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See also: Monocline Monoclinic Monocles Monotonous Monologue Monocracy Monotheism Monopolize Monocotyledon Monopoly Mono Monocrat Monomer Monotype Monolith Monotheistic Monopolistic Monohybrid Monoculture Monogamous Monocor Monopolized Monopolizer Monotone Monotonic Monogram Monopsony Monomania

1. Monoclines are folds consisting of two horizontal (or nearly so) limbs connected by a shorter inclined limb. They can be compared to anticlines, which consist of two inclined limbs dipping away from each other, and synclines, which consist of two inclined limbs dipping towards each other.

Monoclines

2. Anticlines, Synclines, Monoclines, Domes and Basins

Monoclines

3. Other Monoclines rumple the Colorado Plateau--the Waterpocket Fold in Capitol Reef, Comb Ridge near Bluff, the Circle Cliffs, and the Defiance Uplift

Monoclines

4. ‘The Triassic limestones are stacked along Monoclines of c.1 km thickness gently dipping toward the north.’ ‘Ductile fabrics and tectonic boundaries in the southern part of the Cine massif outline a large-scale monocline, the tectonic significance of which is not known.’

Monoclines, Massif, Monocline

5. Monoclines are single limbed folds which develop by ductile folding, or flexural slip of a layered sequence (Fig

Monoclines

6. Monoclines at Colorado National Monument and Dinosaur National Monument are especially impressive

Monoclines, Monument

7. Monocline (plural Monoclines) A unidirectional dip in strata that is not a part of an anticline or syncline A single flexure in otherwise flat-lying strata; See also

Monocline, Monoclines

8. A Anticlines, synclines, antiforms, synforms, and Monoclines B Kinks: folds with sharp, angular hinge regions C "Tightness" of folds D Classification by orientation of axial plane and plunge of fold axis E Symmetrical folds vs

Monoclines

9. The Monoclines are thought to be tangentially compressive Laramide features, and in places they show pronounced coupling action

Monoclines

10. Features depicted are limited to well documented, significant anticlines, synclines and Monoclines in Illinois

Monoclines

11. Monoclines are especially typical of platforms, where they are confined to the limbs of anteclises and syneclises.

Monoclines

12. Monoclines (see image below) are not as common and usually form as an adjustment in the surface layers to some type of tectonic activity happening deep within the Earth’s surface

Monoclines

13. Monoclines are especially typical of platforms, where they are confined to the limbs of anteclises and syneclises

Monoclines

14. Monoclines are step-like folds, in which flat rocks are upwarped or downwarped, then continue flat

Monoclines

15. Monoclines are relatively common on the Colorado Plateau where they form “reefs,” which are ridges that act as topographic barriers and should not be confused with ocean reefs (see Chapter 5)

Monoclines

16. Monoclines may be formed in several different ways (see diagram) By differential compaction over an underlying structure, particularly a large fault at the edge of a basin due to the greater compactibility of the basin fill, the amplitude of the fold will die out gradually upwards.; By mild reactivation of an earlier extensional fault during a phase of inversion causing folding in the

Monoclines, May, Mild

17. Monoclines flank the hanging wall side of surface-breaking normal faults; however, monocline growth precedes surface rupture

Monoclines, Monocline

18. Monoclines thus act as a proxy for the growth evolution of the underlying fault

Monoclines

19. The producing structures in the fields are simple Monoclines and primary recovery is driven by water

Monoclines

20. Synonyms for Monoclines in Free Thesaurus

Monoclines

21. What are synonyms for Monoclines?

Monoclines

22. Monoclines seen in the Grand Canyon are another expression of the region’s faults

Monoclines

23. Monoclines are folds, or bends, in the otherwise horizontal rock layers that dominate the canyon

Monoclines

24. Monoclines are the simplest types of folds

Monoclines

25. Monoclines occur when horizontal strata are bent upward so that the two limbs of the fold are still horizontal Anticlines Anticlines are folds where the originally horizontal strata has been folded upward, and the two limbs of the fold dip away from the hinge of …

Monoclines

26. Structural Features in Illinois - 1995 - Line Features (Axial or Flexure) of Anticlines, Synclines and Monoclines Abstract: This is a partial representation of Plate 1 from ISGS Bulletin 100 (1993)

Monoclines

27. Features depicted are limited to well documented, significant anticlines, synclines and Monoclines in Illinois.

Monoclines

28. 26th attempt Feedback Which statements are true about Monoclines? Choose one or more: A

Monoclines, More

29. The Waterpocket Fold is one of the longest continuously exposed Monoclines in the world and is the centerpiece geologic structure of Capitol Reef (Morris et al

Monoclines, Morris

30. Anticlines and synclines, Monoclines, domes and basins are all types of folds

Monoclines

31. Anticlines are arch-like, synclines are trough-like, Monoclines resemble the shape of a carpet draped over a stair step, basins are shaped like a bowl, and domes are shaped like an overturned bowl

Monoclines

32. Monoclines are, however, characteristic of regions in which sedimentary rocks have been deformed by dip slip movement along vertical or steeply dipping faults in older and deeper rocks, such as the Colorado Plateau of the southwestern United States

Monoclines, Movement

33. It is actually a complex structure of en echelon folds, asymmetrical anticlines, and Monoclines stretching from Stephenson County in northern Illinois through Lawrence County in southeastern Illinois.

Monoclines

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Dictionary

MONOCLINES [ˈmänəˌklīn]

NOUN

  • a bend in rock strata that are otherwise uniformly dipping or horizontal.

Frequently Asked Questions

What causes the formation of monoclines?

This results in the formation of a Monocline, which is a geological formation in which the rock strata has folds in it. These folds resemble steps because the entire strata leans towards the same direction. The following reasons can cause the formation of Monoclines: Fault propagation – extensional fault or reverse fault.

How does a monocline form?

Monoclines may be formed in several different ways (see diagram) By differential compaction over an underlying structure, particularly a large fault at the edge of a basin due to the greater compactibility of the basin fill, the amplitude of the fold will die out gradually upwards.

What is a monocline fold?

Monocline. Monoclines are folds consisting of two horizontal (or nearly so) limbs connected by a shorter inclined limb. They can be compared to anticlines, which consist of two inclined limbs dipping away from each other, and synclines, which consist of two inclined limbs dipping towards each other. Folds such as monoclines, anticlines,...

What does monocline mean?

monocline - a geological formation in which all strata are inclined in the same direction. geological formation, formation - (geology) the geological features of the earth.

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