Scare

1.15 misc draft 

where birds

fouled my head 

chasing vultures that 

do peck at my half living 

corpse schroedinger my other 

half genetically modified we crawl 

together palm to bloodied palm  the slow

movements of the mangled ... kissing the gash

in my arm ... burned mouths that mumble 

deformed syllabubs um pain hurts hard

I push the button now bound and 

gagged to the world for real

the chains forcing me to 

love my favourite 

tree 

beholden to Lala land 

1.20am 16.02.13. © Lizarikk, All Rights Reserved



no worries



nobody does that to me ... 

make my day 
the day is singing 
why can't you hear ... 

Im in between money thoughts 

slowwwww 

I don't care you got status you got history 
you got this people and that can do this 
an I know a geezer over here 
you aint doin it orlright ... 

faker ...

Never fight fairly if you're at a disadvantage because of his size
Deliver a headbutt to the face, the Masseter muscle, the jaw area, 
is the strongest muscle in the human body. However, be aware 
that your adversary's blood may be infected  
Stomping the toes can discontinue a bear hug. Or you can 
simply twist back your foe's finger joints to break his hold

Slipping, bobbing and weaving before a snappy strike is a very essential and effective skill to develop. Being the smaller guy, you're more likely faster than him

Take advantage of your lightness

Volume punching , accumulation factor favors small fighters. 
Train with a speed bag to develop rapid striking

Feint. 

Throw a fake strike followed up by a real strike. Throw a fake left punch to the head. Then strike him with a real right punch in the solar plexus

if I were on the ground Id roll my back throw my legs up 
and attempt to crocodile kick back from there 

Even worse…you can expect something to come crashing on your head…
to be followed immediately by a half dozen rubber soles coming toward your head like a freight train

Unless you're trying to subdue drunk Uncle Charlie at the family picnic, your goal 
when you feel a fight going to the ground is to escape 

Roll Through The Fall

Instead, when you're in the "clinch", locked up with your attacker, 
and you feel like it's heading toward a wrestling match on the ground, 
you want to drop straight down as close to your attacker's feet as possible, while grabbing his clothing around the chest area, with your hands close together

This places their bodyweight completely off-center and their natural momentum 
will send them over your own body, making it easy to flip them 
in the same direction using your knees while twisting them

pull his hands down towards your groin 

then turn around so that your leverage allows you to break their grasp or continue the motion until you've pinned their hands under your arm. Try to flow 
with your opponent's movements

then run at the first opportunity towards public, well-lit areas

Block them with obstacles. If you can put a trashcan, car, bus, or other barrier 
between you and the attacker, all the better. Damage to "soft spots"  
may eventually incapacitate your opponent. Scratching, biting, clawing, spitting, pulling hair can also be used. You are defending yourself from a violent aggressor, not fighting in a ring with rules

Low kicks should be aimed towards the insides or back of calves or thighs  . Do not aim higher than knee or waist height because they will grab your leg. Think you are a wolf, do not think about tomorrow, do not wait for help, 
do not wait for the police

grand slam
a stamp on the leg in a ruck 
under the pump





11.02.13. 3am misc notes© /Lizarikk 





















This process of gradual build-up of strain and stress punctuated by occasional sudden earthquake failure is referred to as the elastic-rebound theory. Most of the earthquake's energy is used to power the earthquake fracture growth or is converted into heat generated by friction. Earthquakes lower the Earth's available elastic potential energy though these changes are negligible compared to the conductive flow of heat out from the Earth's deep interior


There are three main types of fault that may cause an earthquake: normal, reverse (thrust) and strike-slip. Normal and reverse faulting are examples of dip-slip, where the displacement along the fault is in the direction of dip and movement on them involves a vertical component. Reverse faults, particularly those along convergent plate boundaries are associated with the most powerful earthquakes, including almost all of those of magnitude 8 or more. Strike-slip faults, particularly continental transforms can produce major earthquakes up to about magnitude 8

This is so because the energy released in an earthquake, and thus its magnitude, is proportional to the area of the fault that ruptures and the stress drop. Therefore, the longer the length and the wider the width of the faulted area, the larger the resulting magnitude. The topmost, brittle part of the Earth’s crust, and the cool slabs of the tectonic plates that are descending down into the hot mantle, are the only parts of our planet which can store elastic energy and release it in fault ruptures. Rocks hotter than about 300 degrees Celsius flow in response to stress; they do not rupture in earthquakes

http://jupitersterrain5.blogspot.co.uk/2012/08/the-gates-14.html

Wiki 14.16, 16.08.12.