DESDE 1 DE NOVEMBRO DE 1755 ....259 ANOS DE FALHANÇOS NAS PREVISÕES DO APOCALIPSE .....GLOBAL GEOLOGIC AND HYDROLOGICAL CHANGES

Beware the power of ....
Mental note's:
never park vehicle at DUNMOVIN, CA or it may not be dunmovin. ;)

OverwhelmingSilence Holy shit. 

or in simplified views
Oh shit.

THE GLOBAL WARMING Effects


MORE WTF AGW EFFECTS

SHEETED DYKE SWARMS - LAYERED GABBROIC ROCKS - FAULT ZONES - STOCKWORKS THAT DON'T WORK AND MASSIVE SULPHIDE DEPOSITS

The most common sulfide mineral in VMS deposits is pyrite, which is often associated with other sulfides such as pyrrhotite, chalcopyrite, sphalerite, and galena (Galley and others, 2007). Other possible nonsulfide minerals associated in VMS deposits include magnetite, hematite, and cassiterite; barite can be present as a gangue mineral. All these minerals have relatively high values of specific gravity (4.0–7.5 g/cm3; table 7–2), which is in strong contrast to the significantly lower densities measured in their sedimentary or volcanic host rocks. Thomas (2003) measured densities of 2.70–2.84 g/ cm3 for the host rock at the Bathurst mining camp.
Electrical Signature
Electrical methods are highly effective in identifying VMS targets because they respond to the electrical conductivity of the rocks and minerals, which can vary by 20 orders of magnitude (Grant and West, 1965). Electrical methods are unique in being able to detect such a large range of magnitudes; no other physical property has such a wide range. Because of this large potential range in values, a variety of electrical techniques have been developed that capitalize on these differences, such as measurement of conductivity, resistivity (the inverse of conductivity), induced polarization, electromagnetism, and gamma ray spectra (table 7–1). Electrical methods are currently the most used technique in surveying for VMS deposits; a variety of survey types (for example, MegaTEM, Titan24, and borehole techniques) are pushing the limits of detectable depth ranges.
Volcanogenic massive sulfide deposits have high conductivities (fig. 7–2B) exceeding 500 mS/m (millisiemens per meter) and are similar in magnitude to graphite and saltwater (Ford and others, 2007). Compared to igneous and metamorphic rocks with typical conductivities of <1 1="" 500="" a="" also="" and="" anoxic="" are="" as="" associated="" be="" between="" body.="" body="" br="" by="" can="" complicating="" conductive="" conductivities="" conductivity="" contain="" content="" contrast="" could="" definitive="" deposits.="" deposits="" difficult="" distinguish="" distinguishable="" economic="" effectively="" electromagnetic="" exploration="" factor="" from="" fully="" graphite="" highly="" horizons="" host="" however="" in="" increase="" introduced="" its="" m="" mask="" massive="" may="" ms="" noneconomic="" not="" of="" or="" ore="" other="" overlying="" physical="" potentially="" property.="" pyrite-rich="" pyrrhotite-rich="" reducing="" rock="" rocks="" sedimentary="" sediments.="" signal="" significant="" so="" some="" substantially="" such="" sulfide="" techniques="" that="" the="" themselves.="" thus="" to="" tools="" types="" typically="" unit="" useful="" vms="" water-rich="" water="" with="">Electrical resistivity surveys are useful in calculating the apparent resistivity of the subsurface at different depths resulting in the generation of cross sections of true resistivity (Ford and others, 2007). These can be used to produce three-dimensional geometries of ore bodies at depth. Resistivity surveys also are used to estimate the thickness of overburden, which
7. Geophysical Characteristics of Volcanogenic Massive Sulfide Deposits
By Lisa A. Morgan
118 7. Geophysical Characteristics of Volcanogenic Massive Sulfide Deposits
Figure 7–1. Schematic diagram of the modern Trans-Atlantic Geothermal (TAG) sulfide deposit on the Mid-Atlantic Ridge, depicting a cross section of a volcanogenic massive sulfide deposit with concordant semi-massive to massive sulfide lens underlain by a discordant stockwork vein system and associated alteration halo. From Hannington and others (1998) and Galley and others (2007). Modified from Hannington and others (2005).
then can be used to improve interpretation of ground gravity surveys (Ford and others, 2007). Conductivity, the inverse of resistivity, also can be used to map overburden.
Induced polarization (IP) surveys measure the chargeability of the ground and the time variance in the response of the electromagnetic field, which is related to ability of the material to retain electrical charges. Induced polarization surveys are very effective in detecting disseminated sulfide bodies. Typically, these sulfides occur in the altered halo surrounding the massive sulfide ore body and may be associated with clays, which also produce significant IP responses (Ford and others, 2007).
The techniques associated with electromagnetic (EM) surveys, collected both on ground and in air, are the most common electrical methods employed in mineral exploration. Electromagnetic techniques can directly detect conductive features such as base metal deposits where significant contrasts in conductivity values occur between the ore bodies and their resistive host rocks (Thomas and others, 2000). Values for the conductivity of soils, rocks, and ore bodies, measured in milliSiemans per meter, span several orders of magnitude ranging from 3.57×109 mS/m for graphite to 5×108 mS/m for pyrrhotite to 0.01 mS/m for gravel and sand (Thomas and others, 2000). Both airborne and ground electromagnetic techniques are effective in detecting

DIA DE REFLEXÃO NA EUROPA - O APOCALIPSE RUSSO AINDA DEMORA MAIS UNS TEMPOS E O GELO NUNCA MAIS ESTALA NESTA GUERRA FRIA 2014-2018

no news are Bad News 

ONE MILE OF ICE TO MELT on Ice Melt: This Time Greenland

May 19, 2014

Illustration showing newly revealed topography of subsealevel glacial channels in Greenland, from the new Nature Geoscience paper by Morlighem, Rignot et al Note below sea level “bowl” in the interior.

Eric Rignot and his team strike again. This time Greenland.  More vulnerable to melt, more sea level rise likely.  Yadda Yadda.

The bed topography beneath the Greenland ice sheet controls the flow of ice and its discharge into the ocean. Outlet glaciers move through a set of narrow valleys whose detailed geometry is poorly known, especially along the southern coasts. As a result, the contribution of the Greenland ice sheet and its glaciers to sea-level change in the coming century is uncertain. Here, we combine sparse ice-thickness data derived from airborne radar soundings with satellite- derived high-resolution ice motion data through a mass conservation optimization scheme . We infer ice thickness and bed topography along the entire periphery of the Greenland ice sheet at an unprecedented level of spatial detail and precision. We detect widespread ice-covered valleys that extend significantly deeper below sea level and farther inland than previously thought. Our findings imply that the outlet glaciers of Greenland, and the ice sheet as a whole, are probably more vulnerable to ocean thermal forcing and peripheral thinning than inferred previously from existing numerical ice-sheet models. 

Basic issue – Greenland is essentially a ring of mountains surrounding a bowl of ice.
 Where fingers of the sea can reach in beneath the ice and get to the soft underbelly, glacial outflow can proceed really quickly.....NO BECAUSE IS SOME ISOSTATIC COMPENSATION
AND STRESS RELATED FAULTS THAT GOING ON AND OFF

New paper indicates there’s a lot more fingers than we thought, and longer.
This possibility was discussed in my video last year by the ever-prescient Dr.Mike MacCracken.

Greenland’s icy reaches are far more vulnerable to warm ocean waters from climate change than had been thought, according to new research by UC Irvine and NASA glaciologists. The work, published today in Nature Geoscience, shows previously uncharted deep valleys stretching for dozens of miles under the Greenland Ice Sheet.
The bedrock canyons sit well below sea level, meaning that as subtropical Atlantic waters hit the fronts of hundreds of glaciers,THEY GOING TO GO FROM WARM SUBTROPICAL TO 4ºC
AND SINK....AND WATER COLD AND  WITH LOW DENSITY GOING TO APPEAR IN GREAT AMOUNTS AT THE SURFACE... those edges will erode much further than had been assumed and release far greater amounts of water.

Ice melt from the subcontinent has already accelerated as warmer marine currents have migrated north, but older models predicted that once higher ground was reached in a few years, the ocean-induced melting would halt. Greenland’s frozen mass would stop shrinking, and its effect on higher sea waters would be curtailed.

“That turns out to be incorrect. The glaciers of Greenland are likely to retreat faster and farther inland than anticipated – and for much longer – according to this very different topography we’ve discovered beneath the ice,” said lead author Mathieu Morlighem, a UCI associate project scientist. “This has major implications, because the glacier melt will contribute much more to rising seas around the globe.”

To obtain the results, Morlighem developed a breakthrough method that for the first time offers a comprehensive view of Greenland’s entire periphery. It’s nearly impossible to accurately survey at ground level the subcontinent’s rugged, rocky subsurface, which descends as much as 3 miles beneath the thick ice cap.

Since the 1970s, limited ice thickness data has been collected via radar pinging of the boundary between the ice and the bedrock. Along the coastline, though, rough surface ice and pockets of water cluttered the radar sounding, so large swaths of the bed remained invisible.

Measurements of Greenland’s topography have tripled since 2009, thanks to NASA Operation IceBridge flights. But Morlighem quickly realized that while that data provided a fuller picture than had the earlier radar readings, there were still major gaps between the flight lines.

To reveal the full subterranean landscape, he designed a novel “mass conservation algorithm” that combined the previous ice thickness measurements with information on the velocity and direction of its movement and estimates of snowfall and surface melt.

The difference was spectacular. What appeared to be shallow glaciers at the very edges of Greenland are actually long, deep fingers stretching more than 100 kilometers (almost 65 miles) inland.

“We anticipate that these results will have a profound and transforming impact on computer models of ice sheet evolution in Greenland in a warming climate,” the researchers conclude.

“Operation IceBridge vastly improved our knowledge of bed topography beneath the Greenland Ice Sheet,” said co-author Eric Rignot of UC Irvine and NASA’s Jet Propulsion Laboratory. “This new study takes a quantum leap at filling the remaining, critical data gaps on the map.”

The team also reported stark new findings last week on accelerated glacial melt in West Antarctica. Together, the papers “suggest that the globe’s  sheets will contribute far more to sea level rise than current projections show,” Rignot said.

BOMB THE Large-scale fractures related to inception of the

Yellowstone hotspot AND STOP THE MELTING

Jonathan M.G. Glen

U.S. Geological Survey, 345 Middlefield Road, Menlo Park, California 94025, USA, and Berkeley

Geochronology Center, 2455 Ridge Road, Berkeley, California 94709, USA

David A. Ponce

U.S. Geological Survey, 345 Middlefield Road, Menlo Park, California 94025, USA

ABSTRACT

During middle Miocene time, western North America was subject to flood-basalt vol-

canism, dike-swarm injection, and broad-scale fracturing and folding of the crust. We

propose a simple model to account for these events and for a regional pattern of geologic

and geophysical features. Aeromagnetic maps reveal some of the most important elements

of this pattern, which are several narrow, arcuate anomalies, here referred to as the

Northern Nevada rifts. These rifts extend hundreds of kilometers across Nevada and are

likely caused by highly magnetic, middle Miocene mafic dikes. With the aid of filtering

techniques, the anomalies can be traced into Oregon. Together with other geologic fea-

tures, such as fold axes, dike swarms, and faults, they produce a spoke-like pattern fanning

over 220

of arc that converges toward a point near the Oregon-Idaho border

A possible cause for this pattern is a point source of stress at the base of the crust related

to the formation of the Yellowstone hotspot. The spoke-like pattern, however, does not

persist at large distances from the emerging hotspot; several hundred kilometers to the

south, the Northern Nevada rifts deviate significantly (From a radial trend. We show

that a simple model—imposing a point source of stress at the base of the crust and a

regional stress field aligned with the presumed middle Miocene stress direction—fits the

observed fracture pattern. It thus accounts for both the radial pattern present near the

nascent hotspot and the far-field pattern due to regional stresses.

Keywords:

Yellowstone hotspot, Northern Nevada rifts, Snake River Plain, dike swarm, flood

basalts, Columbia River Plateau.

INTRODUCTION

Among the most striking geophysical fea-

tures of western North America (Figs. 1 and

2) are long and narrow positive magnetic

anomalies (collectively referred to here as

the Northern Nevada rifts

A BIOSFERA É DESCONTÍNUA ENTRE CÃO DE FILA E VASCO DA GAMA OU ENTRE GATO-PINGADO E TRISTE TIGRE DE PAPEL SELADO NÃO HÁ ELEMENTOS DE TRANSIÇÃO

VASCO DA GAMA QUE NOS GAMOU GAMA E GAMARÁ

É COMO FLORESTA CADUCA EM GRÃOS DE SILÍCIO SEM HYDOR

OU SEJA EM AREIA DAS MAIS SECAS

É UM BIÓTOPO QUE SÓ CONVEM A CERTAS ESPÉCIES

VASQUINHOS - Quercus sessiliflora Poa memorabilis similar à Poia memorável qu'anda livre....

Lonicera perclymenum (MADRESSILVA UMA MÃE PARA RELVAS MAIS ALTAS) 
Solidago virgaurea ....

a 500 METROS UMA FLORESTA DESENVOLVE-SE EM CASCALHO HÚMIDO

É DO CARALHO O CASCALHO EMBORA ANÁLOGA À PRIMEIRA VISTA

SÓ MANTEM A Poa e a madressilva a Poia foi-se e há duas vezes mais ESPÉCIES DE RELVAS

QUE NO BIÓTOPO ANTERIOR E OS DOMINANTES 

SÃO Quercus pedunculata Fraxinus excelsior Crataegus monogyna (espinheiro-alvar)

Ulmus campestris Hedera helix hera hera ,,,,Vicia sp Viola silvestris viola viola é violeta 

a fôret en dourdain Seine et oise varia em poucos centos de metros 

CONJUNTOS FISIOLÓGICOS AUTOTRÓFICOS PRODUTORES DE ORGÂNICA MATÉRIA

HETEROTRÓFICOS OU JÃBASKISTAS PRODUTORES DE MERDA...

OS RIOS CURSOS DE ÁGUAS MÍTICAS QUE BROTAM DAS PEDRAS E SE EVAPORAM ARMAZENANDO CALOR E ENERGIA POTENCIAL GRAVÍTICA - HOJE TEMOS TÉCNICAS QUE PERMITEM CALCULAR EM CADA MOMENTO A IMPORTÂNCIA DA MASSA LÍQUIDA EM MOVIMENTO MAS AINDA NÃO COMPREENDEMOS TOTALMENTE O COMPORTAMENTO DESSES FLUXOS EM REGIME HIDRÁULICO DITO TURBULENTO NEM TEMOS DADOS SOBRE O SEU REGIME EM PERÍODOS DE ARKSTORMS QUE SE IRÃO TORNANDO PROVAVELMENTE MAIS VULGARES DEPOIS DESTE INVERNO INGLÊS DE 2013-2014

E DOS RIOS E DAS ÁGUAS QUE CAEM DO CÉU SÃO INDISPENSÁVEIS

 

PARA O SUCESSO DAS CULTURAS SÍRIAS OU AFRICANAS

 

QUE NA ESCASSEZ DE ÁGUAS RESULTAM PRIMAVERAS SÍRIAS

 

E DA ESCASSEZ DE GRÃO OU DA SUA CARESTIA

 

RESULTAM PRIMAVERAS RUSSAS

 

OU REVOLUÇÕES OUTONAIS RUSSAS PARA O CASO TANTO FAZ 1917 FOI APENAS

 

UM MOMENTO DE STRESS ALIMENTAR HÁ 96 ANOS E ALGUNS MESES

 

AO ESTUDAR UM RIO NECESSÁRIO É :

 

ANALISAR OS DIFERENTES FACTORES QUE O INFLUENCIAM

 

METEREOLÓGICOS  GEOLÓGICOS TOPOGRÁFICOS E OUTROS QUE CONDICIONEM

A SUA ALIMENTAÇÃO OU AFECTEM O TRANSPORTE 

O HOMME OU HOMO NÃO SAIU DA SUA SUBSERVIÊNCIA PERANTE OS RIOS

DEPENDE DO SEU DÉBITO CADA VEZ MAIS

PARA ABASTECER AS CIDADES E CADA VEZ MAIS SECUNDARIAMENTE OS CAMPOS

AS VARIAÇÕES ANUAIS E SAZONAIS DOS RIOS SÃO CADA VEZ MAIS IMPREVISÍVEIS

OS DÉBITOS MÁXIMOS E MÍNIMOS MEDIDOS NALGUNS CASOS HÁ MAIS DE 150 ANOS

APRESENTAM ANOMALIAS IMPORTANTES NAS ÚLTIMAS DUAS DÉCADAS

AS ESTIAGENS DO AMAZONAS ATINGIRAM NO SÉCULO XXI RECORDES ABSOLUTOS

DE QUE NÃO HÁ REGISTO EM 300 ANOS DE COLONIZAÇÃO

 

E SE PARTE DA PERDA DA ÁGUA PODE SER EXPLICADA PELA E.V.T. 

 

EVAPORAÇÃO DIRECTA 

 

E TRANSPIRAÇÃO DA MASSA VIVA AO LONGO DO SEU CURSO 

A EVAPORAÇÃO FISIOLÓGICA E A FÍSICA NÃO EXPLICAM 

O DESAPARECIMENTO DAS TOALHAS FREÁTICAS E A DIMINUIÇÃO DO PERCURSO

SUBSUPERFICIAL EM ZONAS DE ESCASSA OCUPAÇÃO HUMANA 

A HIDROGEOLOGIA NÃO EXPLICA O DESAPARECIMENTO DE MUITAS TOALHAS 

PROFUNDAS E DE OUTRAS QUE ESTANDO CAPTIVAS 

 

ENTRE ESTRATOS IMPERMEÁVEIS  SE SUMIRAM MIRACULOSAMENTE

O PODER DE EROSÃO DOS RIOS ESPECIALMENTE A EROSÃO VERTICAL

INTENSIFICA-SE EM PERÍODOS TURBULENTOS

APROFUNDA-SE O LEITO DE MUITOS RIOS 

ALARGAM-SE AS SUAS MARGENS DESTRUINDO O ALUVIÃO CEREALÍFICO

O ATAQUE ÀS BRUTAS MARGENS COM SOBRECARREGAMENTO DO CAUDAL LÍQUIDO

COM A MASSA SÓLIDA ARRASTADA ATÉ AO MAR E ASSIM O BANGLADESH DESCE

DESCE

OS VALES ALUVIAIS DIMINUEM A INTENSIDADE DA PLUVIOSIDADE AUMENTA

MAS A TEMPERATURA AMBIENTE INFLUENCIA A EVT E LOGO

 

 A EFICÁCIA DA CHUVA  QUE SE INFILTRA MENOS E IMPEDE O REABASTECIMENTO 

DOS FREÁTICOS E AFECTA A HUMIDADE RELATIVA DOS SOLOS 

 

E LOGO DA ATMOSFERA DAÍ OS GRANDES FOGOS NA ESTEPE RUSSA NESTA DÉCADA

O RITMO DAS CHEIAS E A SUBIDA DE NÍVEL DAS ÁGUAS ALTEROU-SE

SUBSTANCIALMENTE

O GUARYA NO BRASIL SUBIA NOS MÁXIMOS DE CHEIA ATÉ 40 METROS

O RENO EM COLÓNIA TEVE MÁXIMOS SOBRE O LEITO NORMAL DE 12 METROS

MAS ERAM CASOS EXCEPCIONAIS

E HOJE NÃO O SÃO MAIS

NÃO É POSSÍVEL CARACTERIZAR AS CHEIAS ACTUAIS OU AS ESTIAGENS 

COM DADOS DO PASSADO HISTÓRICO O RITMO ALTEROU-SE

DÉBITOS ABSOLUTOS DE 200 MIL METROS CÚBICOS POR SEGUNDO NO AMAZONAS

NO CONGO 70 A 75 MIL E MESMO 80 MIL 

NO MISSUS HIP OU MISSISSIPI E NO VOLGA 60 A 75 MIL EM CHEIAS EXTREMAS

REPRESENTAM DURANTE UMA CHEIA PROLONGADA

200 A 300 MIL MILHÕES DE METROS CÚBICOS DE ÁGUA

E VOLUMES DESSES INFLUENCIAM AS ESTIAGENS SUBSEQUENTES

BAIXAS DE NÍVEL DA ÁGUA ABSURDAS TÊM-SE ACUMULADO DESDE 1992

ESTIAGENS PROLONGADAS E RESERVAS FREÁTICAS BAIXAS

VÃO LIMITAR O CONSUMO E AUMENTAR O RECURSO A RESERVAS SUBTERRÂNEAS

O CASO SÍRIO É BEM PATENTE E DOCUMENTADO DESDE 1979

FRIOS INTENSOS GELARAM MUITAS DAS FONTES COM INVERNOS MAIS RIGOROSOS

E ANOS SUCESSIVOS DE FRACAS PRECIPITAÇÕES SECARAM-NAS

ESTIAGENS DEVIDO AO FRIO SÃO MAIS COMUNS HOJE QUE HÁ 20 ANOS ATRÁS

E O CAUDAL DO AMAZONAS NUNCA ANTES TINHA DESCIDO ABAIXO 

 

DOS 50 MIL METROS CÚBICOS POR SEGUNDO 

E MUITOS RIOS DE REGIMES SIMPLES DE CLIMA TROPICAL TÊM APRESENTADO 

ESTIAGENS EXTREMAS E MÁXIMOS MUITO VARIÁVEIS NA ESTAÇÃO DAS CHUVAS

OS REGIMES GLACIARES TÊM DECRESCIDO POIS NALGUNS CASOS 

A BACIA HIDROGRÁFICA DO RIO DEIXOU DE ESTAR OCUPADA EM 25 OU 35%

POR UM GLACIAR  E OS CAUDAIS MÁXIMOS NO VERÃO TENDO SIDO

MAIS INTENSOS HÁ ALGUNS ANOS COMEÇAM OU COMEÇARÃO A DECRESCER 

SENDO REGIMES CONDICIONADOS PELAS CONDIÇÕES TÉRMICAS

E SENDO OS GLACIARES FORMAS DE ACUMULAÇÃO 

 

DE PRECIPITAÇÃO MULTISECULARES SERÃO DOS MAIS AFECTADOS

E AFECTARÃO 500 MILHÕES DE ASIÁTICOS DIRECTAMENTE

QUE NÃO DEPENDEM DUM REGIME DE PRECIPITAÇÃO MAS DE FUSÃO.....

IDEM PARA OS REGIMES DE NEVES DA MONTANHA COMO O DA SERRA DA ESTRELA

E DE OUTRAS ACUMULAÇÕES INVERNAIS QUE FUNDEM NA PRIMAVERA

OS REGIMES DE NEVES DA PLANÍCIE JÁ TÊM DADO PROBLEMAS NAS PLANÍCIES 

E PLANALTOS DE TODA A ÁSIA CENTRAL

 

 E PROVAVELMENTE NA AMÉRICA DO NORTE MUITO EM BREVE

O VOLGA É O MAIS CARACTERÍSTICO DESTE REGIME E BASTAM UNS ANOS MAUS 

OU AUMENTO DO PERÍODO DE DEGELO PARA SURGIREM 

 

PROBLEMAS DE ABASTECIMENTO SE AS CHUVAS DE VERÃO INFLUÊNCIA 

SECUNDÁRIA DIMINUIREM COMO NOS ÚLTIMOS ANOS

AS RESERVAS DA NEVE EM FUSÃO CHEGAVAM ATÉ JULHO NOS ANOS 40

HOJE CHEGAM A PRINCÍPIOS DE JUNHO NO CURSO SUPERIOR DO VOLGA 

AS VARIAÇÕES INTERANUAIS PEQUENAS DURANTE UM SÉCULO

AUMENTARAM EXTRAORDINARIAMENTE EM APENAS 20 ANOS

effective mitigation is:

a fair tale

a fairy tale

none of the above

first: the albedo decreased lots

second: the permafrost release more ch4 everyday

third or thurd ? cows sacred or not make more turd's this days and they give a extra CH4 before slaughter by chinese and african's and 5 billion others

IV - or intra-ve.....the drop in global GDP if this reduction take place

of about 450 ppm in 2100?
well the killing of joe gallo don't change these emissions

you need to kill the surplus population that by 2100 are at least 9 billion people
2 billion more than now or three
if they reach 10,000,000,000

changes in soil use? said...

changes in water use?

changes in the global menu?

i don't like ratburger's von McDonald

 Abstract: August–July precipitation has been reconstructed back to AD 1724 for the Mohe region in the northern Greater Higgnan Mountains, China, using Pinus sylvestris var. mongolica tree-ring width. The reconstruction explains 39% of the variance in the precipitation observed from AD 1960–2008. Some droughts noted in historical documents are precisely captured in our reconstruction. Wet periods occurred during the periods of AD 1734–1785, AD 1805–1830, AD 1863–1880, AD 1922–1961, and AD 1983–1998; while the periods of AD 1786–1804, AD 1831–1862, AD 1881–1921, and AD 1962–1982 were relatively dry. Power spectral and wavelet analyses demonstrated the existence of significant 24-yr, 12-yr, and 2-yrcycles of variability. The results of the spatial correlations suggest that our reconstruction contains climatic signals for the southern Stanovoy Range and the northern Greater Higgnan Mountains. The positive correlations between the new reconstructed precipitation series and two precipitation reconstructions indicate that our precipitation reconstruction captures broad-scale regional climatic variations. A comparison between the weakening tendency of summer monsoon and the dry period of our reconstruction reveals that the annual precipitation in the Mohe region is partly influenced by the East Asian Summer Monsoon.

"VISCOUS CREEP" ERODE CONTINENTS IN VENUS, ROCKS HEAT AND GO SOFT AND FLOW.....IT'S LIKE THE POLITICAL CRIPS

٠‎ - ١‎ - ٢‎ - ٣‎ -٤‎ - ٥‎ - ٦‎ - ٧‎ - ٨‎ - ٩‎.........١‎٠‎  AND ٢‎  ٣‎  OR٤‎ ٥‎  ٦‎ ٧‎ - ٨ ٠‎ - ١‎ - ٢‎ - ٣‎ -٠‎ - ١‎ - ٢‎ - ٣‎ -٤‎ - ٠‎ - ١‎ - ٢‎ - ٣‎ -٤‎ - ٥‎ - ٦‎ - ٧‎ - ٨‎ - ٩‎) ٥٠‎ - ١‎ - ٢‎ - ٣‎ -٤‎ - ٥‎ - ٦‎ - ٧‎ - ٨‎ - ٠‎ - ١‎ - ٢‎ - ٣‎ -٤‎ - ٥‎ - ٦‎ - ٧‎ - ٨‎ - ٩‎) ٩‎) ‎ - ٦‎ - ٧‎ - ٨‎ - ٩‎) ٩‎) ٩‎PESSOAS)

WTF IS HFT? A GEOLOGIC PROCESS? 10 KM ACROSS CINDER CONES IN APHRODITE THE LARGEST "CONTINENT " ON VENUSIAN SWAMPLANDS?

 LEGLESS HFT'S LARGER THAN LIFE

A SWARMING ARMY OF THIEFS AND THIEF'S WITH BIG THEET?

CRESTED SKULLS OF KAISERLIKE WARRIORS DESCEND FROM MERCKELAND

THEY INSISTED THAT PIIGS ARE SOLID STOLID MIDCASTE UNTERMENSCH

A RACE OF LAZY BEINGS

HEIL THE PURPLE HEART BAND OF BROTHERS

CROWN THE DARK HEARTLINE OF LOST SOULS ACROSS THE INTERCONTINENTAL

DIVIDE

THE SLOW SOFTENING OF THE BONES IN CREMATORIA WORLD'S 
Nobody knows lots of things, could water be essential for plate tectonics? Venus is dominated by hot-spots? U.V rays broke more H2O apart or in two than in the free ozone zone in the 90's ? circular depressions concentric ridgelike rings with hundreds of miles across the CORONAS (not korunas ok) are created by a surge of magma
is a mechanism for venus to shed it's heat?
storms and arkstorms can ye they can trigger earthquakes by the word Let the earth bring forth earthquakes and quacks.....
living creatures according to their kinds—livestock and creeping things and beasts of the earth according to their kinds, this HFT is kind of....

OS NOVOS JUDEUS SÃO OS CIGANOS NÃO QUEREM IR PARA OS CAMPOS DE TRABALHO ENTÃO QUE VÃO PARA O CARALHO NA ALEMANHA TRABALHA-SE OU RALHA-SE - OSAMA BIN LADEN E MERCKEL E TAVARES QUE É RICO E TEM OURO NO PENICO - GUERREIROS DA FÉ É O QUE É VINDOS DUM PASSADO DEMOGRAFICAMENTE ULTRAPASSADO TENTAM SUSTER A MARÉ DOS SUB-HUMANOS FEITOS GADO ESTRAGADO E O OCIDENTE RESPONDE COM O CRUZADO À INVASÃO - O CRUZADO DO SANTO ÓLEO QUE DEFENDE A EUROPA DO CRIME NA CRIMEIA É MEU IRMÃO POIS ENTÃO SENÃO OS ETHNOI COMEM-NOS VIVOS OH BOY HO HO BOY

na realidade 

a alemanha 

por fatalidade

tamanha 

resolveu expulsar

quem não tem lugar

O TEU SEMBLANTE DUAL

DE CHRISTO E DE JUDAS

E NISSO ATÉ AJUDAS

É ATAVISMO MEDIEVAL

PARECES QUIÇÁ AQUI?

Ó INEXISTENTE VIRTUAL

O AYATOLLA KHOMEINI

A PREGAR A SANTA GUERRA

CONTRA A BANCA QUE ENCERRA

NO JURO O PESO DE TODO O MAL

QUE É UM BEM AFINAL

PARA QUEM O RECEBE

OU COMO CROMWELL QUE PERCEBE

QUE É EFÉMERA A VIDA TERRESTRE

NUM BUCOLISMO CAMPESTRE

CALVINO PROCLAMA QUE É ILUSÃO

A FELICIDADE TEMPORAL

E FRAGMENTA A EURO DIVISÃO

POIS DE PORRADA GOSTA AFINAL