<s>[INST] You are a smart text analyzer assistant.
Given a QUESTION and a set of posible texts from which to derive the answer, examine each text and reply whether or not the ANSWER exists within the text.
You MUST give the response in a VALID JSON object with a Yes or No for each text.


So for instance the following:

QUESTION: What is the color of the sky?
POSIBLE ANSWERS:
Source 1: The sky is blue
Source 2: The sea is blue
Source 3: The sky is blue in the daytime but black at night

would give an output of:[/INST]

{
"Source 1": "Yes",
"Source 2": "No",
"Source 3": "Yes"
}
</s>
 
[INST]
QUESTION: what are pyroclastic flows
POSIBLE ANSWERS:
Source 1: Pyroclastic flows commonly are produced either by the fallback and downslope movement of fragments from an eruption column or by the direct frothing over at the vent of magma undergoing rapid gas loss. Volcanic froth so formed is called pumice. The term pyroclastic''--derived from the Greek words pyro (fire) and klastos (broken)--describes materials formed by the fragmentation of magma and rock by explosive volcanic activity.
Source 2: A pyroclastic flow (also known scientifically as a pyroclastic density current) is a fast-moving current of hot gas and rock (collectively known as tephra), which reaches speeds moving away from a volcano of up to 700 km/h (450 mph). The gas can reach temperatures of about 1,000 °C (1,830 °F). Pyroclastic flows normally hug the ground and travel downhill, or spread laterally under gravity. Their speed depends upon the density of the current, the volcanic output rate, and the gradient of the slope. They are a common and devastating result of certain explosive volcanic eruptions
Source 3: GENERAL CHARACTERISTICS. A pyroclastic flow is a fluidized mixture of solid to semi-solid fragments and hot, expanding gases that flows down the flank of a volcanic edifice. PUMICE FLOWS. Pumice flows are pumice-rich pyroclastic flows derived from the collapse of an eruption column. The lowermost part of the eruption column is called the gas thrust region. Here, the density of the eruption column is greater than the density of the surrounding air.
[/INST]
<s>[INST] You are a smart text analyzer assistant.
Given a QUESTION and a set of posible texts from which to derive the answer, examine each text and reply whether or not the ANSWER exists within the text.
You MUST give the response in a VALID JSON object with a Yes or No for each text.


So for instance the following:

QUESTION: What is the color of the sky?
POSIBLE ANSWERS:
Source 1: The sky is blue
Source 2: The sea is blue
Source 3: The sky is blue in the daytime but black at night

would give an output of:[/INST]

{
"Source 1": "Yes",
"Source 2": "No",
"Source 3": "Yes"
}
</s>
 
[INST]
QUESTION: what are pyroclastic flows
POSIBLE ANSWERS:
Source 1: Pyroclastic flows commonly are produced either by the fallback and downslope movement of fragments from an eruption column or by the direct frothing over at the vent of magma undergoing rapid gas loss. Volcanic froth so formed is called pumice. The term pyroclastic''--derived from the Greek words pyro (fire) and klastos (broken)--describes materials formed by the fragmentation of magma and rock by explosive volcanic activity.
Source 2: A pyroclastic flow (also known scientifically as a pyroclastic density current) is a fast-moving current of hot gas and rock (collectively known as tephra), which reaches speeds moving away from a volcano of up to 700 km/h (450 mph). The gas can reach temperatures of about 1,000 °C (1,830 °F). Pyroclastic flows normally hug the ground and travel downhill, or spread laterally under gravity. Their speed depends upon the density of the current, the volcanic output rate, and the gradient of the slope. They are a common and devastating result of certain explosive volcanic eruptions
Source 3: GENERAL CHARACTERISTICS. A pyroclastic flow is a fluidized mixture of solid to semi-solid fragments and hot, expanding gases that flows down the flank of a volcanic edifice. PUMICE FLOWS. Pumice flows are pumice-rich pyroclastic flows derived from the collapse of an eruption column. The lowermost part of the eruption column is called the gas thrust region. Here, the density of the eruption column is greater than the density of the surrounding air.
[/INST]
{
"Source 1": "Yes",
"Source 2": "Yes",
"Source 3": "Yes"
}
<s>[INST] You are a smart text analyzer assistant.
Given a QUESTION and a set of posible texts from which to derive the answer, examine each text and reply whether or not the ANSWER exists within the text.
You MUST give the response in a VALID JSON object with a Yes or No for each text.


So for instance the following:

QUESTION: What is the color of the sky?
POSIBLE ANSWERS:
Source 1: The sky is blue
Source 2: The sea is blue
Source 3: The sky is blue in the daytime but black at night

would give an output of:[/INST]

{
"Source 1": "Yes",
"Source 2": "No",
"Source 3": "Yes"
}
</s>
 
[INST]
QUESTION: what are pyroclastic flows
POSIBLE ANSWERS:
Source 1: Pyroclastic flows commonly are produced either by the fallback and downslope movement of fragments from an eruption column or by the direct frothing over at the vent of magma undergoing rapid gas loss. Volcanic froth so formed is called pumice. The term pyroclastic''--derived from the Greek words pyro (fire) and klastos (broken)--describes materials formed by the fragmentation of magma and rock by explosive volcanic activity.
Source 2: A pyroclastic flow (also known scientifically as a pyroclastic density current) is a fast-moving current of hot gas and rock (collectively known as tephra), which reaches speeds moving away from a volcano of up to 700 km/h (450 mph). The gas can reach temperatures of about 1,000 °C (1,830 °F). Pyroclastic flows normally hug the ground and travel downhill, or spread laterally under gravity. Their speed depends upon the density of the current, the volcanic output rate, and the gradient of the slope. They are a common and devastating result of certain explosive volcanic eruptions
Source 3: GENERAL CHARACTERISTICS. A pyroclastic flow is a fluidized mixture of solid to semi-solid fragments and hot, expanding gases that flows down the flank of a volcanic edifice. PUMICE FLOWS. Pumice flows are pumice-rich pyroclastic flows derived from the collapse of an eruption column. The lowermost part of the eruption column is called the gas thrust region. Here, the density of the eruption column is greater than the density of the surrounding air.
[/INST]
{
"Source 1": "No",
"Source 2": "No",
"Source 3": "No"
}