Am a geoloy student from India. I get a very good feeling when i see such type of videos when real field geologist describe about things we learned from lectures and textbooks. Hoping more such videos from you.
Clearly your animation budget is increasing. Much appreciated as a viewer and learner. Really helps to illustrate the different variations on secondary folds
I've never taken a geology class and I don't understand all of the advanced geological vocabulary but your channel is very very interesting, thank you for sharing!
I just drove past one of these yesterday on the Eastern Freeway, just 20 minutes from Melbourne. It's a very staggering and large refolded fold. Great video, as always mate, cheers.
Roadcuts are a much underrated geological teaching tool. Some beautiful folds in this one also ru-vid.com/video/%D0%B2%D0%B8%D0%B4%D0%B5%D0%BE-ENOslkR0BwI.html
The entire area is a wash with multiple fold events. When I did work at a mine to the south (Camel Creek) , we had a similar case of multiple deformation events in a greywake environment. The end result was a sort of horizontal pipes of ore progressively dipping deeper .
@@GeologyUpSkill, me too, I'm a retired Structural Geologist, for almost 50 years I taught Structural and Field Mapping, here in Brazil. Did my PhD Thesis in Scotland, Moine Thust Zone, mylonites, sheath folds and stuff like that etc... I always Watch your vídeos. Regards.
That's a nice pocket specimen! Room on your shelves? Now that we have video on demand, we can leave the large ones in the field and bring back the video...
Thank you. Last time i heard of chert was in limestone, drilling for lead and zinc at Tara mines. But i never knew if it was true. And forgot to ask my dad a geoligist then. Chert could just bluting our surface set bits..
Cherts do occur in limestones and they can make drilling pretty difficult because they are much harder than the limestone. Limestone is much less common in deep water sediments because calcium carbonate dissolves in deep ocean waters.
@@GeologyUpSkill thank you. In Liscarton and Navan, north of Dublin at arlund Tara mines. There was a quarry , that belonged to Renniks and Bennit. That was a stone quarry that produced much of the pale lime stone and dark limestone ylu will find on Dublin buildings as in O Connell street. Brian Byrne a geoligist who founded Tara mines called them the shady pales and grey whacky. Thats what we called carbonites and sulphides at the Obuasi Ashanti mine in Ghana after many beers. God bless you my friend.
