D'AQUELLA EPOCHA CARACTERISADO (SADO MESMO) POR BURGAU MISTURADO
COM AREIA E SAIBRO
AREIAS ANGULARES E SUBANGULARES E GRANDES PENEDOS QUE ATTINGEM
DIMENSÕES ENORMES (1:000 METROS CÚBICOS E MAIS) ESTANDO ESTES
ELEMENTOS DISPERSOS N'UMA CAMADA DE TERRA ARGILOSA D'UMA COR
OSCILLANDO ENTRE O PARDO E O AMARELLO ESCURO
AS ROCHAS SUBJACENTES SEMPRE QUE APPARECEM APRESENTAM-SE LISAS
E MUITO POLIDAS
EBEL -THEORIA DE QUE OS ALPES ERAM UM PLANO INCLINANDO POR ONDE
OS PENEDOS ESCORREGARAM 1817
BUCH -THEORIA DAS TORRENTES DE LAMA OS GRANDES PENEDOS ERRATICOS
AGUA TORRENCIAL SIMILHANTE A TORRENTES ACTUAIS ANIMADAS D'UMA
VELOCIDADE EXTRAORDINARIA E CARREGADAS DE TANTA LAMA QUE OS
PENEDOS LEVADOS FICAVAM EM SUSPENSÃO N'ESTE LÍQUIDO DE TÃO FORTE
DENSIDADE
IMPULSÃO DADA A ESTAS CORRENTES PELO LEVANTAMENTO DAS CADEIAS
GRANÍTICAS DO MONTE BRANCO
VELOCIDADE CALCULADA 6421 METROS POR SEGUNDO
(SUPER SUPERSÓNICOS PENEDOS)
NA REALIDADE HIGH HYPER
High-hypersonic | 10.0–25.0 | 7,680–16,250 | 12,300–30,740 | 3,415–8,465 | Thermal control becomes a dominant design consideration. Structure must either be designed to operate hot, or be protected by special silicate tiles or similar. Chemically reacting flow can also cause corrosion of the vehicle's skin, with free-atomic oxygen featuring in very high-speed flows. Hypersonic designs are often forced into blunt configurations because of the aerodynamic heating rising with a reduced radius of curvature | . |
---|
1819 ESCHER DE LA LINTH -FUSÃO DOS GELEIROS
ΑπάντησηΔιαγραφή1802 PLAYFAN - A HYPOTHESE QUE O TRANSPORTE DO TERRENO ERRATICO FEITO POR ENORMES GELEIROS
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ΑπάντησηΔιαγραφήE&G / Vol. 60 /
n
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. 2–3 / 2011 / 329–365 / DO
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©
a
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thors / Creative Commons
a
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tribution
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cense
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able of content
1 Intr
oduction
2 Stratigraphic systems of the Quaternary
2.1
Chr
onostratigraphy and comparable classification
sy
stems
2.2
Biostratigraphy
2.3
Lithostratigraphy and comp
arable classification
sy
stems
3 Regional Quaternary stratigraphy of Southern Bavaria
3.1
Climate stratigraphy for Southern Bavaria
3.1.1
Bib
er (‘Biberian’)
3.1.2
D
onau (‘Danubian’)
3.1.3
Günz (‘Guenzian’)
3.1.4
Günz/Mindel (‘Guenz/Mindelian’)
3.1.5
Mindel (‘Mindelian’ sensu lato
)
3.1.6
Mindel/Riß (‘Mindel/Rissian’)
3.1.7
Riß (‘Rissian’)
3.1.8
Riß/Wür
m (‘Riss/Wuermian’)
3.1.9
Wür
m (‘Wuermian’)
3.1.10
Holo
cene
3.2
Terrace stratigraphy for Southern Bavaria
3.2.1
Ältester D
eckenschotter
(‘Oldest
Cover Gravel’)
3.2.2
Ältester Periglazialschotter
(‘Oldest Per
glacial Gravel’)
3.2.3
Höher
er Älterer Deckenschotter
(‘Higher
Older Cover Gravel’)
3.2.4
Tiefer
er Älterer Deckenschotter
(‘Lo
wer Older Cover Gravel’)
3.2.5
Jüng
erer Deckenschotter
(‘Y
ounger Cover Gravel’)
3.2.6
Ho
chterrasse (‘Higher Terrace’)
3.2.7
Üb
ergangsterrasse (‘Transitional Terrace’)
3.2.8
Nie
derterrasse (‘Lower Terrace’)
3.2.9
Spätglazialter
rasse (‘Late Glacial Terrace’)
3.2.10
Postglazialter
rasse (‘Post Glacial Terrace’)
3.2.10.1 Jüng
ere Postglazialterrasse
(‘Y
ounger Post Glacial Terrace’)
3.3 Moraine stratigraphy for Souther
n Bavaria
3.3.1
Ge
omorphological moraine classification
3.3.2
Classification b
y terminal moraine stages
4 Discussion and perspective