Mining Geology - Interview Questions & Answers for Freshers.

Top Interview Questions and Answers you need to know as a Freshers

If you are preparing for a Mining Geology interview, then you have reached the right place.

Mining Engineering is a broad field of study that deals with the Mining Geology.

It is a fast-growing field that has many opportunities for career growth. A Mining Geology interview is a type of interview that is designed to assess a candidate's knowledge of Mining Engineering . The purpose of the interview is to evaluate the candidate's knowledge and deep understanding of subject.

The interview may also assess the candidate's communication skills, such as the ability to present complex information in a clear and concise manner.

The Interview is typically conducted by a hiring manager or recruiter who has experience in the field. The interviewer will typically ask a series of questions about the candidate's background and experience. The interviewer will also ask about the candidate's strengths and weaknesses.

This list of interview questions in Mining Geology includes basic-level, advanced-level, and program-based interview questions.

Here are the commonly asked question list of Mining Geology (Mining Engineering) interview questions and answers that you must prepare for fresher as well as experienced candidates to get your dream job.

1 In the Gondwana succession evidence of cold climate is obtain form

a) Talchir formation  b) Talchir and Damuda formations c) Talchir and Panchet formations d) Talchir Panchet and Mahadeva formations

Your Answer is C) Talchir and Panchet formations

Explaination is : The first evidence if a glacial action in the Gondwanas is obtained from the Talchir rocks of Orissa. The boulder bed is wide in distributoin and occurs in such areas of Hazara, Simla, grahwal, Rajasthan, orrisa and madhya pradesh. This is suggestive of the pressure of an ics sheet in India at that time.  

Another cold cycle was during Panchet, the evidence for which is composed in presense of undecomposed feldspar grains among the climate sediments.