Opening My Gold Mine! Part 13: Gold Mine Geology

hey guys my name is Jason with Mount Baker mining  metals and we're back here at my new gold mine   today this video is going to be a little bit  different I have a really good friend of mine   we went to school together he's one of the best  GEOS I know work for big companies done a lot of   exploration work and we're going to do a little  geology lesson today on how gold veins form but   let me see if I can wave my arms here and show  you some of the big structures we're going to be   talking about today well let's see if this works  here this is the mountain face that holds three   different vein structures actually Four that we're  going to be talking about today off and on but to   get you oriented here's our road going up to our  blacksmith shop is right over here we go in about   600 ft through the mountain hit the Rays go up  the Rays connect through the transfer way and   then here is the Stope that we're working in these  are the vent holes this is where our Escape way is   this is vein number one I'll reference this as  vein number one and we're working over here our   Stope is in the mountain right about here and  we're working our way to the east this is East   towards this big huge fault structure right here  we're going to reference this a lot today this   is what we call the Norths South trending fault in  the underground workings there's a raise that runs   right up the fault and comes out right underneath  that big rock there so that's the vein we're   mining there's another structure right here you  can see the white comes up under vein number one   we're going to talk about we're going to go look  at it today we kind of think it rolls into this   structure comes across the hill there's a little  bit of a vein wisp there and then up changes the   orientation of the vein much more steeply dipping  there's two other veins that we're not going to   see today but I'll mention them while we're here  there's one here that's almost vertically dipping   and more Norths South trending and there's one way  up here on top of the mountain and that's the old   one that the oldtimers worked it was really really  rich but what I wanted to mention also this all   this whole Mountain here this is Cliff former  is a fillite it's a metamorphosed sedimentary   rock and the theory was this was old sea floor  sediments that had some lowgrade gold in them they   got accreted onto the North American Plate there  was some vulcanism that happened all this slope   forming stuff over here this is all an intrusive  diorite so as you had this intrusive diorite   come in hot fluids were circulating through this  system dissolving all the gold out and then they   got later injected back into the the host Rock  here and you have these gold veins come out that   we're mining now today I keep getting raindrops on  my camera so that kind of gives you a little bit   more of the local geology what's going on here  hey this is my buddy Dale morning guys up here   at uh Jason's new Gold Mine scratching around uh  we're going to do a little arm waving on Surface   so I like to spend my free time up here in the  cold rain and wind uh playing with the Rocks so   should be a good day yeah we should hopefully  uh come up with some crazy ideas and you know   see where that takes us yeah want to bring you  guys along and on this beautiful summer day here   in the Cascades yeah it's about normal yeah so  Tamar geological Services uh we started out kind   of core logging uh support for exploration compan  iies around Western North America we nowadays we   do a lot of geologic modeling uh some resource  work uh geophysical modeling pretty much all the   fancy stuff that people like to see in 3d uh  take a take a deposit like this put it in 3D   space so that way people can understand a little  better what they're doing any other exploration   support line cutting soil sampling mapping we do  underground work as well so you know we're pretty   we got a varied skill set and a fire up crew of  GEOS running around the Northwest hit us up if   you're if you need a little bit of this on your  site and uh we'll see where it goes and if you're   interested in some more info on tamarak I'll leave  a link to their website down the description below   so check them out they're doing a lot of cool  stuff so we're going to start today we're right   outside the blacksmith shop portal and we're going  to talk about the host Rock for the veins this is   a Jurassic filite so this is kind of what we're  dealing with this is in some spots they have a   lot of court ringers running through them we  would call that sweat quartz I don't see any   right in here much on this side yeah there's  a little bit and then you got the foliation   plane which is really kind of we're wondering  how important it is with the the rest of the   system is kind of parallel to my hammer and you  can see it you know it's kind of separates these   layers in here in this fresh outcrop and when we  get over to the other side you'll be able to see   the quartz veins or the sweat quartz is kind of  parallel to that foliation plan right and so one   of the things we're going to think about today is  how that plays with um the rest of the system and   this is the contact between the filite here on  the right which is the west and the diorite or   the intrusive on the East so we're going to take a  walk right over here into these bushes find a nice   outcrop of the diorite so you can compare what the  filite looks like that gray massive kind of boring   looking stuff to the diorite and the intrusive  we're about 2 or 300 ft from the blacksmith   shop portal now and I wanted to show you this is  the intrusive right here so it looks a whole lot   different from the fillite there's light colored  grains in there some dark colored grains this is   a weathered surface but this was a big body of  magma that intruded into the surrounding Rock   and may be the source for our gold veins dude that  is a wicked Hammer you got there oh yeah it's you   tool it's uh doubles as a walking stick a digger  it'll cook your breakfast in the morning y it's   my new favorite yeah so here we're just looking  at more of that oxidized intrusive um one of the   things you know you'd be looking for if you're  trying to find more veins or how this is related   to our veins is some alteration in this diorite  um alterations a pretty big subject but uh right   now I'm not really seeing much in here aside  from aside from just some oxidation from the   surface uh so that's one of the things we're kind  of curious about here is the relationship and the   timing between this intrusive and uh the veins  Jason's got gone so about the only place you can   find out crops around here cuz that's what most  of it looks like but the only place you can find   outcrop in the stream beds so this is a pretty  good look at that intrusive again there you go   yeah a little less weathered huh yeah little  less weathered yeah so one of the things you're   looking for in here is uh you know if there's  any Clays around it could be an indication that   we have some hyd type of hydrothermal alteration  around so just a real quick note here all this   Cliff forming stuff here is filite and then right  there is the contact and it turns into this kind   of slope former got all this Talis it's all filite  but then looking around this is all the intrusive   that's much more slope forming there's no Cliffs  out there at all so you can tell just from kind   of looking around at the landscape where you might  have some different rock types just by their slope   forming Cliff forming relationships I wanted to  get you a little a little wider view before we   get up there we're working our way right up that  real steep north south trending fault there's that   big Flat Rock I pointed out earlier what I want  to do is get up here and I want to show you the   vein how it cross Cuts this fault and it appears  that this fault may be older than the vein system   because the vein isn't displaced at all one  of the things we're going to talk a lot about   today is what's controlling the grade cuz there a  minor that's what I care about the most I want to   go mine the highest grade stuff and there's some  there's some evidence that these high angle Faults   Are what's controlling some of the grade in these  systems and the closer that you get to these fault   systems these fault vein intercepts the higher and  the higher grade gets in the veins all right so   this is a piece of a mayic dyke that runs right up  the fault and we'll see this outcrop underground   so when we whack this thing open you're going  to see the difference from the intrusive that   we saw earlier that's much more felic has a lot  more quartz and this is quite a bit more maic so   we shouldn't see hardly any Quartz in this it'll  be real dark real black oh yeah there we go tool   that's what I'm talking about so there's a little  weathering rind where it's been laying on the   surface and oxidized in but once you get into the  clean brake very very fine grained so that tells   us that as it was intruded or injected into the  system it cooled very very fast the grains didn't   have time to grow big and it's also very mic so  yeah you're you know this is very different than   that diorite yep over there and very different  than the fill light mhm yep and hanging out in   this fault that we're standing in here which is  also normal the the dyes really like to squeeze   into existing faults just cuz there's some open  space there exactly ready to take it we've reached   the big Flat Rock I can walk through that hole so  that gives you some scale that think's probably 20   to 30 ft tall and the reason why there's this big  slash to the mountain is you have this fault Zone   that's a weak area in the Rock and as the water  starts trickling down the fault it's a much easier   path to a road for the water over a long long time  the water just eats this huge gash to the mountain   side and it shows where the weak structure of  the fault is and that's how we can follow these   north south trending structures by the erosional  features the fault Ray comes out right up under   this big rock I wanted to pan over and show you  there's quartz running right through there up   on the surface and there's actually two different  quartz veins there's that one and there's another   one that's running up higher than this lower  one and they're separated by about 6 8 10 ft   of weight waste and that's the big question I've  talked a little bit in my past videos about two   different generations of quartz are we looking at  a first generation and a second generation are we   looking at uh kind of a a split section where you  had the vein come into a structure that was maybe   a little bit screwed up and you have two different  systems that have gotten multiple generations of   quarts that's one of the main questions the  other one is does one of these have all the   goodies all the gold and the values and another  one is just Barren this is the lower vein you've   got some Quartz in here all the way up through  this area a fairly well defined hanging wall   coming down here and then this is all waste right  here starting about right here all the way up and   then you get this other little Stringer quartz  and it's hard to tell but I think this is more   or less the foot wall and it runs all the way up  to there so maybe a twoot wide vein here maybe a   2 and 1/2 or 3ot wide vein here and as they work  their way up the side of the Hill they actually   start to separate some cuz one comes here and  one starts to go up the hill at a steeper angle   Dale's checking out vein I'm going to walk  under this big rock and I'll show you right here it's plugged now but right here is where  the fault raise breaks out onto the surface   we're under this big huge Rock right here all this  stuff is being sheltered by this big rock but if   we broke through here we could actually access  the workings down in the blacksmith holway so   this raise comes right up this fault and actually  is there a vein right there looks like there might   be some quartz right there so the vein the  Rays may have followed the vein all the way   up and if you look over here Dale's work in the  vein in the exact same elevation I'm SI sitting   on it the fault raise comes up through and then  there's some quartz right there on the hanging   wall so the fault does not displace the vein  which is very very interesting but may control   some of the grade we'll talk about this a little  bit more underground but there's two different   characteristics of quartz here this is a fairly  coarse grain there's some vuggy stuff a little   bit bigger a whole lot rustier this is this is  what I think might be the first generation which   doesn't carry much gold and this is a much wider  much more fine grain and this is what I've been   finding a lot of the good gold in underground  and so this is the stuff here that we're going   to be trying to identify in these vein systems on  the surface right we're waving our arms about our   two generations Dale's Got a Theory yeah I mean  I'm just kind of thinking you know you have your   your early generation of quartz van um it's there  it happened however it happened and then you have   this second generation that Jason's found that  really carries the grade and you know I'm Pro I'm   thinking of that as kind of its own independent  later thing like it happened in a similar time   frame probably but probably under some slightly  different stresses and so it's kind of cruising   around through the the original quartz vein um  probably because there's a rock strength contrast   there between the filite and the quarts and then  as the original quartz vanan changes orientation   you probably have that that second generation  cross cutting through it for some period of time   maybe it's in the middle of the main bin which  I think you've seen maybe it pops over under the   foot wall or back on the Hang wall it's kind of  its own independent thing um after the fact after   this original courts bin was put in place and  we were just this came up because we were just   talking about one of the other um Banes on this  property and how the the payzone is on the foot   wall we've got some interesting theories about  maybe what's going on there but they're all pretty   big tbds a lot of ideas not a lot of data yeah  exactly well we're finishing up here the lower   vein doesn't seem to have any goodies in it the  upper vein up here right up against the hanging   wall appears to have some really good stuff so  that'll be key when we go underground and we   talk about where the gold might be we're taking  a look at our two veins on the east side of the   fault comes under the big rock where the veins  exposed right at the Rays and we've identified   a spot over here Dale's working it yep that's  quartz Vin all right all right so we got our   vein it works right up here it's really hard to  see on the surface but I think this is it right   here it's about 8 or 10 Ines wide Works its way  right up under these trees and the other thing   this shows is we've got our quartz vein coming  down right across the fault and no dis placement   so the fault either did not displace hardly any  on its initial movement or the cords vein is   younger than the fault and Crosscut the fault  we're working our way around the hill now and   we're standing at the bottom of this more or less  vertical vein that's going up and intersecting our   Stope and for those of you who have seen my videos  over the past couple years this is a spot where I   took a round here a couple years ago so let's go  and take a look at some of the structure here here   and how it might interact with the Stope above  us but here's the lower section of the blast I   haven't got my excavator up here to muck this  out yet but it's really bellying out here it's   doing a little curve around maybe coming quite  a bit more flat Ling and as soon as it goes up   into the vertical position it pinches but then  above up in here there's some spots where it's   up 6 ft wide Works its way up the structure  here and our Stope is right above those little   bushes this is a real interesting spot the  oldtimers didn't focus on this vein hardly at all but I'd really like to understand how this  structure and this vein system interacts with   the current vein we're working so this is  another section where we have a very well   super well- defined hanging wall and within  the vein structure itself almost another very   very well-defined find separation between  the quartz this generation of quarts and   maybe another section of quartz here that came  in and intruded into the same structure and the   question again is what is controlling the grade  in these veins and am I looking in the upper   vein the lower vein do both Generations have  gold lot of big questions so right now we're   on the east side of the fall right we're on  the side of the fault we've just come in the   blacksmith shop we've just rounded the corner in  our first exposure to the vein can you point out   kind of where the vein is there it's a little  skinny guy there you go about 8 in 10 in Works   its way up and around it's a little wider  over there and coming down here the vein continues right there along the wall they drifted  on it all the way out to the surface but there's   no value down here in this vein section and here  in about another 30 ft we'll show you just like on   the east side of the Fault when we were outside  this is the lower of the two veins and there's   an upper vein just right around the corner where  Dale's getting to and they did quite a bit more   work on that vein so we're looking can you show us  the lower vein real hard to tell I don't know yeah   so you got some you've got some vein right there  that's the lower vein that's what we walked in on   and they drifted in on eventually and then they  got here and they realized that there's actually   two veins here separated by waist so from about  Dale's head up to about here is all waste and   then that sucker right there which is about about  3 and 1/2 4 ft wide is all quartz vein and that   is the upper vein we saw it outside that's where I  saw the goodies so what's your takeaway here Jason   you got you got the two veins you got some filite  yeah I I think this is the same upper vein that   we saw on the surface up in the fault we're still  on the east side of the fault I believe the upper   veins carrying the goodies the lower vein over my  right shoulder is pretty much Barren and for some   reason those old guys followed the barren one back  to the fault raay so this would be another Target   for me in the near future cuz we're so close  to the blacksmith shop bring in the drill clean   out this area and get back there and do a couple  rounds up see if I can develop anything up on this   this nice wide minable width bin that hopefully  has some gold in it yep and surface we saw the   the good stuff was in the hanging wall of the  upper vein correct and you're were just looking   at the hanging wall of the upper vein here Y and  it it looked positive look good yeah yeah good   looking stuff okay so this is definitely another  Target for the future all right I like it and   actually when we were putting in this Timber wall  I was scaling right up here found some goodlook   stuff once I got it on the ground I told Chad and  Harry about it and they put it in a bucket for me   I took it home slobbed it up and it's some really  really hot juicy stuff lots of gold in it so this   upper vein here has some really nice gold and  I want to show you here this is the drift where   the lower vein goes takes a little left hand turn  there if you can see going around the corner it's   separating from the upper vein which the old guys  drifted on here and we've blocked it off since but   that has a quite a bit different orientation and  they drifted down on this and there was an old Geo   in the in the'80s that came in took some samples  of this vein and it was running with some gold   they drifted up here on this a couple of raises  we've timbered up one here one over above Dale   there you can see the vein they went up about I  don't know 60 ft or so and never developed much   but there was something good here there's also  right over here there's a little winds we'll go   take a look at that so here's a section and it's  hard to tell is this the upper vein to here and   the lower vein here and they've actually come  together in the same structure if you look over   on this wall then you can see they're separated  again there's one on the lower piece here waist   in the middle and then Vein on the upper piece so  they've come together almost in this section here   right over at the sump this is a winds and they  winds down on it they followed the vein down I   don't know if we can get a good view of it these  old workings are it's real hard to see but this is   mostly vein here I think this the veins that come  together they chased them down there's some vein   stockwork looking stuff here which is probably  the structure of the upper vein but the old guys   chose to follow the lower vein which is right here  here's a good spot lower vein here very nice well-   defined foot wall big horse to waste and then the  upper vein there that follows its way down this   way into the sump and that's where they winds down  and they chose to follow the lower vein for some   reason and after this part we're going to walk  all the way to the fault rays but there's hardly   any development work the vein assay pretty much  nothing for gold and I'm wondering if you go down   here 50 ft and turn left and drill into the wall  20 ft if you find a really well defined secondary   vein that has all the gold in it that's the big  mystery on this side of the fault here's our fault rays here's the Dyke okay that's that  mayic dyke oh yeah and I think there's   a fresh spot on your left that  I scaled some off of behind you   right over here down low at your  hip level yeah and so there's that dice it's pretty rotten yeah that's that  fine grain stuff and so we believe that it   runs right up the fault here and this comes  out right underneath that big rock so we're   going to pull these boards off see if we can  get up in there and take a look but right here   in this level oh look there's some quartz there  yeah but we've been following this back for what   over 100 ft from where we last Saw quartz  vein we're following structure but didn't   see any any veins and on this side there's  nothing so we've taken off the boards we're   looking up the fault Rays here and we're  going to take a little climb I'll show you   where the veins are exposed in The Fault Rays  the Bale's coming up I about 10 ft here's the   structure of the fault get my finger out of the  way right here yeah real nice defined structure and they followed it right up the  Rays but what I'm interested is to   find the veins see if I can  climb and film at the same time and so what we have is just up around the  corner boom We blow up into this nice big wide   well defined quartz vein and they followed  it right up Thea nice oh yeah so that quartz   yeah so ridle me this so on your right hand  there's a pretty well- defined quartz vein   right there with the steel sticking out of  it yeah and then look behind you you got all filite yes you do and now look come on up here a  little bit farther and now look over your   head you got a very nice well-defined  quartz vein running right across the fall yeah sure enough so I haven't been  up here in a long time and here's my new   Theory the first generation came in on that  on this structure over here this guy yeah came across and at the time it came across this side  of the fault was up high the fault had 6 feet of   movement in it dropped this down and the second  generation of quartz came in the same structure   cut right across the fault and kept on going  so this is first gen that's first generation   has been dropped down 6 ft and this is second  generation on the left side of the fault the   east side right and this is both Generations  on the right side so in the Stope you have   one welldefined vein with two generations this  guy yeah yeah on the west side and on the east   side you have two separate quartz veins because  the fall offset them by six feet between the   intrusions we saw this down in the drift we were  just walking we saw it down separ and we saw it   on the surface on the east side of the vein or  east side of the fault I mean here you can see   right there some of those big intrusions of  the Xeno list we were talking about of wall   rock yeah were ripped through Y and then the  vein move or the fault moved the vein down and   the second generation came through off across  yeah yeah I like that I think also you have   evidence for that outside because we didn't see  any reasonable offset on this structure out in   theault goalie correct there could be a little bit  but it wasn't it wasn't significant it wasn't like   you know dozens of feet or 100t right right so  I think the upper Vein on the east side of the fault is the second generation and in the sto  they're mixed I think that's a pretty good I think   that's a pretty good idea Jason so if that's true  then we would expect to see some pretty good good   grades in the hanging wall or somewhere through  this one agreed dead here dead dead there some   good minerals the in the second gen op and does  this look like the other quarts that you the the   type of quarts that you typically have identified  as being just kind of the Dead Bulls ver gen yes   absolutely and this stuff up here has the more  kind of sugary texture to it but yeah this lower   vein here it looks it looks like the stuff I would  not be interested in the sto the xenis in there   pieces of wall Rock the bread see some real nice  bation going along right along the bottom yeah   yeah and typically that stuff assays nothing  nothing nothing nice it's really continuous   man all the way up there it is and we can follow  it all the way up that the the vein is continuous   all the way to the surface awesome but look at how  breated it is in here it entrained a whole bunch   of nasty stuff yep yep all the way up definitely  it looks like there's more of it kind of down here   so it's kind of fingering fingering down through  this Zone picking up a lot of waste hor along the   way yeah we're up here in the Stope since we took  our round you can kind of get a real good look at   what we're looking at and I think what we're  seeing I've talked about this on some of the   other videos you've got two generations of quartz  the upper section here we'll take a closer look is   more or less Barren it's mostly bull quartz white  quartz you've got some of these big xenoliths that   fill light in there some of the smaller ones have  been altered pretty good and it kind of grades   into the hanging wall here little veinlets around  and then you have a second generation which has   made a very nice contact with the first generation  running across it makes a real nice hanging wall   contact right there I want to go look at but that  filite is a horse to waste in the middle of the   first generation the second generation the second  generation kind of Peters out into the foot wall   there but the second generation especially in  the Stope is much more white in color has some   really nice ptite stringers running through it  and then typically right at the hanging wall   contact right there is where we find the really  really juicy stuff and this is where I've been   bringing everybody up and we've been pulling out  grams and grams from a few bags out of this spot   right here it's nice that you have this sulfide  pastry coming through that you can follow that   really defines the the second generation and then  as you're moving forward towards that Vault raise   um if the if the overall system starts to change  orientations with the second gen stays linear   you'll have something nice to follow and it'll  be interesting to see how that plays with what   we saw in the vault r with the two separate veins  up by that North trending Vault yeah you got to   stick on the second generation mhm well and to get  everybody oriented here a little bit if we shoot   about 20 ft this way we intersect the fault Rays  well no if we shoot 20 fet this way we intersect   the fault and then I got to turn and we got to  drift about 30 ft through the fault to intersect   the fault rays and then we can start sending the  muck down the fault rays but how accurate is our   mapping does the vein start doing weird stuff  does it drop off as it gets to The Fault does   it pinch um we're not that's that's kind of our  best guess but my strategy is stay in the pay   mine towards the fault and figure out what happens  when you get there yeah the overall vein systems   probably going to change orientation a fair bit  we've seen it all over the site hopefully the pay   stays reasonably linear yeah well in some of the  areas of the pillars in the Stope the pillars that   they left you get some really really nice pce  streaks right up against the hanging wall and   so it almost seems like second generation kind of  Dipsy Doodles through the vein and in this section   it's kind of more towards the middle but on some  of those pillars you get it right up against the   hanging wall yeah and it's also dipping refly  30° over there right it's flat here y well and   you actually see it here some as this comes across  you know you're getting real close to the hanging   wall here you're only about 6 in away from the  hanging wall right so it's working its way up it   almost looks like the second generation maybe  took a a sweep up here and this one just came   like a laser beam right across right I mean it's  only dipping about what a few degrees yeah it's   pretty flat but it just carries on right across  there right back behind Dale yeah and you got a   lot of pure side all the way down through a  Zone probably foot and a half right through   here yeah and how's the peer Tite is the pier Tite  a good indicator of the gold I think the ptite is   a really good indicator of the second generation  but I think the gold sticks right up against the   hanging wall right up yeah or right right at the  contact or somewhere like that we're looking right   under here where the second generation comes  up and that is really really nice and smooth   it's very smooth if you had so you know when you  only have one or two Chatters you got to be pretty   skeptical about it but let's say those were were  good Chatters and we were pretty confident in it   the way you can work out which way this fault's  moved is by moving your hand over the surface   and feeling which Direction's rough and which  Direction's smooth the direction that's rough   where my hand is on the what would be the foot  wall of this fault couldn't move that way so it   had to have moved this way in this case we don't  know because there's only a couple and it's not   very convincing but that's one of the ways you  can you can work out the kinematics rough this   way this block couldn't have moved that way mhm  had to moved this way uhhuh so then you know   you could picture at some point when this fault  was doing its thing all of this lower stuff was   moving that direction yep and you can work out the  direction based on the the lineations and uh the   direction of the of the movement and then also  um you know the Chatters help with that as well   the chatter marks shatters if you if you've got  some good indicators you can really dial in the   direction and the uh attitude is that the right  word yeah the movement the movement Direction   mhm yeah and that a word that describes all of  that is just the kinematics and kinematics is   just how it moves moves and uh yeah it'd be cool  to find find something more convincing but that's   a really good fault sck yeah really good contact  and the interesting thing we've talked about this   I don't know if I got on camera earlier is the  idea in a lot of veins is you get this fluid and   placed in this in this situation where it's right  against the wall rock you have a very very smooth   well-defined contact and there is absolutely  no alteration no baking no nothing I'm actually   looking over here is there any is there any sort  of like it's all screwed up obviously but is there   any sort of drag in the foliation yes see I was  just I was just thinking we could point that out   because that's another way that you can verify the  the kinematics cuz we said that this wall what did   we say this wall couldn't go that way it had to go  this way uhhuh which means that this one's going   that way right and so you can see if this block  is moving that way does that work with those I   don't I don't I think the orientation screwed  up I think they would be opposite opposite it   almost looks like the top one needs to be going  that way yeah it would dragging the foliation   but I don't it's so chaotic here you can't really  tell but the point being that it's that it's um   there's it's it's very unusual I think to have  such a well-defined contact with no alteration   or change in the in the host Rock I mean it's just  it's it's a laser beam contact and you can't even   tell I mean if you were just looking at this  section of rock you'd never from here up you'd   never even know there was a vein half an inch  down it's crazy yeah yeah if those those would   need to be dragging like this uhhuh according  to those chap those C Chatters could be BS too   yeah there is one so you know this is probably a  better the dragging of the foliation into the um   into the faults probably a better indicator of  the kinematics sure all right guys well thanks   for watching our video hope you enjoyed a couple  of GEOS doing some arm waving underground Dale   how'd you like it yeah it's good you know it's  the third time I've been up here every time you   learn something new I think today we you know  did some heavy arm waving and come up with some   good questions and you know at the end of the day  Jason's he's got the gold in the face and that's   what matters so that's right now I got to make  sense everything we talked about today to find   more gold so yeah but yeah if you haven't checked  out Dale's website check it out Tam geology I'll   leave a link below thanks again everybody  for watching we'll see you on the next video

Channel: mbmmllc

Views: 34,847

Keywords: mbmm, mbmmllc

Id: LQh4-mlKg6Y

Length: 40min 17sec (2417 seconds)

Published: Sun Nov 26 2023