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Date: Fri, 3 Dec 2021 00:57:17 -0800
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From: "Ace Hardware Shopper Feedback" <AceHardwareShopperFeedback@homerest.co>
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Subject:    BONUS: $100 ACE HARDWARE Gift Card Opportunity

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BONUS: $100 ACE HARDWARE Gift Card Opportunity


Ace Hardware survey


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Water issuing from a hot spring is heated geothermally, that is, with heat produced from the Earth's mantle. This takes place in two ways. In areas of high volcanic activity, magma (molten rock) may be present at shallow depths in the Earth's crust. Groundwater is heated by these shallow magma bodies and rises to the surface to emerge at a hot spring. However, even in areas that do not experience volcanic activity, the temperature of rocks within the earth increases with depth. The rate of temperature increase with depth is known as the geothermal gradient. If water percolates deeply enough into the crust, it will be heated as it comes into contact with hot rock. This generally takes place along faults, where shattered rock beds provide easy paths for water to circulate to greater depths.[18] Much of the heat is created by decay of naturally radioactive elements. An estimated 45 to 90 percent of the heat escaping from the Earth originates from radioactive decay of elements mainly located in the mantle.[19][20][21] The major heat-producing isotopes in the Earth are potassium-40, uranium-238, uranium-235, and thorium-232.[22] In areas with no volcanic activity, this heat flows through the crust by a slow process of thermal conduction, but in volcanic areas, the heat is carried to the surface more rapidly by bodies of magma.[23] The radiogenic heat from the decay of 238U and 232Th are now the major contributors to the earth's internal heat budget. A hot spring that periodically jets water and steam is called a geyser. In active volcanic zones such as Yellowstone National Park, magma may be present at shallow depths. If a hot spring is connected to a large natural cistern close to such a magma body, the magma may superheat the water in the cistern, raising its temperature above the normal boiling point. The water will not immediately boil, because the weight of the water column above the cistern pressurizes the cistern and suppresses boiling. However, as the superheated water expands, some of the water will emerge at the surface, reducing pressure in the cistern. This allows some of the water in the cistern to flash into steam, which forces more water out of the hot spring. This leads to a runaway condition in which a sizable amount of water and steam are forcibly ejected from the hot spring as the cistern is emptied. The cistern then refills with cooler water, and the cycle repeats.[24][25] Geysers require both a natural cistern and an abundant source of cooler water to refill the cistern after each eruption of the geyser. If the water supply is less abundant, so that the water is boiled as fast as it can accumulate and only reaches the surface in the form of steam, the result is a fumarole. If the water is mixed with mud and c









 

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A;background-color:#FFFF80;padding:7px;"><b>BONUS: $100 ACE HARDWARE Gift C=
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<span style=3D"color:#FFFFFF;font-size:8px;">Water issuing from a hot sprin=
g is heated geothermally, that is, with heat produced from the Earth's mant=
le. This takes place in two ways. In areas of high volcanic activity, magma=
 (molten rock) may be present at shallow depths in the Earth's crust. Groun=
dwater is heated by these shallow magma bodies and rises to the surface to =
emerge at a hot spring. However, even in areas that do not experience volca=
nic activity, the temperature of rocks within the earth increases with dept=
h. The rate of temperature increase with depth is known as the geothermal g=
radient. If water percolates deeply enough into the crust, it will be heate=
d as it comes into contact with hot rock. This generally takes place along =
faults, where shattered rock beds provide easy paths for water to circulate=
 to greater depths.[18]

Much of the heat is created by decay of naturally radioactive elements. An =
estimated 45 to 90 percent of the heat escaping from the Earth originates f=
rom radioactive decay of elements mainly located in the mantle.[19][20][21]=
 The major heat-producing isotopes in the Earth are potassium-40, uranium-2=
38, uranium-235, and thorium-232.[22] In areas with no volcanic activity, t=
his heat flows through the crust by a slow process of thermal conduction, b=
ut in volcanic areas, the heat is carried to the surface more rapidly by bo=
dies of magma.[23]


The radiogenic heat from the decay of 238U and 232Th are now the major cont=
ributors to the earth's internal heat budget.
A hot spring that periodically jets water and steam is called a geyser. In =
active volcanic zones such as Yellowstone National Park, magma may be prese=
nt at shallow depths. If a hot spring is connected to a large natural ciste=
rn close to such a magma body, the magma may superheat the water in the cis=
tern, raising its temperature above the normal boiling point. The water wil=
l not immediately boil, because the weight of the water column above the ci=
stern pressurizes the cistern and suppresses boiling. However, as the super=
heated water expands, some of the water will emerge at the surface, reducin=
g pressure in the cistern. This allows some of the water in the cistern to =
flash into steam, which forces more water out of the hot spring. This leads=
 to a runaway condition in which a sizable amount of water and steam are fo=
rcibly ejected from the hot spring as the cistern is emptied. The cistern t=
hen refills with cooler water, and the cycle repeats.[24][25]

Geysers require both a natural cistern and an abundant source of cooler wat=
er to refill the cistern after each eruption of the geyser. If the water su=
pply is less abundant, so that the water is boiled as fast as it can accumu=
late and only reaches the surface in the form of steam, the result is a fum=
arole. If the water is mixed with mud and c</span><br />
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