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| Terry Tate Videos |
Published
06/21/2005
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All Videos , Funny Videos , Extreme Videos , Commercials , Sports Videos
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The Terry Tate Collection has to be among the best series of commercials of all time. Here they are...all of them, to enjoy...Just don't take the last cup of coffee, DOUG! WOOOOOOOOOO!!!
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Comments
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Comment #1
(Posted by an unknown user)
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WOOO! I am considering going Terry Tate on my co-worker Joe. He keeps taking down our internet connection.
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Comment #2
(Posted by an unknown user)
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It's funny but most of all, we all know someone that we would like to hit like the TTT!!!
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Comment #3
(Posted by Terry Tates #1 Fan)
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I love Terry Tate
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Comment #4
(Posted by an unknown user)
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terry tate is the farken maddest crunt in the the whole farken world
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Comment #5
(Posted by an unknown user)
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comment one if ur a grown man why would u be watching internet movies when ur suposed to be mature dum fucken cunt
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Comment #6
(Posted by an unknown user)
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...yes
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Comment #7
(Posted by fundamentals35@hotmail.com)
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THAT WAS FUCKIN SICK BABY!! WOOO!!
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Comment #8
(Posted by an unknown user)
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terry tate rocks!!!!! wwooooooo
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Comment #9
(Posted by an unknown user)
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funniest commercial ever
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Comment #10
(Posted by an unknown user)
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Right Doggy What Happen To Terry Tate
Neo_cy_pher@hotmail.com ATrian
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Comment #11
(Posted by an unknown user)
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OMG...These videos are hilarious!!! I love Terry Tate and like they say every office could use and Office Linebacker!!
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Comment #12
(Posted by an unknown user)
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Terry Tate is awsome and anyone who tinks otherise is really dumb
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Comment #13
(Posted by an unknown user)
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i luv u!
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Comment #14
(Posted by an unknown user)
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Terry tate is my freaken idol! I'd love to tackle the hell out of a coworker like TTT!!!!!!!!!
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Comment #15
(Posted by an unknown user)
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This is HILARIOUS
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Comment #16
(Posted by an unknown user)
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Hey comment #5 shut the hell up faggot
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Comment #17
(Posted by an unknown user)
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because you guys fucking suck!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! and i boned your mothers
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Comment #18
(Posted by an unknown user)
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i love these
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Comment #19
(Posted by an unknown user)
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Terry Tate is absolutely hilarious ... and he keeps workers productive to boot! LOL
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Comment #20
(Posted by an unknown user)
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#5 and #22 Can suck on his lolipop. TTT rocks.
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Comment #21
(Posted by steve.UK.)
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Absolutely amazing, come on the Tate. These aint yo pens richard......Yo ass must be crazy!
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Comment #22
(Posted by CRAIG)
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THAT'S A LONG DISTANCE CALL! DOUG!
OMGZORS
OMGZORS
OMGZORS
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Comment #23
(Posted by an unknown user)
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i hope they continue the series
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Comment #24
(Posted by an unknown user)
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TTT is nutz!!! I love this commercial. I still laugh uncontrollably.
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Comment #25
(Posted by an unknown user)
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I think it's funny we don't get this type of think in australia.
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Comment #26
(Posted by an unknown user)
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WOOOOOOOOOOO!
When it's game time, it's pain time baby!
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Comment #27
(Posted by an unknown user)
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This is great! You should make more.
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Comment #28
(Posted by an unknown user)
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it is the funniest thing EVER
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Comment #29
(Posted by an unknown user)
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OMG this is by far the funniest thing ever, i can't belive this was an AD, i would be crying with laughter from this
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Comment #30
(Posted by an unknown user)
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LMFAOWROTF that was the funniest thing ive ever seen. We dont get this humor in australia. :)
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Comment #31
(Posted by an unknown user)
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wooooooooooooo
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Comment #32
(Posted by Poo Gas)
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Thats a long distance call Doug. Dude, this guys hilarious
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Comment #33
(Posted by an unknown user)
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Terry Tate is the man keeping the office production up. I watch TT in school everyday
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Comment #34
(Posted by an unknown user)
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I almost shit my pants damn it! This is awesomeeeee!!!!!!!!
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Comment #35
(Posted by an unknown user)
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hailrous ha ha ha ha
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Comment #36
(Posted by an unknown user)
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Triple T baby
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Comment #37
(Posted by an unknown user)
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Terry Tate rules!!!
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Comment #38
(Posted by an unknown user)
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I love it! I think we all would like to exercise a little Terry Tate once in a while.
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Comment #39
(Posted by an unknown user)
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funniest commercail ever #5 and #22 sbut up.
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Comment #40
(Posted by Niceguy)
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Your dumb shits , as if you would watch shit like that
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Comment #41
(Posted by an unknown user)
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its so fuuny
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Comment #42
(Posted by an unknown user)
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Ferking classic...
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Comment #43
(Posted by an unknown user)
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too funny
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Comment #44
(Posted by an unknown user)
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You kill the joe u make some mo i am going to be here all day bringing the pain wooooooo! these are tight as hell with bonecrushing hits
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Comment #45
(Posted by an unknown user)
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I put in for a headcount for an Office Linebacker. I wonder what it'd take to get TTT from Felcher?
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Comment #46
(Posted by an unknown user)
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good
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Comment #47
(Posted by an unknown user)
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he levels people
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Comment #48
(Posted by an unknown user)
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loves the terry tate videos
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Comment #49
(Posted by an unknown user)
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here comes the pain train baby!
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Comment #50
(Posted by an unknown user)
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it sucked
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Comment #51
(Posted by an unknown user)
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TTT bringing the pain all day every day, WOOOOOOO
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Comment #52
(Posted by an unknown user)
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the person who wrote comemnt 5 should die
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Comment #53
(Posted by an unknown user)
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*
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Comment #54
(Posted by an unknown user)
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FUkcIN EH!
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Comment #55
(Posted by an unknown user)
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terry tate should have been in that movie Office Space lol. he would have been a fine addition to initech!!
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Comment #56
(Posted by an unknown user)
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blah
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Comment #57
(Posted by an unknown user)
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action and pain
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Comment #58
(Posted by an unknown user)
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Perfect for my work day, I was ready to Bus' sum heads in today....
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Comment #59
(Posted by an unknown user)
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BWAHAHAHAHA!! man, that's hilarious! 5, 22, etc. If you don't like, go away :)
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Comment #60
(Posted by an unknown user)
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whoooooo
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Comment #61
(Posted by an unknown user)
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Terry Tate ROCK !!!
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Comment #62
(Posted by an unknown user)
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Terry Tate ROCK!!!
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Comment #63
(Posted by an unknown user)
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dude, this is absolutely hilarious, and anybody who disagrees should have get a ride on the PAIN TRAIN!! all you people who think this is stupid, YO' ASS MUST BE CRAZY!!!!
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Comment #64
(Posted by an unknown user)
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I'm doing Terry Tate, on some special somebodys, hehehehe
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Comment #65
(Posted by an unknown user)
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that was funny as hell
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Comment #66
(Posted by bigmomma3)
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knock him the f**k out terry well that was so funny
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Comment #67
(Posted by an unknown user)
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Funniest shows ever.Every office needs a TERRY TATE!
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Comment #68
(Posted by an unknown user)
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Very Cool. I can watch it a million times!
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Comment #69
(Posted by an unknown user)
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these are some of the funniest videos ive ever seen i need to bring terry to school
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Comment #70
(Posted by an unknown user)
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THOSE VIDEOS ROCK
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Comment #71
(Posted by an unknown user)
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this was the stupidest thing i ever saw
ever in a million years
ha
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Comment #72
(Posted by an unknown user)
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THESE AINT UR PENS RICHARD THESE PENS BELONG IN MY HOUSE YOU CAN'T COME IN MY KITCHEN AND TAKE A BOX FULL OF BALL POINT PENS!!!! YOUR ASS MUST BE CRAZY!!
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Comment #73
(Posted by Terrys Biggest Fan)
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TERRY! TERRY! TERRY! OOOOHHHH YEEEAAAHH BABY!!! WHOOOOOOOO!!!!
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Comment #74
(Posted by an unknown user)
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Effing awesome!
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Comment #75
(Posted by an unknown user)
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hes so hot! He knows his job.. oh yeah!
Ill hire him any day! Oh yeah...
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Comment #76
(Posted by an unknown user)
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this shit is the bomb
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Comment #77
(Posted by an unknown user)
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this shit is off the hook
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Comment #78
(Posted by an unknown user)
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you cant make a pass and pinch pablo's ass...
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Comment #79
(Posted by an unknown user)
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HUGE-HITS MAN!!!!! I LOVE IT!!!!!!
TAKE THAT, DOUG!!!!
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Comment #80
(Posted by an unknown user)
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TTT is so fucking money man!
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Comment #81
(Posted by uhu)
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Funny but kinda stupid - we got it from slap a co-worker day email tha was goig around. You can probably find it by typing in "slap a co worker day" into google.
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Comment #82
(Posted by POOP)
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THIS SHIT IS DOPE, MAN TOTALLY THE SHIT!!!
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Comment #83
(Posted by an unknown user)
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U PEOPLE SHOULD GO AND SUCK A DICK
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Comment #84
(Posted by an unknown user)
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POOP
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Comment #85
(Posted by ajnov9@hotmail.com)
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THese are the funniest movies ever
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Comment #86
(Posted by Big C)
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Terry Tate is the Man
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Comment #87
(Posted by an unknown user)
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Its like motivation in a bottle...WOOOOOO!!!
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Comment #88
(Posted by an unknown user)
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THESE ARE AMAZING
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Comment #89
(Posted by an unknown user)
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i dont know why really
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Comment #90
(Posted by an unknown user)
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i thought it was really cool didnt you think it too
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Comment #91
(Posted by Kay)
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TTT is the best!!
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Comment #92
(Posted by an unknown user)
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This Is the shit! You've got to make more of these,office workers may not be able to do this but they should be aware.....a triple "T" analogy could be waiting for them!
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Comment #93
(Posted by an unknown user)
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Hey #75 "Niceguy" Maybe your thinking you want nice guy/s/! Suck my dick asshole, I happen to think this is one of the funniest clips invented and i'm rather bright! I could be mistaken,maybe you're the funniest clip invented,doush bag! Maybe you need to tippy toe your ass from this humpty bump! Whooo,shove that up your candy ass,BITCH!
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Comment #94
(Posted by an unknown user)
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Comment #95
(Posted by teen)
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teen
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(Posted by teen)
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teen
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(Posted by an unknown user)
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Comment #99
(Posted by an unknown user)
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Its funny!
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Comment #100
(Posted by olahcersss)
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Hello! Good Site! Thanks you! mczpoflzqhp
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Comment #101
(Posted by an unknown user)
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One of the Best Terry has to be in the Office Sports Hall of Fame!
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(Posted by an unknown user)
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Comment #103
(Posted by UndedelsHeafe)
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top of pageBenthic sled with manipulatorMidwater Suction Sampler w/ 12 buckets Ц RobisonаLeg 3: Submarine Canyons (April 21-30)3 Flow Injection Analysis System, 300 lbsа Gay Men Sex Webcam Pics French-fry basket scoop1 Air compressor - Johnson ~200 lbsParticipants:
top of page67-85 35.6200 124.5500 2 CTD, nets D3,Purpose:Expedition Principal Investigator:аGary GreeneD7 26.7300 147.0400 9 DIVE, nets, CTD Nude Asian Lesbian Sex 3 white collapsible pallet boxes and misc. gear - Robison ~600 lbs totalа*Note: weight does not include sea waterVibra peeper corer (if functional)/li>
Objective is to compare surface water iron and aluminum concentrations during a "dust" season to those of a "non-dust" season (the transit to Hawaii). Underway mapping of surface water Iron and Aluminum with tow-fish pneumatic pumping system. Rosette/CTD casts at 8 stations of approximately 2 hrs each to collect metal, nutrient and chlorophyll samples to augment surface mapping findings.Ken Johnson (male), Ginger Elrod (female), Steve Fitzwater (male), Hans Jannasch (male, tentative) and Josh Plant (male, tentative)Expedition Chief Scientist: Bruce RobisonGLORIA mapping around the Hawaiian Islands identified numerous cones and high-backscatter lava flows on the seafloor in four areas: 1) north of Oahu (the North Arch lavas described by Clague et al., 1990; Dixon et al., 1997; and Frey et al., 2000 and mapped by GLORIA and SeaBeam 2100 collected by Clague on a JAMSTEC cruise in 1999), 2) west of Oahu (mapped by GLORIA imagery and transit SeaBeam lines), 3) on the southeast flank of Kauai (mapped by Simrad EM300 by U.S. Geological Survey), and particularly 4) west of Niihau Island (mapped by Simrad EM300 by MBARI). The Simrad mapping of the region northwest of Niihau in 1998 revealed that the cones are large flat-topped cones with steep sides (Clague et al., 2000) despite their inferred alkalic compositions which contrast with the tholeiitic basalt compositions of similar cones along the rift zones. These cones are scattered over the seafloor from about 1500 to >5000 m depth and provide an unparalleled opportunity to understand degassing of magmas erupted at different depths or confining pressures. These cones have been interpreted to belong to the rejuvenated stage of volcanism and to correlate with the Kiekie Volcanics on Niihau (Clague, unpub. data), the Koloa Volcanics on Kauai (Clague and Dalrymple, 1988), the Honolulu Volcanics on Oahu (Clague and Frey, 1982), and the Kalaupapa Basalt on Molokai (Clague et al., 1982). They should retain significant volatile components, particularly those erupted at the greatest depths. The combination of quenched, relatively-primitive glasses and fresh lava interiors makes such samples ideal to evaluate the spatial distribution of the different mantle source components that melt to produce Hawaiian magmas. In particular, these submarine lavas allow us to include volatile components in our analysis of plume components since the quenched glasses will retain much of their initial complement of water, carbon dioxide, sulfur and rare gases. We have arranged for state-of-the-art volatile analyses of these samples with collaborators Hanyu (rare-gases) and Dixon (water and carbon dioxide). We will determine the degassing history of these lavas as done for Kilauea and North Arch lavas (Dixon et al., 1991, 1997). The rejuvenated stage lavas from the North Arch and those from the main islands are derived mainly from a depleted lithospheric source, but one that has been modified by addition of a component from the Hawaiian plume (Frey et al., 2000; Dixon and Clague, 2000). We hope to define this component and its distribution in space and time. These cones and flows are fairly large and it is unlikely we will be able to sample more than 2 or 3 vents on a single dive, hence our request for so many dives for this important objective.Expedition Chief Scientist: David Clague Anal Sex Picture Gallery Gay 1 bongo frame and net and lead - Chavez ~200 lbsFrench-fry basket scoopThe rift is also surmounted by a series of three extensive coral terraces at 1150, 400 and 150-m depths. These coral terraces correlate with dated terraces at similar depths on the west side of the island that are 15, 125, and 425 thousand years old (summary in Moore and Clague, 1992). Several additional terraces between the 125 and 425 ka terraces present on the west side of the island are missing here. The terraces drowned during sea level fluctuations when sea level rose faster than the reefs could grow at the onset of interglacial periods during the Pleistocene. Confirming that the reefs are indeed correlated correctly with those from the west side of the island is critical to determining the subsidence of the island and whether Hawaii has tipped significantly. In addition, a small reef terrace at about 380-m depth is evident in the bathymetry, but is never modelled, suggesting that the sea level variation curves for the Pleistocene-the best record of long-term climatic change-have smoothed out some real sea level fluctuations. Collection and dating of samples from this reef would allow us to determine when this sea level fluctuation took place.
Submarine jack hammer (if available)67-60 36.4530 122.7730 2 nets, CTDExpedition Principal Investigator:аDavid ClagueD7 26.7300 147.0400 9 DIVE, nets, CTDPush cores, 12-24 per diveа Interracial Gay Man Sex M1 36.7550 122.0250 2 nets, CTD2 steel tow fish (1 as back up) + pump+block - Johnson. ~350 lbsаTRACE METAL: Ginger Elrod (female), and Steve Fitzwater
Francisco Chavez's chlorophyll filtration manifold and fluorometer, 40lbsаThese deposits record the explosive eruptive history of Loihi Seamount for many thousands of years, perhaps as long as 25 ka and thus provide an opportunity to evaluate the frequency and style of such explosive activity on a submarine volcano at relatively shallow depths. The 11-m section we have located has been sampled with two 25 cm pushcores and half a dozen sediment scoops that demonstrate that most of the Hawaiian-style eruptions are alkalic basalt in composition. To decipher the type of eruptions that form the different layers, it is important to be able to sample the layers without contamination as one important criterion to distinguish the different types of activity is the homogeneity or heterogeneity of the glass fragments in a single layer. The sediment scoop samples are always contaminated with surficial material that mantles the slope. In addition, to determine the timing of these deposits, we need to recover enough foraminifera tests to date using 14C techniques. The recovered samples contain some foraminifers, but we did not encounter any layers with enough for dating. Hopefully, a more complete section will recover some layers with abundant foraminifers accumulated during eruptive hiatuses from which we can obtain ages. Additionally, samples of ash from several other locations on Loihi contain fragments of glass from explosive eruptions on Kilauea Volcano. None of these fragments were found in the samples from the thick section, although they are almost certainly present. The compositions of glasses from all the large explosive eruptions on Kilauea during the past 50 ka are well-documented and well-dated (Clague et al., 1995, and in preparation) and may provide additional age control on the Loihi section.D9 21.4900 158.4100 7 DIVE - no net, CTDD4 33.1300 130.59 9 DIVE, nets, CTD3 Flow Injection Analysis System, 300 lbsа Have Lesbian Sex Teen Equipment Description (include weight if available):D4 33.1300 130.59 9 DIVE, nets, CTDPurpose:
Participants:Benthic sled with manipulatorScheduled Start Date: 2001-04-01 0800 Local Moss Landing timeSta. Name Latitude (deg N) Longitude (deg W) Hrs on Station Purposevibra-peeper coring systemа Anal Sex Tips Tricks The submarine east rift zone on Haleakala extends about 135 km from the present shoreline. The shallower half of the rift is characterized by a smooth surface and numerous shoreline terraces, indicating that the region has subsided at least 2200 m and tipped towards the younger Hawaii Island to the south (Moore et al., 1990). Dredging the largest of these submerged terraces recovered corals that proved too old to reliably date using U-series analyses, suggesting that this prominent terrace is older (>500 thousand years) than the oldest terrace found around Hawaii. This once-subaerial surface is disrupted by a cluster of about 20 steep-sided cones (all shallower than about 1 km depth)-only one of which has been sampled. These cones are structurally distinct from subaerial cinder cones (they have no summit craters) and hence are thought to have formed below sea level. Below the deepest shoreline feature, the submarine rift zone resembles the rift zones of Kilauea, Mahukona, and Hilo Ridge with numerous flat-topped volcanic cones (Clague et al., 2000) and linear pillow ridges. In addition, two perched lava ponds were discovered in the Simrad dataset (Clague et al., 2000). These ponds, each several km across, formed above submarine eruptive fissures, built lava levees, and then drained (either back down the eruptive vent or out the side of the pond). Such features indicate that submarine eruptions can be voluminous enough to maintain lava ponds on the seafloor. Exploration of one of these features should confirm our morphologic analysis and provide information about the chemistry, eruptive temperature, and rheology of the lava that built such features.Box corer1. Loihi Seamount
Francisco Chavez's chlorophyll filtration manifold and fluorometer, 40lbsаThe following sections outline specific targets for dives with Tiburon in Hawaii, all tied to the large themes outlined in the general project proposal. Manned submersibles have done considerable work around Hawaii, most notably the Hawaii Underseas Research LaboratorieТs (HURL) Pisces V submersible and the programs run by JAMSTEC using the R/V Karei and ROV Kaiko in 1998 and the R/V Yokosuka and 6500-m submersible Shinkai in 1999. The Kaiko and Shinkai programs focussed largely on deep targets related to giant landslides (Nuuanu and Hilina slides on Oahu and Kilauea, respectively) and on deep (>4 km depth) hydrothermal discharge from Loihi. The Pisces V is limited to operations in <2000 m and has focused its operations for much of the past 14 years on Loihi Seamount. Recent changes in the scientific objectives of the NOAA- NURP programs have shifted HURLТs program almost entirely into fisheries-related work and bioproducts research (bacteria studies on Loihi)-geologic studies like those proposed here are no longer within the scope of HURL and therefore the Pisces V submersible is no longer a viable option for future work in Hawaii.Purpose:Most of the objectives and targets outlined below are either too deep for Pisces to operate or use special ROV tools (e,g,, rockdrill, vibracorer, impact glass sampler, box corer) that MBARI has developed. A few dives in <2 km of water will be utilized to locate specific targets for more special operations (e.g., use of the vibracorer or rockdrill) and a few others will capitalize on our ability to do back-to-back dives on multiple shallow targets during a single dive day, unlike manned submersibles which can do only a single launch and recovery each day. The long duration of ROV dives in comparison to manned submersible dives, coupled with use of the impact glass sampler also allows us to complete long traverses while collecting many more samples than could be recovered by manned submersibles. Each target has multiple objectives with observations of volcanic landforms coupled with geochemical studies of recovered samples that will address important questions about the geometry of the components that make up the Hawiian plume and degassing of magmas of different compositions. Dives along drowned coral reefs will also be used to collect volcanic samples providing samples to address questions related to geologic historical reconstructions and petrology of the lavas, in addition to subsidence and climate change.We request 1 short (6-hr) Tiburon dive to map and sample the deepest (and least degassed) of the volcanic cones of the Honolulu Volcanics. This cone is structurally simple and the summit is at a depth of only about 800 m, so the dive to explore the summit and collect the lava flows and hyaloclastite can be short. Collection of submarine-erupted lavas allows for analysis of rare gas and volatile components in the quenched glasses, as well as better whole-rock trace element analyses since the submarine lavas are far less altered than those exposed to subaerial weathering (rainfall leaches many components from the subaerial lavas after their emplacement), as outlined under the "Submarine Cones and flows" section of this proposal. What Does Male Anal Sex Feel like 67-70 36.1200 123.4850 2 nets, CTDLeg 4: Lava flows (May 9-18)We request 9 12-hr Tiburon dives to sample and observe the structures of cones from between Kauai and Oahu, on the south flank of Kauai, and from a range of depths on NiihauТs northwest flank. The dives are designed to observe the range of volcanic landforms identified in the Simrad data in order to understand their formation, and to collect samples from as wide an area and as great a depth range as possible. Most of these dives are in water too deep for Pisces V operations, but several, selected to provide more complete spatial coverage, are <2,000 m deep. The ability of the ROV to cover more ground (up to 4 km at 3,500 m depth) than can be done during a typical Pisces dives (usually <1.5 km) makes the ROV the ideal vehicle to examine these large features. In shallower water, traverses can be even longer, or two dives may be accomplished in a single work day. The plan is to steam west from Honolulu about 4 hrs and dive in the channel between Oahu and Kauai, then to go to the south flank of Kauai (another 4 hr steam), and then on to NiihauТs west flank (another roughly 4-hr steam), then reverse the steps so that no transits monger than about 4 hrs are required. These samples will form the basis of a study of the geochemistry of rejuvenated stage lavas erupted near the center of the plume trace and should serve to define source region mixing near the margins of the Hawaiian plume.
Scoop bags, 12Plastic storage shed, 6x6x3 ft, w/ table - Chavez ~200 lbsа3. Puna RidgeLeg 2: Karst and Volcanos (April 1-16)67-55 36.6200 122.4150 0 no stop D1, Free Teen Lesbian Sex Video The northeast flank of Oahu shares many characteristics with the north slope of Molokai. The outer part of an terrace is punctuated by a large volcanic cone, most probably related to the rejuvenated stage Honolulu Volcanics on Oahu (Clague and Frey, 1982). This area was mapped with the Simrad EM300 system by the U.S. Geological Survey in 1998, just before the MBARI surveys were collected. The objectives in sampling this cone are similar to those outlined in the section on "Submarine cones and flows" and it is singled out here simply because it is located in a different region.Expedition Chief Scientist: David ClagueDepart Honolulu and transit 7 nm to dive 4/1A site just offshore Diamond Head, dive in 400 m water on two adjacent volcanic cones (track about 1.3 km long). Transit 3.6 nm south-southeast to dive 4/1B just off Koko Head, dive in 500 m water along chain of 3 volcanic cones (track about 1.6 nm). Transit overnight 115 nm to dive 4/2 site on Mahukona Volcano, dive in 1180-1240-960 m of water. Night operations wil consist of gravity coring within 15 nm of dive site. Dives 4/3A and 4/3B will be two half day dives within 5 nm of each other on the -400 m reef to explore karst topography. Night operations will consist of gravity coring and a 45 nm transit to dive site 4/4 on Haleakala Volcano to the north-northeast. Dive 4/4 wil be a long shallow dive designed to sample and observe volcanic structures on 5-6 pointed cones at 990 to 325 m depth. Night operations will consist of using the rock crusher within about 12 nm of the end of the dive to sample additional shallow cones and a 50 nm east-southeast transit to dive 4/5 site on Haleakala. Dive 4/5 at 2975 to 2650 m depth will sample and observe the structure of a lava pond and several vents along the rift zone of Haleakala Volcano. Night operations will consist of gravity coring following a 44 nm transit to Hilo Ridge. Dive 4/6 will start at 1460 m depth and rise up the face of the -1150 m reef, collect some volcanic cones on top of the reef and then proceed up the face and across the reef flat of the -400 m reef, ending at about 365 m depth. Night operations will consist of a 28 nm transit to Puna Ridge followed by using the rock crusher. Dive 4/7 will map and collect lava and volcaniclastic sediments in the area where some extremely high-temperature lavas erupted at about 2100 m depth, searching for the source vent. Night operations will consist of using the rock crusher in an area about 10 nm to the east and then returning to the same area where dive 4/7 was done for dive 4/8. Night operations following dive 4/8 to consist of using the rock crusher and then a 54 nm transit to Papa'u Seamount for dive 4/9. Dive 4/9 on the southwest flank of Papa'u will start at xx m depth and sample the volcaniclastic rocks exposed in the marginal fault bounding the Hilina Slump. Night operations will consist of a 13 nm transit to Loihi Seamount's summit and gravity coring prior to dive 4/10, which will be used to sample an 11-m thick section of volcanic ash on the eastern margin of the summit platform at about 1100 m depth. Night operations will consist of gravity coring within about 15 nm of dive 4/10 site. Dive 4/11 will be Geoff Wheat's and Hans Jannasch's dive to collect osmosamplers from the southern pit crater on Loihi Seamount's summit. The dive will also measure temperatures of vents, collect discrete water samples, push cores or vibra-peeper cores, and samples of barite/sulfide hydrothermal chimneys. Night operations will again consist of gravity coring followed by an 8-10 nm transit back to Papa'u Seamount where dive 4/12 will take place on the southern margin of the seamount. Night operations will consist of a 42 nm transit followed by rock crusher on Puna Ridge. Dive 4/13 will be along the shallow submarine Puna rift zone of Kilauea Volcano starting at about 710 m depth and ending at about 410 m depth. This dive will explore and sample a variety of volcanic landforms including a large flat-topped cone, a cone with summit crater, a spatter rampart, and several low-relief, smooth cones. Night operations will consist of rock crusher on Puna Ridge followed by a roughly 16 nm transit back to Hilo Ridge for dive 4/14. Dive 4/14 will start on a pointed volcanic cone on Hilo Ridge at a depth of 1670 m and traverse up the reef face of first the -400-m reef and then the -150-m reef, ending in about 120 m of water. Night operations will consist of an 89 nm transit back to Mahukona Volcano for dive 4/15. Dive 4/15 will start at about 1335 m depth and end at about 1310 m depth, exploring several varieties of volcanic cones and spatter ramparts as well as the deepest and oldest drowned coral reef on Mahukona Volcano. Night operations will consist of a 114 nm transit to the northeast side of Oahu. Dive 4/16 is a short dive on a volcanic cone between about 950 and 650 m depth. The dive will end in time to transit 31 nm to Honolulu for arrival by 5 pm.
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