Adjective:

क्रस्टल,

crustal शब्द के हिंदी अर्थ का उदाहरण:

छोटा जोर दोष के साथ होता है और पपड़ी overthickened है [18] कम घना महाद्वीपीय परत "मंगाई" के बाद से सघन विरासत चट्टानों के नीचे, किसी भी क्रस्टल सामग्री के वजन को ऊपर की ओर मजबूर पहाड़ियों के रूप में करने पर, पठारों या पहाड़ों में एक बहुत बड़ी विरासत में नीचे की ओर मजबूर मात्रा की उछाल बल द्वारा संतुलित किया जाना चाहिए।

इसके साथ ही भूगणित के अन्दर भूगतिकीय (geodynamical) घटनाओं (जैसे ज्वार-भाटा, ध्रुवीय गति तथा क्रस्टल-गति आदि) का भी अध्ययन किया जाता है।

इसके साथ ही भूगणित के अन्दर भूगतिकीय (geodynamical) घटनाओं (जैसे ज्वार-भाटा, ध्रुवीय गति तथा क्रस्टल-गति आदि) का भी अध्ययन किया जाता है।

कुकुम्बर सैंडविच (इंग्लैंड) क्रस्टलेस के दो पतली स्लाइस के बीच खीरा, हल्के मक्खनयुक्त सफेद रोटी।

छोटा जोर दोष के साथ होता है और पपड़ी overthickened है [18] कम घना महाद्वीपीय परत "मंगाई" के बाद से सघन विरासत चट्टानों के नीचे, किसी भी क्रस्टल सामग्री के वजन को ऊपर की ओर मजबूर पहाड़ियों के रूप में करने पर, पठारों या पहाड़ों में एक बहुत बड़ी विरासत में नीचे की ओर मजबूर मात्रा की उछाल बल द्वारा संतुलित किया जाना चाहिए।

सीज़ोमेटिकोनिक्स, क्रस्टल प्रोसेसस।

कुकुम्बर सैंडविच (इंग्लैंड) क्रस्टलेस के दो पतली स्लाइस के बीच खीरा, हल्के मक्खनयुक्त सफेद रोटी।

सीज़ोमेटिकोनिक्स, क्रस्टल प्रोसेसस।

crustal's Usage Examples:

The Pacific coast has been defined chiefly by relatively recent crustal deformations, and hence still preserves a greater relief than that of the Atlantic. The minor features of each coast will be mentioned in connexion with the land districts of which the coast-line is only the border.

The oblique trend of the coast would be even more pronounced but for a comparatively modern crustal movement, causing a depression in the northeast, with a resulting encroachment of the sea upon the land, and an elevation in the south-west, with a resulting advance of the land upon the sea.

The main point to observe in this connexion is that large tracts of land in many parts of the world were at a critical level as regards the sea, a condition highly favourable to frequent extensive incursions of marine waters over the low-lying areas in a period of extreme crustal instability.

A broad, low crustal arch extends southward at the junction of the Atlantic and Gulf coastal plains; the emerged half of the arch, constitutes the visible lowland peninsula of Florida; the submerged half extends westward under the shallow Florida.

The basins have been variously ascribed to glacial erosion, to obstruction of normal outlet valleys by barriers of glacial drift, and to crustal warping in connection with or independent of the presence of the glacial sheet.

crustal plates which move very slowly.

In North America, the crustal movements at the beginning of the period are less evident than in Europe, but a marked parallelism exists; for in the east, in the Appalachian tract, we find detrital sediments prevailing, while the open sea, with great deposits of limestone, lay out towards the west in the direction of that similar open sea which lay towards the east of Europe and extended through Asia.

The close of the period was marked by very profound changes which may be classed under three general headings: (1) the emergence of great areas which had been submerged until the closing stages of the period; (2) the beginning of the development of most of the great mountains of the west; (3) the inauguration of a protracted period of igneous activity, stimulated, no doubt, by the crustal and deeper-seated movements of the time.

In intimate relationship with the mountain-building orogenic crustal movements was the prevalence of volcanic activity during the earlier part of this period.

trend to crustal deformations which in very early geological time gave a beginning to what later came to be the Appalachian mountain system; but this system had Its climax of deformation so long ago (probably in Permian time) that it has since then been very generally reduced to moderate or low relief, and owes its present altitude either to renewed elevations along the earlier lines or to the survival of the most resistant rocks as residual mountains.