Noun:

அனிலன்,

anticline தமிழ் அர்த்தத்தின் உதாரணம்:

இந்த அட்ட வசுக்களில் தரா எனும் வசு புவியையும், அனலன் எனும் வசு நெருப்பையும், ஆப எனும் வசு நீரையும், அனிலன் எனும் வசு காற்றையும், துருவன் எனும் வசு துருவ நட்சத்திரத்தையும், சோமன் எனும் வசு சந்திரனையும், பிரபாசன் எனும் வசு வைகறையையும், பிரத்யூசன் எனும் வசு ஒளியையும் குறிப்பவர்கள்.

இந்த அட்ட வசுக்களில் தரா எனும் வசு புவியையும், அனலன் எனும் வசு நெருப்பையும், ஆப எனும் வசு நீரையும், அனிலன் எனும் வசு காற்றையும், துருவன் எனும் வசு துருவ நட்சத்திரத்தையும், சோமன் எனும் வசு சந்திரனையும், பிரபாசன் எனும் வசு வைகறையையும், பிரத்யூசன் எனும் வசு ஒளியையும் குறிப்பவர்கள்.

anticline's Usage Examples:

For example, in many coal regions the deposits have been conserved in some districts in the synclines or "basins," while they have been removed by denudation from the uplifted anticlines in others.

Near the crest of anticlines is commonly an enriched portion of the ground in mineralized districts; and, in the case of water supply, the tilt of the strata determines the direction of the underground flowage.

Owing to difference of density the oil and water in the anticlines separate into two layers, the upper consisting of oil which fills the anticlines, while the water remains in the synclines.

2 there is obviously a general inclination of the beds towards the71orth, besides the outward dip from the anticline and the inward dip from the syncline.

The portion of an anticline which has been removed by denudation is the "aerial arch," dotted in fig.

The observer in passing northwards along the axis of that anticline finds himself getting into progressively higher strata as the fold sinks down.

(I-17) thrown into an anticline (AA') and syncline (BB').

Where they dip away from the axis of movement the structure is termed an anticline or anticlinal fold; where they dip towards the axis, it is a syncline or synclinal fold.

The terraces may thus be regarded as flat and extended anticlines.

3), sometimes styled an "open anticline"; (2) the limbs may be parallel in "closed" folds (commonly known as isoclinal folding); (3) the limbs may make an open angle or widen out towards the crest (fig.

of England are the two Tertiary basins of London and Hampshire, separated by the dissected anticline of the Weald.

Hence the anticline noses out to the north and the syncline to the south.

The whole region may be looked upon as formed by an arch or anticline of Carboniferous strata, the axis of which runs north and south; the centre has been worn away by erosion, so that the Coal Measures have been removed, and the underlying Millstone Grit and Carboniferous Limestone exposed to the influences which form scenery.