THE NEW SHARKS A EVOLUTIONARY PERSPECTIVE FOR THE NEXT THOUSAND YEARS - WITH THE INCREASING OF THE CHINESE SHARK SOUP THE REMAINING SHARKS IN THOUSAND YEARS SHOULD BE VERY SMALL IT'S A ADAPTATIVE WAY OF LIFE BLUE WHALE 600 THOUSAND IN THE XIX CENTURY 100 THOUSAND IN 1930 AND 10 THOUSAND IN 1972 YES WE CAN , YES WE CAN

GREY WHALE PACIFIC RACE 

100 THOUSAND XIX CENTURY 1930 RARE

ATLANTIC 100 THOUSAND EXTINCT 1930

SPERM WHALE 1,200,000 (600,000 -1930)

1972 ----150,000 TO 200,000

SEI WHALE 400,000 .....60,000 IN THE 70'S 

THE FREEZING YEARS IN HOT COLD TIMES ARE AS FAR AWAY THAN THE COLD WAR FROM NOW AND FOREVER - AS FAR AS PROTECTION FOR COLD SPELLS AND BURNING HELLS OF AUSTRALIAN PURE FLAME

WORDS OF TIMES TO COME


AND THEY COME FASTER 


THAN YOU THINK


AND YOU CAN'T RUN FROM IT  


The recent HOT OR cold snap 


has threatened 


the FOOD cropS. 


The first expression presumably likens snap 


in the sense of “a sudden bite or cut”


 to sudden unexpected cold.

THE SHARK SURGE - NINE ELEVEN SHADOWS OF GRAY WITH A STUDY IN RED - Vorwärts MARCHING Morons Vorwärts! Musterbrief deutsch Anfrage in the IS by Osiris , IS THE IS a state like the US of A and other states made by Terrorists of the foreign descent? Vive la France les anglais out of America DON'T LIVE ON FEAR OF IS ,LIVE ON FEAR OF US OF A, MEGABUCK'S RULE THE SHARK WORLD SPEND SOME MEGABUCK'S NOW

GIVING WEAPONS FOR FREE IS MORE THAN A FELONY IT'S A SIN

READ YOUR WALT DISNEY BIBLE 

AND FOR THE GREATER GOOD

OBEY TO THE SACRED RULES 

OF OUR FORD

YOU CAN YES YOU CAN 

HAVE A MILLION OF BUCKS

BUT ONLY IN ZOMBIE BLACK OPS

BUY FORDS BY OUR FORDSAKE

DON'T BUY MAZDAS 

OR MERCEDES BENZ

BE A GOOD BLOKE 

DON'T BE A ASS AUSSIE

BUY AMERICAN PLEASE

DON'T GO CHINESE ON US OF A 

BUY AMERICAN YES WE CAN GOODS

DEFEAT ISIS 

ISLAMIC STATE IS ONLY A STATE 

OF MIND 

DON'T FEAR IS FEAR US ....

OR WE FIRE ON .....

THE TOHU BOHU SHARKS - AND THE WATERS TURN RED IN THE TOHU WA BOHU .....A EUROPA ALBERGA E GERA AS NINHADAS DO TOHU BOHU QUE a ditadura produz os fanáticos E OS FANÁTICOS DERRUBAM TODAS AS DITADURAS POR AMOR À SUA NOÇÃO DE DEMOCRACIA ENTRE IRMÃOS CRENTES E OS IRMÃOS NA FÉ DO VERO FANUM os fanáticos geram o terror ENTRE OS INFIÉIS ...A DEMOCRACIA ALBERGA E CRIA NINHOS DOS FANÁTICOS GERADOS PELAS DITADURAS E TAL COMO A SUIÇA ALBERGOU LENINE QUE DISSE FIAT LUX O HOMEM NOVO NASCEU וְהָאָ֗רֶץ הָיְתָ֥ה תֹ֙הוּ֙ וָבֹ֔הוּ וְחֹ֖שֶׁךְ עַל־פְּנֵ֣י תְהֹ֑ום וְר֣וּחַ אֱלֹהִ֔ים מְרַחֶ֖פֶת עַל־פְּנֵ֥י הַמָּֽיִם

E A DEMOGRAFIA DA MISÉRIA E DO MEDO


GERA O CHAOS 

SEM FORMA ....O VAZIO .....O TOHU BOHU 


Now the earth was formless and empty, 


darkness was over the surface of the deep, 



and the Spirit of THE GodSHARK 


was hovering over the waters.


AND THE WATERS ARE FULL OF SHARKS

COMO CONSTRUIR UM CONDENSADOR DE ÁGUA DOCE SEM FAZER MUITA FORÇA SE NÃO TIVER VIDRO OU PLÁTICO PARA CONSTRUIR UMA ESTUFA NÃO FAZ MAL É SÓ ARRANJAR PEDRAS DESDE QUE NÃO SEJA ARENITO OU OUTRA ROCHA SEDIMENTAR ÁVIDA DE ÁGUA O PROCESSO FUNCIONA E FUNCIONA HÁ MAIS DE 2000 ANOS - OS PRIMEIROS CONDENSADORES SOLARES ENCONTRADOS SÃO GREGOS DAS COLÓNIAS NA SECA CRIMEIA FAZIAM MONTES DE PEDRAS EXPOSTAS AO SOL QUE AQUECIAM DURANTE O DEMÓNIO DO MEIO-DIA E ARREFECIAM E ESCORRIAM ÁGUA DE NOITINHA CENTOS DE TONELADAS DE PEDRAS QUE DURANTE O ESFRIAMENTO NOCTURNO FALHAVAM O EQUILÍBRIO TÉRMICO COM O AMBIENTE DO SOL NASCENTE E ASSIS PROVOCAVAM A CONDENSAÇÃO DA HUMIDADE ATMOSFÉRICA E ERAM COLONOS GREGOS QUE NEM SABIAM A DIFERENÇA ENTRE UM IOTA E UM IDIOTES .. NUMA ESTUFA O AR SATURA-SE DE VAPOR QUANDO ENTRA EM CONTACTO COM O VIDRO OU COM O PLÁSTICO PORQUE ACONTECE ISSO? O VIDRO OU O PLÁSTICO FUNCIONAM COMO INTERFACES TÉRMICAS PORQUÊ? É TODA UMA CIÊNCIA DE EXPERIMENTADORES SEM DIPLOMAS NEM GRAUS DE PHilo doctoris

E SE SÓ HOUVER ÁGUA SALGADA 

OU MUITO INQUINADA DE INUNDAÇÕES

SUCESSIVAS É SÓ DESTILAR

E EM BREVE VAI HAVER MUITA GENTE

COM NECESSIDADES DESTILATÓRIAS

PODE É DEMORAR UMAS DÉCADAS

EM BREVE EM TERMOS GEOLÓGICOS

DEMORA MUITO A CHEGAR 

OU SE CALHAR NON 

GLASS BOWL DISTILLER

1. 
   1
   Fill a 5-gallon (18.927 L) 
2. stainless steel pot about halfway full
3. 
   
4. 
   2
   Place a glass bowl in the water. Be sure it floats. The bowl should not touch the bottom of the pot.
   

   • If the bowl doesn't float, remove it from the water and set a round baking rack on the bottom of the pot. Then place the bowl back in the water
5. 
   3
   Watch the water collecting in the bowl. This water should be hot but should not boil. If the water begins to boil, turn down the heat on the stove.
6. 
   4
   Create a condensation effect with a hot/cold barrier. You can do this by inverting the pot's lid and filling it with ice. When hot steam hits the cold lid, it will create condensation.
7. 
   

   
   

   
   
   Edit step
   5
   Boil the water in your pot. As the water continues to boil, it will cause steam to rise and condense on the pot's lid. The condensation will drip into the bowl. Allow the distillation process to continue until you have enough distilled water in the bowl for your needs.

DAS INFEÇÕES POLÍTICAS TERMINAIS NO IMPÉRIO AMERICANO E NAS SUAS COLÓNIAS GREGAS E ROMANAS ....A POLÍTICA COMO INFECÇÃO AGUDA E COMO MANIFESTAÇÃO CRÓNICA DO ESTADO DEPAUPERADO DO NAZIONAL-PORREIRISMO PORREIRO PÁ.....É GERALMENTE A CARGA BACTERIANA INICIAL CONSTITUIDA POR GERMES POLÍTICOS VÁRIOS E A PRESENÇA OU A AUSÊNCIA DE ORGANISMOS ORÇAMENTORESISTENTES QUE DETERMINA O TRATAMENTO MACROECONÓMICO A UTILIZAR PARA OBTER UMA CULTURA PURA E EXTERMINAR TODAS AS RESTANTES COLÓNIAS POLÍTICAS ,,,HÁ VÁRIAS TÉCNICAS E VÁRIOS TÉCNICOS-PALHAÇOS TAMBÉM DENOMINADOS ESPECIALISTAS DE ALDRABABUGEM....TÉCNICAS COM O PATROCÍNIO E SELO DE APROVAÇÃO DA FOX NEWS 1)ELIMINAM-SE OS MICROORGANISMOS PARTIDÁRIOS DE COR MALFAZEJA OU MALFADADA ATRAVÉS DA SÁTIRA POLÍTICA OU DO PUNHAL DE BRUTUS CHAMA-SE A ESTA TÉCNICA LIMPEZA OU LAVAGEM E O TÉCNICO PALHAÇO OU MESMO O PALHAÇO-TÉCNICO DEVE EVITAR USAR ÁGUA PARA FAZER TAIS LAVAGENS POIS CONTAMINA O SUBSTRACTO ONDE NADAM OS GERMES POLÍTICOS E DEVE UTILIZAR PAPEL COMERCIAL OU NÃO MAS NUNCA PAPEL FORA DE PRAZO OU DO GRUPO GES ,,,PAPEL-MOEDA TAMBÉM DENOMINADO FOTOCÓPIAS OU LIVROS DO DUDA SÃO BEM ACEITES NESTAS TÉCNICAS DE LIMPEZA A SECO OU DE LAVAGEM A SÓLIDO

FILTRAÇÃO ,,É UMA TÉCNICA


 QUE DEPENDE DO CONTROLO 

ABSOLUTO OU QUASE 

DOS FLUXOS LÍQUIDOS E BRUTOS


 DE INFORMAÇÃO E DE INFORMA MAÇÃO

 ,,,FAZENDO PASSAR A INFORMAÇÃO 

POR UMA PLACA FILTRADORA


 IMPERMEÁVEL À CONTAMINAÇÃO


 BACTERIANA MALÉFICA ...


A XXI CENTURY FOX 

É UM EXEMPLO NOTÁVEL 


DESSAS PLACAS

A MICROSOFT E O FACEBOOK SÃO 

OUTRAS ....

SURFING THE TECTONIC SHOCKWAVE -THE NAZCA AFTERSHOCK the higher see level reached in the Neogene is 15,5 Ma-old and is only 150 m above the present see level (Ha rd e nbo l et al., 1998). In our study area, in contrast, the oJder abrasion surface is higher th an 500 m asl, evidencing the uplift of that part of the Chilean coast. The observed uplift cannot result from the subduction of the Juan Fernandez ridge since the north of the study area, far from the ridge, is more uplifted than the southern part. Moreover, we most1y observe N-$ striking normal faults, whereas the subduction of the Juan Fernandez ridge should be result in the formation of E- W faults in this part of the ChiJean coast. We also note that abrasion surfaces are also present in other parts of the Chilean coast, such as in the Mejillones Peninsula (about 23° 15' S), where 400 m-high Quaternary surfaces have been described (Ort1ieb et al., 1996a). This shows that the subduction plane geometry is not responsible for the coastal uplift since the Mejillones Peninsula is located above an inclined subduction segment, contrary to our study area. We observe that the region studied here is situated at a particularly small distancefrom the trench and that this distance is smaUer in the northern part of our study area. In fact, the trench closest area is also the most uplifted. The same phenomenon is observed by Ortlieb et al (1996a) for the Mejillones Peninsula. Thus, we argue that the phenomenon that could explain the tectonics affecting the Chilean coast is the underplating beJow the Coastal Cordillera ----long-term uplift is positively correlated with the coseismic uplift, i.e. that the post seismic and interseismic subsidence of the coast does not completely compensate the uplift that occurs during earthquakes. The coseismic uplift being larger when the coast approaches the trench Neogene tectonic and geomorphologic evolution of the chilean coast between 30°S and 32°S : study of marine abrasion surfaces above a fiat subduction segment that could result from the subduction of the Juan Fernandez ridge at around 33°S since 10 My (Yafiez et al, 2001). Along that part of the coastal zone, we observe discontinuous, parai leI to the coast, gently seaward-sloping marine abrasion surfaces. They are lirnited by a scarp both their base and their top. In the following, we characterise these surfaces by the altitude of their upper internaI Iimit, at the foot of the top scarp, called shoreline angle (Fig.l) ; we recognize up to four surface levels corresponding to terraces reaching more than 500 m of elevation (above present-day MSL): To, Tl'T2 ,T3 ; T, being the younger and T3 the older surface. According to their geographical location, their width is more or less important and their characteristic elevation varies (Fig.2-3). COASTALMORPHOLOGY Distribution ofmarine abrasion surfaces: Tois the less-developed abrasion surface. It corresponds to the active abrasion surface which is still submitted to marine action in its lower part; it contains relicts of the previous surface which are not completely levelled yet.

THE TECTONICS OF NOT YET ....

Salvador Sóares Das Silvas PREFIRA O ARAMAICO QUE HÁ EM SI ....BEMOL...THE MEDICAL FAULTS faults cutting sediment or displacing abrasion surfaces correspond to normal faults striking more or less parallel to the coast (between about N340° and N400), with a vertical slip, without any strike-slip component (Fig.2). These faults do not influence markedly the morphology of surfaces; they just influence their width and elevation. Ali the faults dori'tmove the different surfaces of the same amount of displacement. Within a same surface, the vertical movement of a fault can also vary; for instance, from 9 m (Punta Limari Sur) to 54 m (Punta Limari Norte) for T2. More generally, on the one hand,we observe that the T3 surface is more deformed by faults than the three other surfaces: it is eut by a greater number of faults, and their vertical offset is also larger; and on the other hand, we observe that the northwestern part of the study area (Altos e Talinay) is more deformed than the southern (CaletaManso-Los Vilos) and the eastern (Bahia Tongoy )zones (Fig.2). N-S variations of marine abrasion surfaces elevation: in the north, at Altos de Talinay ; we note the four surfaces whereas in the south, at Caleta Derumbe for instance, only the T3 surface is visible (Fig.2-3). South 30°58', the T, surface disappears; the T3 surface becomes wider and its shoreline angle elevation decreases from north to south (Fig.2-3). Generally, we notice that surface elevations are smaller in the south than in the north (Fig.3). This shows that the northern part of the study area was further uplifted than its southern part.

number

of

faults,

and

their

vertical

offset

is also

larger;

and on the

other

hand, we

observe

that the

northwestern

part

of

the

study

area

(Altos