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this video is about using strike lines to determine the strike and dip of beds so what we have here is a geologic map where the units are indicated by symbol so get units a b c d e and f and we also have typography so these dash lines in here are your top graphic contours we've got eight hundred nine hundred a thousand and then it's gonna start going uphill over here so 1000 and 1100 you've got a little valley here and you go back up to 1,000 and then one thousand one hundred and then down here we start to go downhill so we have 900 then 800 700 600 if you're familiar with the rule of v's you can see that here we've got to be pointing up and then this v is pointing up I don't really don't really go by rules but what I can see here is that I'm going downhill and that that downhill is kind of tucked in right here so if I imagine trying to hike up I could hike up here through my different elevations and then I could hike up here or hike up here so either way I'm going uphill but this one...