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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 weamp;#39;ve got eight hundred nine hundred a thousand and then itamp;#39;s gonna start going uphill over here so 1000 and 1100 youamp;#39;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 youamp;#39;re familiar with the rule of vamp;#39;s you can see that here weamp;#39;ve got to be pointing up and then this v is pointing up I donamp;#39;t really donamp;#39;t really go by rules but what I can see here is that Iamp;#39;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 h