द्रोणिका हिंदी उपयोग और उदाहरण

""सुरु और जांस्कर घाटी शानदार द्रोणिका का निर्माण करती हैं।

इसे द्रोणिकाभ्रंश कहते हैं।

भ्रंशोत्थ पर्वत या ब्लॉक पर्वत का निर्माण पृथ्वी के उपरी सतहो मे भ्रन्शन के द्वारा भूभाग के उपर उठने अथवा बहुत बडे भाग के टूट कर ऊर्ध्वाधर रूप से विस्थापित होने से होता है ऊपर उठे खण्ड को उत्खण्ड(हार्स्ट) तथा नीचे धँसे खण्डों को द्रोणिका भ्रंश(ग्राबेन) कहा जाता है।

द्रोणिका इसके अंग्रेजी अर्थ का उदाहरण

The Wave consists of intersecting U-shaped troughs that have been eroded into Navajo Sandstone of Jurassic age.

The two major troughs which comprise this rock formation are wide by long and wide by long.

Initially, infrequent runoff eroded these troughs along joints within the Navajo Sandstone.

After their formation, the drainage basin, which fed rainwater to these troughs, shrank to the point that the runoff became insufficient to contribute to the cutting of these troughs.

As a result, the troughs are now almost exclusively eroded by wind, as indicated by the orientation of erosional steps and risers cut into the sandstone along their steep walls.

These erosional steps and risers are oriented relative to the predominant direction of the wind as it is now naturally funneled into and through these troughs.

A disturbance formed south of Diego Garcia on 29 February, and Météo-France La Réunion (MFR) upgraded the identified system within the monsoon trough to a tropical disturbance on the next day.

The system subsequently started to move towards the southeast during December 29, in response to a strengthening steering flow, provided by an upper level trough of low pressure and a baroclinic system near New Caledonia.

Zoe subsequently turned towards the southwest and passed in between the Solomon Islands of Anuta and Fataka, as the subtropical ridge weakened in response to an upper level trough of low pressure over the Tasman Sea.

During December 29, after the system had stalled, Zoe started to move towards the southeast in response to the strengthening steering flow, provided by an upper level trough of low pressure and a baroclinic system near New Caledonia.

The system and associated trough of low pressure, subsequently impacted Fiji and the northern islands of Vanuatu.

Folk footwear In medicine and pharmacology, a trough level or trough concentration (Ctrough) is the lowest concentration reached by a drug before the next dose is administered, often used in therapeutic drug monitoring.

The name comes from the idea that on a graph of concentration versus time, the line forms a U-shaped trough at the lowest region, before a new dose sends it higher again.