This Wednesday, join the NU Writing Center for an insightful workshop led by Dr. Carlos M Abaunza.

Workshop Highlights:

Interpreting Data: Learn how to extract rich stories from both qualitative and quantitative data.

Clear and Concise Presentation: Discover techniques for presenting your findings in a way that captivates your audience.

Visualizations and Graphs: Use visuals effectively to enhance understanding.

Essence of Research: Capture the heart of your research and communicate it effectively.

Who Should Attend?

Undergraduate and graduate students working on capstone projects, theses, or dissertations.

Anyone eager to acquire new academic writing skills.

Workshop Details:

Level: Beginner-Intermediate

Date: Wednesday, October 9, 2024

Time: 6:00pm

Location: 5E.228 Library Conference Hall, Main Campus

Reserve Your Spot: Make your free appointment at nazarbayev.mywconline.com. Don’t miss this opportunity to enhance your research communication skills!

No single scientific definition of the term exists, and it has been applied to a variety of rock features that fall into one of four general categories: - A glacial erratic is a boulder that was transported and deposited by glaciers or ice rafts to a resting place on soil, on bedrock, or on other boulders. It usually has a different lithology from the other rocks around it. Not all glacial erratics are balancing rocks; some are firmly seated on the ground. Some balancing erratics have come to be known as rocking stones, also known as logan rocks, logan stones, or logans, because they are so finely balanced that the application of just a small force may cause them to rock or sway. A good example of a rocking stone is the Logan Rock in Cornwall, England, United Kingdom; another is the Trembling Rock in Brittany, France. - A perched block, also known as a perched boulder or perched rock, is a large, detached rock fragment that most commonly was transported and deposited by a glacier to a resting place on glacial till, often on the side of a hill or slope. Some perched blocks were not produced by glacial action, but were the aftermath of a rock fall, landslide, or avalanche.

An erosional remnant is a persisting rock formation that remains after extensive wind, water, and/or chemical erosion. To the untrained eye, it may appear to be visually like a glacial erratic, but instead of being transported and deposited, it was carved from the local bedrock. Many good examples of erosional remnants are seen in Karlu Karlu/Devils Marbles Conservation Reserve in the Northern Territory of Australia. - A pedestal rock, also known as a rock pedestal or mushroom rock, is not a true balancing rock, but is a single continuous rock form with a very small base leading up to a much larger crown. Some of these formations are called balancing rocks because of their appearance. The undercut base was attributed for many years to simple wind abrasion, but is now believed to result from a combination of wind and enhanced chemical weathering at the base where moisture would be retained longest. Some pedestal rocks sitting on taller spire formations are known as hoodoos.

We are thrilled to announce that the Wildcard Competition of the NU Three Minute Thesis (3MT) for 2024 will take place on Tuesday, September 10, in the Senate Hall of Block 1. The 3MT competition challenges students to present their thesis research in just three minutes, using only one slide, making it an excellent opportunity to hone your presentation skills and engage with a broader audience. The Wildcard Competition is a special round where School People's Choice winners get another chance to compete for a spot in the NU Finale scheduled for September 20. Don’t miss this exciting event and come support your peers as they showcase their research in a dynamic and engaging format!

NU Graduate Studies Office is excited to invite you to the University Final of the 3MT (Three Minute Thesis) Competition, where PhD students will showcase their research in just 3 minutes! Date: 20th September 2024 Venue: Green Hall, Block C2 Time: 5:30 PM Come and support our talented graduate students as they present their innovative ideas and research breakthroughs. This is a great opportunity to learn, network, and be inspired by the work being done in our community. We look forward to seeing you there!

No single scientific definition of the term exists, and it has been applied to a variety of rock features that fall into one of four general categories: - A glacial erratic is a boulder that was transported and deposited by glaciers or ice rafts to a resting place on soil, on bedrock, or on other boulders. It usually has a different lithology from the other rocks around it. Not all glacial erratics are balancing rocks; some are firmly seated on the ground. Some balancing erratics have come to be known as rocking stones, also known as logan rocks, logan stones, or logans, because they are so finely balanced that the application of just a small force may cause them to rock or sway. A good example of a rocking stone is the Logan Rock in Cornwall, England, United Kingdom; another is the Trembling Rock in Brittany, France. - A perched block, also known as a perched boulder or perched rock, is a large, detached rock fragment that most commonly was transported and deposited by a glacier to a resting place on glacial till, often on the side of a hill or slope. Some perched blocks were not produced by glacial action, but were the aftermath of a rock fall, landslide, or avalanche.

An erosional remnant is a persisting rock formation that remains after extensive wind, water, and/or chemical erosion. To the untrained eye, it may appear to be visually like a glacial erratic, but instead of being transported and deposited, it was carved from the local bedrock. Many good examples of erosional remnants are seen in Karlu Karlu/Devils Marbles Conservation Reserve in the Northern Territory of Australia. - A pedestal rock, also known as a rock pedestal or mushroom rock, is not a true balancing rock, but is a single continuous rock form with a very small base leading up to a much larger crown. Some of these formations are called balancing rocks because of their appearance. The undercut base was attributed for many years to simple wind abrasion, but is now believed to result from a combination of wind and enhanced chemical weathering at the base where moisture would be retained longest. Some pedestal rocks sitting on taller spire formations are known as hoodoos.