Wavy, flaser, and lenticular bedding can all be formed by tides (flood current picks up and deposits sand then suspended mud is deposited during transition from flood to ebb current). A transition from wavy to flaser bedding (more to less mud) indicates a transition to a higher flow regime (stronger current) that is able to pick up more sand. Hope that makes sense ;)
very informative video,thanks alot, could you make a video about how to draw stratigraphic charts, as well as continuing the videos on depositional environment,plus giving some insights about the hydrocarbon reservoir potentiality of different depositional environments
Technically all water experiences tides its just that except for really large lakes bordering on full fledged seas, the effect of tides is too small to be observed. This is because rather than the actual tide what we experience is the amplification it is the size of a body of water which is largely responsible of amplifying tidal influences due to hydrogen bonds pulling on each other. As a result this effect is directly proportional to the amount of water in a body of water which can slosh around amplifying the tidal effect. Without this effect the strength of lunar not to mention solar tides would be relatively tiny which is why we don't really have to worry about tides in other substances like rocks the way Io does. Oh and tidal forces depend on a -2/r^3 relationship rather than the normal 1/r^2 gravitational force because tidal forces are the derivative of gravitational forces.
I think you can turn them off ? I didn't put any subtitles, so it is probably showing whatever subtitles were automatically generated by RUclips, I think they may have size or placement options if you click on the settings icon in the bottom corner. Sorry about that!
@@GEOGIRL thanks for ur reply Types of landforms like fluvial, glacial, karst just brief about evry type in video including there depositional and erosion effects will be very helpful
![Blox Fruits Dragon Rework Update [Full Stream]](http://i.ytimg.com/vi/EqDAp8udhm0/mqdefault.jpg)
Excellent stuff. Incidentally, best in-depth prog just on tides I've seen was a preMatt PBS SpaceTime.
thank u rachel I just started reading up on tidal sediment transfer and this was a great help!
You are most certainly welcome! I am so glad I could help ;)
I am going to write my geology exam tomorrow. You really helped me to understand tidal flows. Thank you very much.❤❤
So glad you found the video helpful. Best of luck on your exam!
which university are you in?
@@EmmanuelMthombeni Wits University in South Africa
hi rachel , how does wavy , flaser and lenticular bedding are formed ? what is the meaning of the transition from wavy to flaser bedding ?
Wavy, flaser, and lenticular bedding can all be formed by tides (flood current picks up and deposits sand then suspended mud is deposited during transition from flood to ebb current). A transition from wavy to flaser bedding (more to less mud) indicates a transition to a higher flow regime (stronger current) that is able to pick up more sand. Hope that makes sense ;)
Love your enthusiasm! Sending love from another Geo Girl here 💕
Thanks so much! ;D
very informative video,thanks alot, could you make a video about how to draw stratigraphic charts, as well as continuing the videos on depositional environment,plus giving some insights about the hydrocarbon reservoir potentiality of different depositional environments
Technically all water experiences tides its just that except for really large lakes bordering on full fledged seas, the effect of tides is too small to be observed. This is because rather than the actual tide what we experience is the amplification it is the size of a body of water which is largely responsible of amplifying tidal influences due to hydrogen bonds pulling on each other. As a result this effect is directly proportional to the amount of water in a body of water which can slosh around amplifying the tidal effect.
Without this effect the strength of lunar not to mention solar tides would be relatively tiny which is why we don't really have to worry about tides in other substances like rocks the way Io does.
Oh and tidal forces depend on a -2/r^3 relationship rather than the normal 1/r^2 gravitational force because tidal forces are the derivative of gravitational forces.
that wsa an informitive.
thaks and keep it up .
Thanks, so glad it helped you!
Thank you for the explanation darling, I now understand 🙏♥️
It is almost perfect but your subtitles effects covering all the imp diagrams and points...
Please use default subtitles 🙌
I think you can turn them off ? I didn't put any subtitles, so it is probably showing whatever subtitles were automatically generated by RUclips, I think they may have size or placement options if you click on the settings icon in the bottom corner. Sorry about that!
Very helpful.
Thanks, I am so glad you found it helpful :D
Excellent video! Thanks so much. Could you please do a video on deep-water turbidites and depositional facies? Thanks in anticipation.
I have one on that topic! -> ruclips.net/video/5fvpge3KqF8/видео.html
Let me know if it answers the questions you are having about turbidites! ;)
Loving ur videos providing exact information i need
I request u to make next videos on types on landforms
Sounds great, thanks for the input! What landforms were you thinking about? And what kind of information about them would you like?
@@GEOGIRL thanks for ur reply
Types of landforms like fluvial, glacial, karst just brief about evry type in video including there depositional and erosion effects will be very helpful
@@amanmehta2161 Cool, I will start working on that!
@@GEOGIRL Thank you That would be very kind of you
You're so beautiful.