This monoclinal fold extends for slightly over 100 miles in the desert of central Utah.

Although other boundaries appear to be monoclinal flexures, faulting is suspected at depth.

Slump: typically monoclinal, result of differential compaction or dissolution during sedimentation and lithification.

Associated with these irregular escarpments are occasional rectilinear ridges, the work of extensive erosion on monoclinal structures.

When this old-mountain lowland was broken into blocks and the blocks were tilted, their attitude, but not their structure, was monoclinal.

The province was uplifted and divided into great blocks by faults or monoclinal flexures and thus exposed to long-lasting denudation in a mid-Tertiary cycle of erosion.

Neither faults nor scarps that are possibly associated with faults or monoclinal folding appear to be common in the Beethoven quadrangle, possibly because of the high sun elevation.

This monoclinal structure forms part of a semi-continuous structure extending eastwards through the Isle of Wight as the Portland-Wight Monocline (or Disturbance).

In the north, where dislocations have invaded the field of the horizontal Columbian lavas, as in southeastern Oregon and northeastern California, the blocks are monoclinal in structure as well as in attitude.

Defining features of the landscape in the commune of Surduc are the result of selective modeling of geological substratum, consisting of sedimentary rocks of different resistance and arranged in an obvious monoclinal structure.

Its geology is similar to that of the "haut plateaux" of the Vercors Massif to the west, but differs from that of the valley to the east, which is monoclinal in structure, although still of Lower Cretaceous age.

The whole crust in the area was bent into a monocline.

At a time in the past, monocline formed to the west of Sydney.

It is the largest exposed monocline in North America.

Landslides and narrow gullies have formed along the northern edge of the monocline.

Geologically, the range is considered a monocline; part of a rifted volcanic margin.

A monocline is a step-like fold, in which one limb is roughly horizontal.

The Purbeck Monocline defines the fields southern limit.

The Lebombo monocline strikes N-S and dips to the east.

The Purbeck Monocline is a geological fold.

The outcrops lie within the Purbeck Monocline, with the beds dipping moderately steeply to the north.

Death Hollow Creek, east of The Box, has carved its way through a gently dipping monocline.

(The river then turns due-south down the East Kaibab Monocline.)

In both reverse and normal faults this leads to folding of the overlying sequence, often in the form of a monocline.

The sequence is affected by the Purbeck Monocline and dips moderately steeply to the north along its whole outcrop.

The west section of the Butte Fault is the East Kaibab Monocline.

A distinctive monocline can be seen from the historic truss bridge that crosses Middle Creek about twenty feet above the Falls.

Lapstone monocline in the Blue Mountains (Australia)

The Purbeck Monocline was formed during the late Oligocene and early Miocene epochs, about 30 million years ago.

This follows the front of the Rosedale monocline, a gently southwest-tilting formation that forms the bluffs on which Tacoma is built.

The mineralization at the mine is secondary copper minerals in a breccia zone along a monocline flexure in Navajo Sandstone.

It is a homoclinal ridge, formed from a monocline, composed of steeply tilted strata of rock protruding from the surrounding area.

Fault scarps will only be formed where a fault breaks the surface; they can either die out laterally or merge into a monocline (Fig. 3.33(A)).

When the thrusting die out the north slopes of the central Greater Caucasus form a basement uplift, forming a monocline dipping North.

The flat-lying Chuska Sandstone rests unconformably on Mesozoic rocks deformed in the Defiance monocline.

The monocline continues under the English Channel as the Wight-Bray Monocline.