Відео

you are the best Geology teacher.. love from Nigeria❤❤

Beautiful. You a great teacher. Loved rhe explanation. Like to see more such ones on geology

❤ Excellently explained. Great going

simple and clear as always. thank you so much! Now I can identify faults even without the arrows given.

very clear video to explain strike and dips for dummies! thank you so much in helping me understand geological mapping.

It's really nice to see you using technology instead of white board to explain things ma'am.....looking for more

Keep coming with more such beneficial videos ma'am

Very nicely explained ma'am....keep ur work up...❤

Thank you❤

Soo much problem with that

Thankyou

Gnarly

This explanation is exactly what I needed. Thank you!

The best explanation on Strike and Dip I have come across on UA-cam. Clear, concise and visually makes sense. Thank you for posting this.

Thankyou , love the presentation I did comprehend well

Why are you drawing a rectangle instead of a circle?

I would assume that since extrusive/volcanic igneous rocks cool quickly, they'd be more aphanitic whereas intrusive/plutonic igneous rocks would tend to be more phaneritic?

Ma'am I have doubt in terms of longitudes: 1.I agree with your statement that moving from point A to be B longitude value decreased so the object is moving west 2. But we cannot say whether the object is on east or west of prime meridian without sign, how did you say that object is on west of prime meridian? If the intial starting point was 117.5° and ending point was 117° then object could've been on any side (assuming i didn't mention sign)

Very easily explained!😊

The simplest and clearest explanation I've ever seen about strike and dip conception. Thanks a lot👌👏🙏

My professer was confused himself while explaning this😂

Thank you so much, it was really helpful

i think of lattitude and change the word to LADDER, as in up and down. so if you are not going up or down then it would be LONGITUDE as in LONG lines

Thank you. Quite clear, and I didn't know yhe difference between mudstone and shale before. Seeing those in the thumbnail got me to watch.

Thanks form India

OMG totally, literally NICE👍

3:57 um sorry, isn't the mesosphere a layer of the atmosphere?

Pov: the best teacher ever😊

You're awesome 😊

Explained nicely 😊

excellent explanation!

You have an amazing way of explaining things. Please keep making these videos for future students to come across, it really helps us. Bless you.

This is really good for cramming

How come the first number is 33.5? Cause it’s between 33 and 34 latitude. Thanks?

Thank q so much.. you explained well and good. I am feom india. Keep it up 👍 😇 😉

Thanks mam ❤ love from India😊

That was wonderful! Makes sense now. Do you have a video that takes it a bit further and discusses fractional crystallization and all that stuff that is left after Bowen's does its thing and those things left that don't play pretty with the big 10 rock forming minerals ends up as an ore body or a pegmatite. I'm originally from NC and was a "rock hound" in my youth and love pegmatites :). Obviously there has to still be a lot of silica left to get silicates in pegmatites. I grew up digging around in pegmatites and hard rock mining gold. Pegmatite yield silicates combined with the left over stuff that won't bond with anything ... but there is a LOT of quartz in pegmatites. And, we had pegmatites and gold bearing ore bodies within miles of each other?? Does stuff like beryl and tourmaline fall a lot lower on Bowen's reaction series, or is just that the elements that combine to make those minerals just can't crystallize out in a melt early because they won't combine with the basic stuff in the melt. You can count the constituents of the stuff in Bowens reaction series on two hands. So all that other stuff ends up as a hydrothermal soup that makes pegmatite and ore bodies? Sorry, that's about 3 masters level university classes. Sorry, my mind runs away sometimes .....

Thank you so much for your videos! I am a geology student at a university (a VERY old geology student) and your videos really help in understanding topics that might be a little muddy. I have always thought the angle of repose was this magic angle that applied to every situation. Thinking specifically of fluvial crossbedding and you always read the angle of repose is some set number and that's written in stone. I live in a sedimentary area with some Penn fluvial crossbeds and can't make sense of the angle cos it don't seem like the textbooks. These are textbook quality fluvial crossbreeds, but the Penn is very eroded around here and just occurs on the tops of hills, so I an never sure if I'm looking at the Penn sitting on the Miss or just a boulder that might have moved a bit over the (lot) of years. Kinda neat outcrop because it really is just a large bolder and you can walk behind it and see the troughs. Don't think I can post a pic in comments or I would. The crossbreeds are compacted into maybe a couple of meters, so I have a good horizontal reference on top and bottom. Still can't make sense of it :). Thank you so much for your videos. I know you are making them for your students, but they really help a lot of other folks like me who are trying to sort things out.

Thank you ma'am

Great explanation 👍

wish high schools would teach this.

Thanks from india

Know I know how to do it 🎉😂❤

Used to ace geomorphology in highschool, and figured I'd be up for Geology. Lord was i wrong... But this eased things up just a little, sedimentary rocks are a definite nightmare, and this video is a def necessity. Highly appreciated, gracias, ngiyabonga!

what would the velocity of the ice that flowed over the rock causing the striations to be on average? Thank you

Thanks miss 🥰

My lecturer failed to explain this in 6 months. You've done it in 6 minutes

Merhaba Öğretmenim . Bazik ve asidik bunlarda etki ediyordu ?

Hi mam I have some doubts how can I solve with you

Very good video