Questões de Concurso Público CPRM 2025 para Analista em Geociências - Letras
Foram encontradas 70 questões
Q3757719
Inglês
Texto associado
READ TEXT I AND ANSWER THE QUESTION:
TEXT I
Products and dynamics of lava-snow explosions: The 16 March
2017 explosion at Mount Etna, Italy
Abstract
Volcanic hazards associated with lava flows advancing on snow
cover are often underrated, although sudden explosions related to
different processes of lava-snow/ice contact can occur rapidly and
are only preceded by small, easily underrated precursors. On 16
March 2017, during a mildly effusive and explosive eruption at
Mount Etna, Italy, a slowly advancing lava lobe interacted with the
snow cover to produce a sudden, brief sequence of explosions.
White vapor, brown ash, and coarse material were suddenly
ejected, and the products struck a group of people, injuring some
of them. The proximal deposit formed a continuous mantle of ash,
lapilli, and decimeter-sized bombs, while the ballistic material
travelled up to 200 m from the lava edge. The deposit was
estimated to have a mass of 7.1 ± 0.8 × 104 kg, which corresponds
to a volume of 32.0 ± 3.6 m3 of lava being removed by the
explosion. Data related to the texture and morphology of the
ejected clasts were used to constrain a model of lava-snow
interaction. The results suggest that the mechanism causing the
explosions was the progressive build-up of pressure due to vapor
accumulation under the lava flow, while no evidence was found for
the occurrence of fuel-coolant interaction processes. Although
these low-intensity explosions are not particularly frequent, the
data set collected provides, for the first time, quantitative
information about the processes involved and the associated
hazard and suggests that mitigation measures should be
established to prevent potentially dramatic accidents at
worldwide volcanoes frequented by tourists and with fairly easy
access, such as Etna.
Source: GSA Bulletin (2024) 136 (5-6): 2325–2342. Available at
https://pubs.geoscienceworld.org/gsa/gsabulletin/article/136/5-
6/2325/628546/Products-and-dynamics-of-lava-snow-explosions-The
Based on Text I, mark the statements below as TRUE (T) or FALSE
(F).
I) The eruption resulted in no casualties.
II) Fragments were launched high above the edge of the lava.
III) Fuel and coolant interaction caused the explosion at Mount Etna.
The statements are, respectively
I) The eruption resulted in no casualties.
II) Fragments were launched high above the edge of the lava.
III) Fuel and coolant interaction caused the explosion at Mount Etna.
The statements are, respectively
Q3757720
Inglês
Texto associado
READ TEXT I AND ANSWER THE QUESTION:
TEXT I
Products and dynamics of lava-snow explosions: The 16 March
2017 explosion at Mount Etna, Italy
Abstract
Volcanic hazards associated with lava flows advancing on snow
cover are often underrated, although sudden explosions related to
different processes of lava-snow/ice contact can occur rapidly and
are only preceded by small, easily underrated precursors. On 16
March 2017, during a mildly effusive and explosive eruption at
Mount Etna, Italy, a slowly advancing lava lobe interacted with the
snow cover to produce a sudden, brief sequence of explosions.
White vapor, brown ash, and coarse material were suddenly
ejected, and the products struck a group of people, injuring some
of them. The proximal deposit formed a continuous mantle of ash,
lapilli, and decimeter-sized bombs, while the ballistic material
travelled up to 200 m from the lava edge. The deposit was
estimated to have a mass of 7.1 ± 0.8 × 104 kg, which corresponds
to a volume of 32.0 ± 3.6 m3 of lava being removed by the
explosion. Data related to the texture and morphology of the
ejected clasts were used to constrain a model of lava-snow
interaction. The results suggest that the mechanism causing the
explosions was the progressive build-up of pressure due to vapor
accumulation under the lava flow, while no evidence was found for
the occurrence of fuel-coolant interaction processes. Although
these low-intensity explosions are not particularly frequent, the
data set collected provides, for the first time, quantitative
information about the processes involved and the associated
hazard and suggests that mitigation measures should be
established to prevent potentially dramatic accidents at
worldwide volcanoes frequented by tourists and with fairly easy
access, such as Etna.
Source: GSA Bulletin (2024) 136 (5-6): 2325–2342. Available at
https://pubs.geoscienceworld.org/gsa/gsabulletin/article/136/5-
6/2325/628546/Products-and-dynamics-of-lava-snow-explosions-The
In the fragment “a mildly effusive and explosive eruption”, the
adverb is comparable in meaning to
Q3757721
Inglês
Texto associado
READ TEXT I AND ANSWER THE QUESTION:
TEXT I
Products and dynamics of lava-snow explosions: The 16 March
2017 explosion at Mount Etna, Italy
Abstract
Volcanic hazards associated with lava flows advancing on snow
cover are often underrated, although sudden explosions related to
different processes of lava-snow/ice contact can occur rapidly and
are only preceded by small, easily underrated precursors. On 16
March 2017, during a mildly effusive and explosive eruption at
Mount Etna, Italy, a slowly advancing lava lobe interacted with the
snow cover to produce a sudden, brief sequence of explosions.
White vapor, brown ash, and coarse material were suddenly
ejected, and the products struck a group of people, injuring some
of them. The proximal deposit formed a continuous mantle of ash,
lapilli, and decimeter-sized bombs, while the ballistic material
travelled up to 200 m from the lava edge. The deposit was
estimated to have a mass of 7.1 ± 0.8 × 104 kg, which corresponds
to a volume of 32.0 ± 3.6 m3 of lava being removed by the
explosion. Data related to the texture and morphology of the
ejected clasts were used to constrain a model of lava-snow
interaction. The results suggest that the mechanism causing the
explosions was the progressive build-up of pressure due to vapor
accumulation under the lava flow, while no evidence was found for
the occurrence of fuel-coolant interaction processes. Although
these low-intensity explosions are not particularly frequent, the
data set collected provides, for the first time, quantitative
information about the processes involved and the associated
hazard and suggests that mitigation measures should be
established to prevent potentially dramatic accidents at
worldwide volcanoes frequented by tourists and with fairly easy
access, such as Etna.
Source: GSA Bulletin (2024) 136 (5-6): 2325–2342. Available at
https://pubs.geoscienceworld.org/gsa/gsabulletin/article/136/5-
6/2325/628546/Products-and-dynamics-of-lava-snow-explosions-The
The closest translation into Portuguese of “Volcanic hazards
associated with lava flows advancing on snow cover are often
underrated” is
Q3757722
Inglês
Texto associado
READ TEXT I AND ANSWER THE QUESTION:
TEXT I
Products and dynamics of lava-snow explosions: The 16 March
2017 explosion at Mount Etna, Italy
Abstract
Volcanic hazards associated with lava flows advancing on snow
cover are often underrated, although sudden explosions related to
different processes of lava-snow/ice contact can occur rapidly and
are only preceded by small, easily underrated precursors. On 16
March 2017, during a mildly effusive and explosive eruption at
Mount Etna, Italy, a slowly advancing lava lobe interacted with the
snow cover to produce a sudden, brief sequence of explosions.
White vapor, brown ash, and coarse material were suddenly
ejected, and the products struck a group of people, injuring some
of them. The proximal deposit formed a continuous mantle of ash,
lapilli, and decimeter-sized bombs, while the ballistic material
travelled up to 200 m from the lava edge. The deposit was
estimated to have a mass of 7.1 ± 0.8 × 104 kg, which corresponds
to a volume of 32.0 ± 3.6 m3 of lava being removed by the
explosion. Data related to the texture and morphology of the
ejected clasts were used to constrain a model of lava-snow
interaction. The results suggest that the mechanism causing the
explosions was the progressive build-up of pressure due to vapor
accumulation under the lava flow, while no evidence was found for
the occurrence of fuel-coolant interaction processes. Although
these low-intensity explosions are not particularly frequent, the
data set collected provides, for the first time, quantitative
information about the processes involved and the associated
hazard and suggests that mitigation measures should be
established to prevent potentially dramatic accidents at
worldwide volcanoes frequented by tourists and with fairly easy
access, such as Etna.
Source: GSA Bulletin (2024) 136 (5-6): 2325–2342. Available at
https://pubs.geoscienceworld.org/gsa/gsabulletin/article/136/5-
6/2325/628546/Products-and-dynamics-of-lava-snow-explosions-The
When the fragment “were suddenly ejected” is translated into
“foram ejetados de forma muito súbita”, the strategy used was
Q3757723
Inglês
Texto associado
READ TEXT I AND ANSWER THE QUESTION:
TEXT I
Products and dynamics of lava-snow explosions: The 16 March
2017 explosion at Mount Etna, Italy
Abstract
Volcanic hazards associated with lava flows advancing on snow
cover are often underrated, although sudden explosions related to
different processes of lava-snow/ice contact can occur rapidly and
are only preceded by small, easily underrated precursors. On 16
March 2017, during a mildly effusive and explosive eruption at
Mount Etna, Italy, a slowly advancing lava lobe interacted with the
snow cover to produce a sudden, brief sequence of explosions.
White vapor, brown ash, and coarse material were suddenly
ejected, and the products struck a group of people, injuring some
of them. The proximal deposit formed a continuous mantle of ash,
lapilli, and decimeter-sized bombs, while the ballistic material
travelled up to 200 m from the lava edge. The deposit was
estimated to have a mass of 7.1 ± 0.8 × 104 kg, which corresponds
to a volume of 32.0 ± 3.6 m3 of lava being removed by the
explosion. Data related to the texture and morphology of the
ejected clasts were used to constrain a model of lava-snow
interaction. The results suggest that the mechanism causing the
explosions was the progressive build-up of pressure due to vapor
accumulation under the lava flow, while no evidence was found for
the occurrence of fuel-coolant interaction processes. Although
these low-intensity explosions are not particularly frequent, the
data set collected provides, for the first time, quantitative
information about the processes involved and the associated
hazard and suggests that mitigation measures should be
established to prevent potentially dramatic accidents at
worldwide volcanoes frequented by tourists and with fairly easy
access, such as Etna.
Source: GSA Bulletin (2024) 136 (5-6): 2325–2342. Available at
https://pubs.geoscienceworld.org/gsa/gsabulletin/article/136/5-
6/2325/628546/Products-and-dynamics-of-lava-snow-explosions-The
According to Text I, the study concludes with
Q3757724
Inglês
READ TEXT II AND ANSWER THE QUESTION:
TEXT II
“Trench-parallel mid-ocean ridge subduction driven by alongstrike transmission of slab pull”
Source: https://pubs.geoscienceworld.org/geology/issue/52/12
In this title, the noun phrase “slab pull” refers to
TEXT II
“Trench-parallel mid-ocean ridge subduction driven by alongstrike transmission of slab pull”
Source: https://pubs.geoscienceworld.org/geology/issue/52/12
In this title, the noun phrase “slab pull” refers to
Q3757725
Inglês
TEXT II
“Trench-parallel mid-ocean ridge subduction driven by alongstrike transmission of slab pull”
Source: https://pubs.geoscienceworld.org/geology/issue/52/12
The most adequate translation of “driven” is
“Trench-parallel mid-ocean ridge subduction driven by alongstrike transmission of slab pull”
Source: https://pubs.geoscienceworld.org/geology/issue/52/12
The most adequate translation of “driven” is
Q3757726
Inglês
Texto associado
READ TEXT III AND ANSWER THE QUESTION:
TEXT III
Original: Maciços rochosos constituídos por arenitos eólicos
muitas vezes são considerados depósitos homogêneos com
relação às suas propriedades hidráulicas em função das suas
características texturais.
Source: https://www.abge.org.br/arquivos/ARTIGO%201%20-%20RevistaABGE-14-
2_Ok.pdf
Virtual Translator: Rock masses made up of aeolian sandstones are often considered homogeneous deposits in relation to its hydraulic properties depending on its textural characteristics.
Virtual Translator: Rock masses made up of aeolian sandstones are often considered homogeneous deposits in relation to its hydraulic properties depending on its textural characteristics.
Virtual Translator: Rock masses made up of aeolian sandstones
are often considered homogeneous deposits in relation to its
hydraulic properties depending on its textural characteristics.
One of the problems with the translation provided by the virtual translator is
One of the problems with the translation provided by the virtual translator is
Q3757727
Inglês
Texto associado
READ TEXT III AND ANSWER THE QUESTION:
TEXT III
Original: Maciços rochosos constituídos por arenitos eólicos
muitas vezes são considerados depósitos homogêneos com
relação às suas propriedades hidráulicas em função das suas
características texturais.
Source: https://www.abge.org.br/arquivos/ARTIGO%201%20-%20RevistaABGE-14-
2_Ok.pdf
Virtual Translator: Rock masses made up of aeolian sandstones are often considered homogeneous deposits in relation to its hydraulic properties depending on its textural characteristics.
Virtual Translator: Rock masses made up of aeolian sandstones are often considered homogeneous deposits in relation to its hydraulic properties depending on its textural characteristics.
In Text III, instead of “depending on”, the translator should have
chosen
Q3757728
Inglês
Texto associado
READ TEXT III AND ANSWER THE QUESTION:
TEXT III
Original: Maciços rochosos constituídos por arenitos eólicos
muitas vezes são considerados depósitos homogêneos com
relação às suas propriedades hidráulicas em função das suas
características texturais.
Source: https://www.abge.org.br/arquivos/ARTIGO%201%20-%20RevistaABGE-14-
2_Ok.pdf
Virtual Translator: Rock masses made up of aeolian sandstones are often considered homogeneous deposits in relation to its hydraulic properties depending on its textural characteristics.
Virtual Translator: Rock masses made up of aeolian sandstones are often considered homogeneous deposits in relation to its hydraulic properties depending on its textural characteristics.
By opting for “made up of”, the translator has introduced a phrasal
verb that is more
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