BASTAM QUATRO HOMENS BONS PARA FAZER UMA SALADA NAZIONAL
E UM PERDULÁRIO PARA BOTAR AZEITE NELA
UM FILÓSOFO PARA TEMPERAR A SALADA POLÍTICA
E UM MISERÁVEL PRA BOTAR O VINAGRE
SE NÃO HOUVER VINAGRE DEITAI FEL
UM OU MAIS LOUCOS PARA REMEXER A SALADA
E 1977 E SEGUINTES TRARÃO NOVAMENTE VERÕES FRIOS E BANCARROTAS
OU VERÕES QUENTES E BANCARROTAS
ENFIM PARA CORSÁRIOS DAS SALADAS
E PARA SALADAS DE BANCARROTAS
DEVEMOS TÊ-LAS ATÉ AO BICENTENÁRIO
BICENTENÁRIO DO QUÊ
ORA DA DE 1891.....
DA DE 1755 NÃO DÁ JEITO POIS SÃO LOGO DOIS BI-BI'S E INDA SOBRA
UMA CRUZ
E JÁ NUM BOU AO MERCADO DO BOLHÃO DESDE O EURRO 2002
OdgovoriIzbrišiQUE CRISE AHN ....EM ESCUDOS JÁ TINHAMOS FALIDO UMAS QUATRO VEZES
VIVA EL TANGO ARGENTINO
OdgovoriIzbrišiO PAÍS QUE MAIS SAMBOU OS CREDORES EM 200 ANOS
A CORRENTE QUENTE AFROUXOU OU ESTÁ A GOTEJAR
The latest value: 6,325,923 km2 (August 8, 2014)
E ESTE VERANO POUCO AZUR É PRA CONTINUAR?
JÁ PARECE A REPÚBLICA CHECA
The latest value: 6,169,448 km2 (August 10, 2014).....
IzbrišiThe latest value: 5,753,168 km2 (August 16, 2014
Izbriši416,000....in 6 days
200 thousand 4 days....
IzbrišiThe sedimentary record of the Late Permian and Early Triassic of the eastern Iberian Ranges shows four major, sudden, or very rapid, vertical changes in fluvial style. The Late Permian sedimentary cycle starts with the Boniches Formation, of alluvial fan-braided fluvial origin, which grades vertically over within a few metres into the Alcotas Formation, deposited by low to high sinuosity, avulsion-prone rivers with extensive floodplains. The Alcotas Formation contains calcimorphic soils, plant remains and pollen and spore assemblages. However, the upper third of the unit is devoid of all organic remains and soils and is characterized by a dominant red colour, the sandstone levels were deposited by high-sinuosity, meandering rivers. This major change took place during the Late Permian and is probably coeval with the emplacement of the Emeishan basaltic Large Igneous Province (LIP) in SE China. Rocks of the Boniches and Alcotas Formations are separated by an angular unconformity from the overlying strata, which consist of the Late Permian conglomeratic Hoz del Gallo Formation, of alluvial fan–gravel braided fluvial origin and the sandy Cañizar Formation, of low-sinuosity sandy river origin. The Permian–Triassic boundary lies, probably between the upper part of the Hoz del Gallo Formation and the first metres of the Cañizar Formation. Late Permian pollen and spore assemblages have been found in the Hoz del Gallo Formation but the Cañizar Formation is barren, with the exception of an Anisian (Middle Triassic) assemblage at the top. Tectonic extensional pulses in the Iberian Basin caused the changes observed between the lower and upper parts of the Boniches Formation, at the base of the Hoz del Gallo Formation and between the lower and upper part of this Formation. The changes observed in the uppermost part of the Alcotas Formation are not easily explained by tectonic causes, nor those in the passage from the Hoz del Gallo Formation to the Cañizar Formation. Similar sedimentary characteristics of the sandy Cañizar Formation such as amalgamated sandstone bodies, erosion and reactivation surfaces, dominant trough cross-stratification, tabular geometry, absence of plant remains and pollen and spores, and absence of silts and clays to those of coeval formations in places as far away as Australia, South Africa and Brazil suggest a global rather than local cause for these abrupt changes in fluvial style. This global cause was probably die-off of plant cover over extensive areas of the catchment, related to the end of the Permian mass extinction and possibly related to the emplacement of the West Siberian basaltic Large Igneous Province (LIP), responsible for drastic atmospheric and marine changes
OdgovoriIzbrišiLoki-Fogrufjoll
IzbrišiLoki-Fögrufjöll (also known as Hamarinn or Lokahryggur) is a subglacial volcano under the Vatnajökull glacier.
The subglacial volcano is found within the Bárðarbunga fissure system, but is independent of Bárðarbunga itself.
The last confirmed eruption was in 1910 when Tephra was erupted, but may also have had subglacial eruptions in, 1986, 1991, 2006 and 2008.
The latest value: 5,243,796 km2 (August 28, 2014)
Izbriši290 in 8....in 18 days minimum 4,700,000?
flatliner.....
Izbriši::::::::::::::::::::::
IzbrišiE SEGUNDO UM PATETA ALEGRE ATÉ FUNCIONA COM DITADURAS E DITAMOLES
OdgovoriIzbrišiMESSIAS ÀS TONELADAS N'ESTE ANO DE MIL NOVECENTOS E OITENTA E TRÊS COM TANTOS MESSIAS OU A BARCA AFUNDA OU VAMO-NOS DE VEZ OU A TRINDADE CHEGA E VEM EM PACOTES DE TRÊS....VINTÉNS E O QUE RIMA COM VINTÉNS
ZÉS-NINGUÉM'S MIGUENS? TENS OU NÃO TENS?
NÃO TENS?
MERDA TÁS LIXADO PÁ.....
SE NÃO TENS
ARRANJA-O
COMO DIZIA O OUTRO AS GARINAS GOSTAM DO MEU CABEDAL E OBVIAMENTE ADMITO-O CONSEGUE GANHAR MAIS QUE UM DEPUTADO E TEM MAIS DE PUTA DO.....QUE DEPUTADO NÉ...
É UM COMÉRCIO DA CARNE EM TEMPO DE CRISE
E JÁ VAI NO ANO VIII OU XXVIII UMA DESSAS CUM S.S.'S