anticline


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Related to anticline: monocline
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anticline

an·ti·cline

 (ăn′tĭ-klīn′)
n. Geology
A fold with strata sloping downward on both sides from a common crest.

anticline

(ˈæntɪˌklaɪn)
n
(Geological Science) a formation of stratified rock raised up, by folding, into a broad arch so that the strata slope down on both sides from a common crest. Compare syncline

an•ti•cline

(ˈæn tɪˌklaɪn)

n.
an anticlinal rock structure.
[1860–65]
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anticline

an·ti·cline

(ăn′tĭ-klīn′)
A fold of rock layers that slope downward on both sides of a common crest. Anticlines form when rocks are compressed by plate-tectonic forces. They can be as small as a hill or as large as a mountain range. Compare syncline.

anticline

An upfold in the rocks.
Translations

anticline

[ˈæntɪˌklaɪn] nanticlinale f
References in periodicals archive ?
The Paniala Anticline appears as a north facing, asymmetric anticline exposing the Permian rocks in its core.
Seismic line 976-FZP-06 lies in Fazilpur area that shows Sakhi Sarwar anticline with a ower structure present in the core suggesting wrenching along with compression.
The hanging wall of Surghar Thrust is moderately to tightly folded with Surghar Anticline being the most prominent fault bend fold structure.
Lower Takwen Syncline, Lower Takwen Anticline, Takwen Syncline, Upper Takwen Anticline, Upper Takwen Syncline, Saloi Takwen Anticline, Saloi Syncline, Saloi Anticline, Lahr Syncline and Wahali Anticline.
Two anticlines such as Paniala Anticline in the western domain and Paharwala Anticline in the central domain selected for the desired studies, where Chhidru and Amb formations are dominantly exposed, respectively.
Imperative structural elements of the Khisor Range are the Paniala, Saiyiduwali, Mir Ali and Khisor anticlines along with a frontal fracture zone in the form of Khisor thrust zone whereas Marwat Anticline construct the key topographic expression of the Marwat Range.
The surface structural cross-section shows gentle-dipping pair of anticline (Jhatla) and syncline (Khichh) with open interlimb angle, therefore, the same, at least part of, is well manifested in the N-S trending seismic sections.