" results in a normal dextral gastropod appearing to be a rare and abnormal sinistral one.

The dextral shell is ovate oblong, subcylindrical and slender.

Valley Fault System, a dextral strike-slip fault in the Philippines.