The Basics of Geology: Converting a Topographic Profile into a Surface Cross Section Part 2

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  • เผยแพร่เมื่อ 2 ก.พ. 2025

ความคิดเห็น • 13

  • @dylanmckeen7332
    @dylanmckeen7332 3 ปีที่แล้ว +1

    Thanks for this, quite helpful. I was finishing a lab at home and definitely would have done the bedding wrong without your video

  • @1bonnotg
    @1bonnotg 8 ปีที่แล้ว +6

    Very helpful! Also, nice Wario Land music in the intro

    • @geologic7656
      @geologic7656  7 ปีที่แล้ว

      Thanks! Glad it was helpful.

  • @darkchylde3525
    @darkchylde3525 5 ปีที่แล้ว +1

    what will you do if the strike and dip is not specified on one another area (e.g. if there's no strike and dip for A, will the boundary just be a straight line?)

  • @George_77726
    @George_77726 3 ปีที่แล้ว

    thanks you. it really helpful.

  • @anandlamdhade2350
    @anandlamdhade2350 3 ปีที่แล้ว

    Thanks mate

  • @pixiejud
    @pixiejud 7 ปีที่แล้ว +3

    Very helpful indeed, but just a thing I'd like to point out. In science it is good practice to ditch the imperial system and adopt the metric system... :)

  • @mannanali1002
    @mannanali1002 7 ปีที่แล้ว

    can you please tell me how to draw dip if the dip direction is N-S for this same profile? thanking you in anticipation

    • @geologic7656
      @geologic7656  7 ปีที่แล้ว +1

      The answer is simple: you wouldn't perceive the dip because it would be going into or out of the page. It's one of the issues of using a two-dimensional diagram to represent our three-dimensional world. This is why, assuming you want to show the dip of the surface, you should always draw a cross-sectional diagram in the direction of the dip.

  • @ntumnyuygrace7723
    @ntumnyuygrace7723 9 หลายเดือนก่อน

    Sir please I don't understand that step

  • @skiidzman
    @skiidzman 6 ปีที่แล้ว +1

    Wait till you gotta do the apparent dip...

  • @mesterchinwi623
    @mesterchinwi623 6 ปีที่แล้ว

    youR Facebook pLiese ?