And so I cry sometimes when I’m lying in bed
Just to get it all out, what’s in my head
And I, I am feeling a little peculiar
And so I wake in the morning and I step outside
And I take A deep breath and I get real high
And I scream from the top of my lungs,
What’s goin’ on
And I say hey, hey, hey, hey hey
Hey, hey, hey
I said hey, what’s goin’ on
And I say hey, hey, hey, hey hey
Hey, hey, hey
I said hey, what’s goin’ on
And he tries
oh my God, do I try
I try all the time in this institution
And he prays
oh my God, do I pray
I pray every single day FOR REVOLUTION!
And I say hey, hey, hey, hey hey
Hey, hey, hey
I said hey, what’s goin’ on
Don’t cry out loud
Just keep it inside
Learn how to hide your feelings
(Hey, hey, hey, hey hey)
(Hey, hey)
HEY EY EY
I say HEY
What’s goin’ on
YEAH
If I was your mother, which I am not, I would remove all those stupid books from your room and fucking burn them all. You are being brainwashed by this unnecessary twattery. I am trying to stop myself from being “one of those” atheists, but it’s hard not to. I don’t have the time or the nature to be drawn in by religion. I enjoy not being anything, thank you.
Famous Gals in Glasses
First row: Marilyn Monroe, Ava Gardner and Brigitte Bardot.
Second row: Jayne Mansfield, Bettie Page and Lucille Ball.
Third row: Julie Newmar, Grace Kelly and Raquel Welch.
![Pāhoehoe
Pāhoehoe lava from Kīlauea volcano, Hawaii, United States
Pāhoehoe (/pəˈhoʊ.iːˈhoʊ.iː/; from Hawaiian [paːˈhoweˈhowe],[8] meaning “smooth, unbroken lava”), also spelled pahoehoe, is basaltic lava that has a smooth, billowy, undulating, or ropy surface. These surface features are due to the movement of very fluid lava under a congealing surface crust. The Hawaiian word was introduced as a technical term in geology by Clarence Dutton.[7]
A pāhoehoe flow typically advances as a series of small lobes and toes that continually break out from a cooled crust. It also forms lava tubes where the minimal heat loss maintains low viscosity. The surface texture of pāhoehoe flows varies widely, displaying all kinds of bizarre shapes often referred to as lava sculpture. With increasing distance from the source, pāhoehoe flows may change into ʻaʻā flows in response to heat loss and consequent increase in viscosity. Pahoehoe lavas typically have a temperature of 1100 to 1200 °C.
The rounded texture makes pāhoehoe a poor radar reflector, and is difficult to see from an orbiting satellite (dark on Magellan picture).](http://25.media.tumblr.com/tumblr_m77skjzqnB1r7ni69o1_500.jpg)
Pāhoehoe
Pāhoehoe (/pəˈhoʊ.iːˈhoʊ.iː/; from Hawaiian [paːˈhoweˈhowe],[8] meaning “smooth, unbroken lava”), also spelled pahoehoe, is basaltic lava that has a smooth, billowy, undulating, or ropy surface. These surface features are due to the movement of very fluid lava under a congealing surface crust. The Hawaiian word was introduced as a technical term in geology by Clarence Dutton.[7]
A pāhoehoe flow typically advances as a series of small lobes and toes that continually break out from a cooled crust. It also forms lava tubes where the minimal heat loss maintains low viscosity. The surface texture of pāhoehoe flows varies widely, displaying all kinds of bizarre shapes often referred to as lava sculpture. With increasing distance from the source, pāhoehoe flows may change into ʻaʻā flows in response to heat loss and consequent increase in viscosity. Pahoehoe lavas typically have a temperature of 1100 to 1200 °C.
The rounded texture makes pāhoehoe a poor radar reflector, and is difficult to see from an orbiting satellite (dark on Magellan picture).
