GEO GIRL 😁😁.Yes I guess I was swimming here and not in the mud fans or alluvial fan you are correct 😅😊 but to be honest I wasn't fun time at geography during school but after seeing two of your videos by coincidence I became very excited and want to know and learn more and more about geography 🤩 ...thanks to you for sharing such a valuable information and i wish you also more progress and lots of success .
Thank you! :) Yes, alluvial fans are adjacent to mountain ranges where rocks pill up due to either gravity debris flows or those caused by water run off (here's a video I did over alluvial fans: ruclips.net/video/CobjL0eXG00/видео.html). On the other hand, I actually haven't heard of fluvial fans, but my guess is those are fan shaped deposits directly due to fluval (river) input. So for example, fluvial fans may be included with alluvial fans such that all fluvial fans are alluvial fans but not all alluvial fans are fluvial fans. But that is just my guess, hope it helps ;)
I used the books Depositional Sedimentary Environments: amzn.to/3kutTso and Facies models 4: amzn.to/3Fp5v3B for the information. For the images, my links are in the description of the video. At 4:10 specifically, I used figure 8 from this paper: www.researchgate.net/publication/276526949_The_role_of_sea-level_change_in_deep_water_deposition_along_a_Carbonate_Shelf_Margin_Early_and_Middle_Permian_Delaware_Basin_Implications_for_reservoir_characterization/figures?lo=1 Hope that helps! ;)
Geo is a beautiful world
From Iraq, thanks for this useful explanation
GEO GIRL 😁😁.Yes I guess I was swimming here and not in the mud fans or alluvial fan you are correct 😅😊 but to be honest I wasn't fun time at geography during school but after seeing two of your videos by coincidence I became very excited and want to know and learn more and more about geography 🤩 ...thanks to you for sharing such a valuable information and i wish you also more progress and lots of success .
Thanks so much! I am so glad my videos have excited you about these topics ;D
Thank you for the turbidite lesson.
No problem, glad you enjoyed it! :)
Wonderful explanation! I learn a lot thank you very much
You are very welcome! So glad you found this video useful :D
Thank you for the vid!
You're very welcome ;D
I wish you had this video before lol :P
Love it!
Bouma Sequence is named after Arnold Bouma, a legend in turbidite.
informative that what i want
valuable young lady thank you for a great content keep it up
Thanks, so glad you found value from it, I will keep doing my best! :D
you are amazing
Very informative video
Is there a difference between fluvial and alluvial fans
Thank you! :)
Yes, alluvial fans are adjacent to mountain ranges where rocks pill up due to either gravity debris flows or those caused by water run off (here's a video I did over alluvial fans: ruclips.net/video/CobjL0eXG00/видео.html). On the other hand, I actually haven't heard of fluvial fans, but my guess is those are fan shaped deposits directly due to fluval (river) input. So for example, fluvial fans may be included with alluvial fans such that all fluvial fans are alluvial fans but not all alluvial fans are fluvial fans. But that is just my guess, hope it helps ;)
if you allow, you can make a video on the abyssal plains, oceanic ridges, pelagic sediments, please
Thanks for the suggestion! I will look into it :)
@@GEOGIRL you are most welcome
Ahh, so turbidity is NOT from turbulent! Thank you.
from which book or paper you collected these images (4.10 mainly) please tell me i need it for reference
I used the books Depositional Sedimentary Environments: amzn.to/3kutTso and Facies models 4: amzn.to/3Fp5v3B for the information.
For the images, my links are in the description of the video. At 4:10 specifically, I used figure 8 from this paper: www.researchgate.net/publication/276526949_The_role_of_sea-level_change_in_deep_water_deposition_along_a_Carbonate_Shelf_Margin_Early_and_Middle_Permian_Delaware_Basin_Implications_for_reservoir_characterization/figures?lo=1
Hope that helps! ;)
@@GEOGIRL thanks it will help me a lot