Hello Connections!
We at Sarrthi IAS are looking for Hindi Translators.
Role: In-office, located in Karkarduma, Delhi.
Experience: 1-2 years.
Note: This is a full-time position, not freelance or project-based.
Interested candidates, please fill out the form: LINK
We at Sarrthi IAS are looking for Hindi Translators.
Role: In-office, located in Karkarduma, Delhi.
Experience: 1-2 years.
Note: This is a full-time position, not freelance or project-based.
Interested candidates, please fill out the form: LINK
POV - You are the one managing FEEDBACK forms 🧐🥳
✅ Wake Up
✅ Deliver awesome content & lectures to students
✅ Prepare for the next class & Sleep
✅ Repeat
✅ Wake Up
✅ Deliver awesome content & lectures to students
✅ Prepare for the next class & Sleep
✅ Repeat
History Timeline (1765 - 1875)
Understanding the timeline of historical events is crucial for both the preliminary and main exams. This information, often found at the end of each chapter in NCERT books, can be effectively reproduced in exams as flowcharts, serving as valuable additions to your answers.
We use such flowcharts in MMP+ to explain complex Mains Topics in a structured manner.
Batch 3 Starts 24th August. Call us on 9569093856 for details!
Understanding the timeline of historical events is crucial for both the preliminary and main exams. This information, often found at the end of each chapter in NCERT books, can be effectively reproduced in exams as flowcharts, serving as valuable additions to your answers.
We use such flowcharts in MMP+ to explain complex Mains Topics in a structured manner.
Batch 3 Starts 24th August. Call us on 9569093856 for details!
MMP+ Batch 3 Starts 24th August
Call us on 9569093856 to know more!
While preparing for UPSC Mains, students often:
❌ Lack content created specifically for Mains
❌ Don't go through PYQs of the last 11 years
❌ Don't practice answer writing
✅ Directly jump to Test Series
This approach is problematic. Hundreds of students end up buying costly test series, but only about 5% write till the last Mains test!
We are here to change this system with our MMP+ Program.
✅ First, focus on completing Mains Notes using GS Modules (Content + Lectures Sorted)
✅ Second, learn how to write answers through Answer Thinking Skills
✅ Next, practice answer writing - at least 5 questions in a time-bound manner
✅ Only then, attempt a Full-Length Test
Link to Course
Call us on 9569093856 to know more!
While preparing for UPSC Mains, students often:
❌ Lack content created specifically for Mains
❌ Don't go through PYQs of the last 11 years
❌ Don't practice answer writing
✅ Directly jump to Test Series
This approach is problematic. Hundreds of students end up buying costly test series, but only about 5% write till the last Mains test!
We are here to change this system with our MMP+ Program.
✅ First, focus on completing Mains Notes using GS Modules (Content + Lectures Sorted)
✅ Second, learn how to write answers through Answer Thinking Skills
✅ Next, practice answer writing - at least 5 questions in a time-bound manner
✅ Only then, attempt a Full-Length Test
Link to Course
Intrusive Forms
Lava from volcanic eruptions cools into igneous rocks either on the surface (volcanic rocks) or within the crust (plutonic rocks). When lava cools within the crust, it forms various intrusive structures.
1. Batholiths: Large, dome-shaped bodies of cooled magma found deep in the crust. They are exposed after erosion removes overlying materials & are usually granitic.
2. Laccoliths: Dome-shaped intrusive bodies with a flat base, connected to a magma source below. Resembling surface volcanic domes, they are located deeper in the crust.
3. Lapoliths, Phacoliths, & Sills: Lava moving horizontally forms various shapes. A saucer-shaped, concave body is called a lapolith. Wavy intrusive rocks at synclines' bases or anticlines' tops are phacoliths. Near-horizontal bodies are called sills (thicker) or sheets (thinner).
4. Dykes: When lava fills cracks and fissures, it cools into wall-like structures called dykes, often seen in western Maharashtra.
Lava from volcanic eruptions cools into igneous rocks either on the surface (volcanic rocks) or within the crust (plutonic rocks). When lava cools within the crust, it forms various intrusive structures.
1. Batholiths: Large, dome-shaped bodies of cooled magma found deep in the crust. They are exposed after erosion removes overlying materials & are usually granitic.
2. Laccoliths: Dome-shaped intrusive bodies with a flat base, connected to a magma source below. Resembling surface volcanic domes, they are located deeper in the crust.
3. Lapoliths, Phacoliths, & Sills: Lava moving horizontally forms various shapes. A saucer-shaped, concave body is called a lapolith. Wavy intrusive rocks at synclines' bases or anticlines' tops are phacoliths. Near-horizontal bodies are called sills (thicker) or sheets (thinner).
4. Dykes: When lava fills cracks and fissures, it cools into wall-like structures called dykes, often seen in western Maharashtra.