UPSC GEOGRAPHY

🌟 The 555 Program: Your Path to Excel in Anthropology 🤝 After extensive interactions with numerous students and top performers, we've gained valuable insights into the challenges that anthropology aspirants face at various stages of their preparation. 📌 These concerns span different phases, from attending classes and taking notes to truly comprehending the subject matter. Let's delve into the common issues that students encounter 📌Active Engagement: Many students find themselves in a passive mode during their preparation, which can hinder their progress significantly. 📌Content Validation: The uncertainty about whether the study materials being used are appropriate can be a significant source of stress. 📌Guidance Gap: Daily doubts arise, but often there's no accessible source for reliable guidance. 📌Expert Companion: While there may be individuals available for guidance, the constraints of time and the need for a dedicated expert companion can be challenging to address. ✅️️ Effective Note-Taking: Students often resort to preparing notes in a Question and Answer (PYQ-based) format, but they frequently miss critical aspects: a) Understanding Over Memorization b) Analytical Insights c) Content Enhancement 🎯The 555 Program is meticulously designed to surmount these challenges. It stands as the ultimate solution for excelling in anthropology. More details : Orientation video: https://t.me/shivateja_anthropology/197 Brouchure: https://t.me/shivateja_anthropology/199 Contact : Call/whatsapp: 8076822001 Telegram : @AnthroCrest. 🚨🚨Limited seats : Last few seats remaining, register before it’s full. While it's referred to as a program, it's born out of a DEEP PASSION to produce outstanding results.

■ IGNEOUS ROCKS #Rocks #Geomorphology ◇ The word igneous has been derived form a Latin word ‘Ignis’, meaning thereby fire. ◇ The rocks are formed due to cooling, solidification and crystallization of hot and molten materials known as magmas and lavas. ◇ Also called as primary rocks because these were originated first of all the rocks during the formation of upper crust of the earth on cooling, solidification and crystallization of hot and liquid magmas after the origin of the earth. ◇ All the subsequent rocks were formed, whether directly or indirectly, from the igneous rocks in one way or the other. This is why igneous rocks are also called as parent rocks. ▪︎JOIN - @upsc_geography_notes

Solve complete Daily Quiz here. Average score is 11/20. Solve: https://www.goaltideias.com/startdailyquizs-detail/936 Telegram link: https://t.me/goalTide

◇ Laccoliths - Laccoliths are formed due to injection (intrusion) of magmas along the bedding planes of horizontally bedded sedimentary rocks. Laccoliths are of mushroom shape having convex summital form. ◇ Phacoliths - are formed due to injection of magma along the anticlines and synclines in the regions of folded mountains. ◇ Lopoliths —The word lopolith has been derived from German word 'lopas' meaning thereby a shallow basin or bowl shape body. When magma is injected and solidified in a concave shallow basin whose central part is sagged downward, the resultant form of solidified magmas is called a lopolith. ◇ Sills - The sills are usually parallel to the bedding planes of sedimentary rocks. In fact, sills are formed due to injection and solidification of magmas between the bedding planes of sedimentary rocks. Thick beds of magmas are called sills whereas thin beds of magma are termed as ‘sheets . ◇ Dykes - represent wall-like formation of solidified magmas. These are mostly perpendicular to the beds of sedimentary rocks. ▪︎JOIN - @upsc_geography_notes

■ INTRUSIVE LANDFORMS #Geomorphology #Igneousrocks ◇ The magmas are solidified in different forms depending upon the hollow places such as batholiths, laccoliths, phacoliths, lopoliths, sills, dikes, etc. ◇ Batholiths - are long irregular and undulating forms of solidified intruded magmas. They are usually dome-shaped and their side walls are very steep, almost vertical. The upper portions of batholiths are seen when the super incumbent cover is removed due to continued denudation but their bases are never seen because they are buried deep within the earth.

👆8Qs in GS-1, 13Qs in GS-2 & 11Qs in GS-3 in CSE Main 2023 from our IAS Mentorship Program👈 👉 Our UPSC CSE Toppers 👉https://youtu.be/B0tOU7hlVsc 👉https://youtu.be/8484fIg4M3U 👉https://www.youtube.com/watch?v=piJ1YSx2vec 👉 https://youtu.be/ANCJR190ayc            .     👇Join👇 "IAS Mentorship Program - CSE 2024" (with Reyasat Ali sir, CSE Mentor/ educator since 2011 & experienced team) 👉*Online course 👉Batch Starts: 17th OCT 👉*Contact - 8090528260, 9319612575 For Details Visit: https://www.iasmentorship.com/?utm_source=Social+Media&utm_medium=Teligram 👉Why to join IAS Mentorship program?? (1) 👉Our Results *Tarun Bansal (AIR 204,2022 *Abhishek Vashishtha (IPS-2023 *Maya Chahar (AIR 547,2022 *Taskeen Khan (AIR 736,2022 *Nidhi Singh (AIR 748,2022 *Mohibullah Ansari (IPS-2021 *Vivek Yadav(AIR 393,CSE-2021 *ILMA AFROZ IPS-2018 (2) 👉Our Performance in CSE Main exam: Every year at least 10 to 15 Qs in each GS papers from our IAS Mentorship Program 👉Join Telegram for CSE support👇 https://t.me/+SMjIfcj3AZf6SVJy

◇ Laccoliths - Laccoliths are formed due to injection (intrusion) of magmas along the bedding planes of horizontally bedded sedimentary rocks. Laccoliths are of mushroom shape having convex summital form. ◇ Phacoliths - are formed due to injection of magma along the anticlines and synclines in the regions of folded mountains. ◇ Lopoliths —The word lopolith has been derived from German word 'lopas' meaning thereby a shallow basin or bowl shape body. When magma is injected and solidified in a concave shallow basin whose central part is sagged downward, the resultant form of solidified magmas is called a lopolith. ◇ Sills - The sills are usually parallel to the bedding planes of sedimentary rocks. In fact, sills are formed due to injection and solidification of magmas between the bedding planes of sedimentary rocks. Thick beds of magmas are called sills whereas thin beds of magma are termed as ‘sheets . ◇ Dykes - represent wall-like formation of solidified magmas. These are mostly perpendicular to the beds of sedimentary rocks. ▪︎JOIN - @upsc_geography_notes

■ INTRUSIVE LANDFORMS #Geomorphology #Igneousrocks ◇ The magmas are solidified in different forms depending upon the hollow places such as batholiths, laccoliths, phacoliths, lopoliths, sills, dikes, etc. ◇ Batholiths - are long irregular and undulating forms of solidified intruded magmas. They are usually dome-shaped and their side walls are very steep, almost vertical. The upper portions of batholiths are seen when the super incumbent cover is removed due to continued denudation but their bases are never seen because they are buried deep within the earth.

Demo Questions for UPSC Prelims Test Series 2024. Average score: 9/20. Solve: https://www.goaltideias.com/startdailyquizs-detail/992 Telegram link: https://t.me/goalTide

■ INTRUSIVE IGNEOUS ROCKS #Geomorphology #Rocks ◇ When the rising magmas during a volcanic activity do not reach the earth's surface rather they are cooled and solidified below the surface of the earth, the resultant igneous rocks are called intrusive igneous rocks. ◇ These rocks are further subdivided into two major groups of plutonic intrusive igneous rocks and hypabyssal intrusive igneous rocks. ◇ Plutonic igneous rocks are formed due to cooling of magmas very deep inside the earth. Since the rate of cooling of magmas is exceedingly slow because of high temperature prevailing there and hence there is sufficient time for the full development of large grains. ◇ Hypabyssal igneous rocks are formed due to cooling and solidification of rising magma during volcanic activity in the cracks, pores, crevices, and hollow places just beneath the earth's surface, the resultant rocks are called as hypabyssal igneous rocks. ▪︎JOIN - @upsc_geography_notes

Demo Questions for UPSC Prelims Test Series 2024. Average score: 8/20. Solve: https://www.goaltideias.com/startdailyquizs-detail/973 Telegram link: https://t.me/goalTide

■ CLASSIFICATION OF ROCKS #Geomorphology #Rocks ◇ The crustal rocks are classified on several grounds e.g. mode of formation, physical and chemical properties, locations etc. ◇ On the basis of mode of formation The rocks are divided into three broad categories :- 1. Igneous rocks 2. Sedimentary rocks, 3. Metamorphic rocks. ▪︎JOIN - @upsc_geography_notes

🎓 Listen to three visionary educators, one unified goal: Your UPSC success. 🌟 Meet India's most loved educators & UPSC Toppers on 23 October at 9 PM. Let's hear what they are telling us 👇 https://lu.ma/crackupsc2025

■ CLASSIFICATION OF ROCKS #Geomorphology #Rocks ◇ The crustal rocks are classified on several grounds e.g. mode of formation, physical and chemical properties, locations etc. ◇ On the basis of mode of formation The rocks are divided into three broad categories :- 1. Igneous rocks 2. Sedimentary rocks, 3. Metamorphic rocks. ▪︎JOIN - @upsc_geography_notes