6b Besides Crater Lake give another example on Earth of thi.pdf
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6b Besides Crater Lake, give another example on Earth of this feature. 74 This is the term for the mixture of Water and Voicanic . Debris/mud that can flow down an erupting composite volcano, burying everything under many tons of mud. 8. This is the term for the Fast-flowing mixture of Super-Hor Gasses and Volcanic Debris that can cascade down an erupting composite volcano, incinerating everything in its path. 9. True or False). Some Large Vertical Eruptions (Plinian Eruptions) can inject enormous amounts of volcanic ash and sulfur-dioxide aerosols into the Stratosphere, causing global cooling for a year or more afterwards. 10 (True or False). Some volcanoes can release enormous amounts of gasses such as fluorine, Carbon Dioxide, or Sulphur Dioxide at the ground level, poisoning, suffocating, or chemically burning all living things in its path. 11a2 (True or False). The Volcanic Explosivity Scale is logarithmic, meaning that a category 3 eruption is 10 times more explosive than a category 2 eruption. 11b (True or False) The highest possible number on The Volcanic Explosivity Scale is 10. 12 Name one of the Super Volcanoes labeled as such by the USGS (from our notes).
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What are volcanic hazards
The USGS monitors almost 70 active and potentially active volcanoes in the US to assess hazards and closely monitor the most dangerous ones. Volcanoes produce many hazards including eruption columns and clouds, lava and pyroclastic flows, landslides, and lahars (mudflows) that can kill people and destroy property even long distances away. The USGS works to detect signs of unrest and warn the public of impending eruptions and hazards in order to protect lives and property.
What are volcanic hazards 1
The USGS monitors almost 70 active and potentially active volcanoes in the US to assess hazards and closely monitor the most dangerous ones. Volcanoes produce many hazards including eruption columns and clouds, lava and pyroclastic flows, landslides, and lahars (mudflows) that can kill people and destroy property even long distances away. The USGS works to detect signs of unrest and warn the public of impending eruptions and hazards in order to protect lives and property.
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The USGS monitors almost 70 active and potentially active volcanoes in the US to assess hazards and closely monitor the most dangerous ones. Volcanoes produce a variety of hazards including eruption columns and clouds, lava and pyroclastic flows, landslides, and lahars that can kill people and destroy property from miles away. The USGS works to detect signs of unrest and warn the public of impending eruptions and hazards to help reduce risks from volcano activity.
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Lahars, which can occur even when a volcano is quiet, are perhaps the next most dangerous volcanic hazard (figure 7.33). These mixtures of volcanic debris and water can flow for tens of kilometers down steep volcanic slopes at speeds that may exceed 100 kilometers (60 miles) per hour. Lahars pose a potential threat to many communities downstream from glacier-clad volcanoes such as Mount Rainier. Other potentially destructive mass-wasting events include the rapid collapse of the volcano's summit or flank.
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TNY—2006_11_20—PAGE 66—133SC.—livE ArT r15667—CriTiCAl CuT To .docx
TNY—2006_11_20—PAGE 66—133SC.—livE ArT r15667—CriTiCAl CuT To bE wATChEd ThrouGhouT ENTirE PrESS ruN—
#2 page—new title at top!
annals of science
The darkening sea
What carbon emissions are doing to the ocean.
by elizabeTh kolberT
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The neW yorker, noVeMber 20, 2006 67
Pteropods are tiny marine organisms that belong to the very broad class
known as zooplankton. Related to snails,
they swim by means of a pair of winglike
gelatinous flaps and feed by entrapping
even tinier marine creatures in a bubble of
mucus. Many pteropod species—there
are nearly a hundred in all—produce
shells, apparently for protection; some of
their predators, meanwhile, have evolved
specialized tentacles that they employ
much as diners use forks to spear escargot.
Pteropods are first male, but as they grow
older they become female.
Victoria Fabry, an oceanographer at
California State University at San Mar-
cos, is one of the world’s leading experts
on pteropods. She is slight and soft-
spoken, with wavy black hair and blue-
green eyes. Fabry fell in love with the
ocean as a teen-ager after visiting the
Outer Banks, off North Carolina, and
took up pteropods when she was in grad-
uate school, in the early nineteen-eighties.
At that point, most basic questions about
the animals had yet to be answered, and,
for her dissertation, Fabry decided to
study their shell growth. Her plan was to
raise pteropods in tanks, but she ran into
trouble immediately. When disturbed,
pteropods tend not to produce the mucus
bubbles, and slowly starve. Fabry tried
using bigger tanks for her pteropods, but
the only correlation, she recalled recently,
was that the more time she spent improv-
ing the tanks “the quicker they died.”
After a while, she resigned herself to con-
stantly collecting new specimens. This, in
turn, meant going out on just about any
research ship that would have her.
Fabry developed a simple, if brutal,
protocol that could be completed at sea.
She would catch some pteropods, either
by trawling with a net or by scuba diving,
and place them in one-litre bottles filled
with seawater, to which she had added a
small amount of radioactive calcium 45.
Forty-eight hours later, she would re-
move the pteropods from the bottles,
dunk them in warm ethanol, and pull
their bodies out with a pair of tweezers.
Back on land, she would measure how
much calcium 45 their shells had taken
up during their two days of captivity.
In the summer of 1985, Fabry got a
berth on a research vessel sailing from
Honolulu to Kodiak Island. Late in the
trip, near a spot in the Gulf of Alaska
known as Station Papa, she came upon a
TNY—2006_11_20—PAGE 68—133SC.TNY—2006_11_20—PAGE 68—#2 page new article.
68 The neW yorker, ...
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- Mud volcanoes which form from eruptions of wet
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c clustering
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symmetry 8. Which of the following taxonomic groups lacks parasitic organisms? a) Ecdysozoa b)
Nematoda c) Turbellaria d) Cestodes e) Trematoda For each of the following, select (A) True or
(B) False. 9. More than 50% of extant (currently living) animals are arthropods. 10. Segmentation
is a synapomorphy of Porifera. 11. According to recent molecular evidence presented in lecture,
Ctenophora is conclusively the most ancestral group of organisms on the animal phylogeny. 12.
On the traditional phylogeny based on morphological data, Nematoda is the most ancestral
bilaterian Phylum. 13. Pseudocoelomates lack a coelom. 14. "True jelly fish" belong to the Class
Scyphozoa. 15. Closed circulatory system is a synapomorphy of Mollusca. 16. Scolex is a unique
and distinguishing synapomorphy of Rotifers. 17. A key distinguishing synapomorphy of Bivalvia is
adductor muscles. 18. Planarians are pseudocoelomates. 19. A defining synapomorphy of
Cnidaria is choanocytes. 20. Corals provide zooxanthellae with carbon dioxide and nitrogen..
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K t boundary and Probable causes of Dinosour extinction
The K-T boundary marks the mass extinction event around 65 million years ago that killed the non-avian dinosaurs and many other species. Several lines of evidence indicate this was caused by an asteroid impact, including an iridium layer, glass spherules, shocked quartz, and soot from widespread fires. In contrast, a volcanic eruption could not explain the global distribution of these impact markers or the presence of shocked minerals only seen in impact sites. While volcanism may have also played a role, the catastrophic nature of the extinctions requires an impact to have been the ultimate cause of the end-Cretaceous mass extinction.
TNY—2006_11_20—PAGE 66—133SC.—livE ArT r15667—CriTiCAl CuT To .docx
TNY—2006_11_20—PAGE 66—133SC.—livE ArT r15667—CriTiCAl CuT To bE wATChEd ThrouGhouT ENTirE PrESS ruN—
#2 page—new title at top!
annals of science
The darkening sea
What carbon emissions are doing to the ocean.
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The neW yorker, noVeMber 20, 2006 67
Pteropods are tiny marine organisms that belong to the very broad class
known as zooplankton. Related to snails,
they swim by means of a pair of winglike
gelatinous flaps and feed by entrapping
even tinier marine creatures in a bubble of
mucus. Many pteropod species—there
are nearly a hundred in all—produce
shells, apparently for protection; some of
their predators, meanwhile, have evolved
specialized tentacles that they employ
much as diners use forks to spear escargot.
Pteropods are first male, but as they grow
older they become female.
Victoria Fabry, an oceanographer at
California State University at San Mar-
cos, is one of the world’s leading experts
on pteropods. She is slight and soft-
spoken, with wavy black hair and blue-
green eyes. Fabry fell in love with the
ocean as a teen-ager after visiting the
Outer Banks, off North Carolina, and
took up pteropods when she was in grad-
uate school, in the early nineteen-eighties.
At that point, most basic questions about
the animals had yet to be answered, and,
for her dissertation, Fabry decided to
study their shell growth. Her plan was to
raise pteropods in tanks, but she ran into
trouble immediately. When disturbed,
pteropods tend not to produce the mucus
bubbles, and slowly starve. Fabry tried
using bigger tanks for her pteropods, but
the only correlation, she recalled recently,
was that the more time she spent improv-
ing the tanks “the quicker they died.”
After a while, she resigned herself to con-
stantly collecting new specimens. This, in
turn, meant going out on just about any
research ship that would have her.
Fabry developed a simple, if brutal,
protocol that could be completed at sea.
She would catch some pteropods, either
by trawling with a net or by scuba diving,
and place them in one-litre bottles filled
with seawater, to which she had added a
small amount of radioactive calcium 45.
Forty-eight hours later, she would re-
move the pteropods from the bottles,
dunk them in warm ethanol, and pull
their bodies out with a pair of tweezers.
Back on land, she would measure how
much calcium 45 their shells had taken
up during their two days of captivity.
In the summer of 1985, Fabry got a
berth on a research vessel sailing from
Honolulu to Kodiak Island. Late in the
trip, near a spot in the Gulf of Alaska
known as Station Papa, she came upon a
TNY—2006_11_20—PAGE 68—133SC.TNY—2006_11_20—PAGE 68—#2 page new article.
68 The neW yorker, ...
The end of the world is at hand
This ppt is about the world's apocalypse, whenever it comes. We describe what can cause the world to end, what are the dangers to be aware of etc. We also explain how to protect oneself, if unfortunately the apocalypse had happened.
Volcanoes
The document discusses volcanoes and volcanic eruptions. It provides information on the number of active volcanoes, the types of eruptions (explosive vs. non-explosive), the composition of magma and how it determines eruption type, and how volcanoes form and are affected by tectonic plate boundaries and hot spots. It also discusses how volcanologists study and monitor volcanoes to predict eruptions using seismic, deformation, gas, and thermal measurements.
Volcano stations
This document provides information about a station-based volcano education program. The stations cover topics like classifying volcanoes, eruption types, magma composition, and volcanic hazards and benefits. At each station, students fill out worksheets or do activities to learn about parts of volcanoes, what causes eruptions, how silica and water content determine explosivity, different lava and pyroclastic material types, and examples of shield, cinder cone, and composite volcanoes. Math problems calculate totals, differences, distances, times, costs, and rates related to volcanic eruptions, ash and lava flows, and operating robots. The goal is to help students understand volcanoes through hands-on activities at multiple informative stations.
Volcanoes and volcanic erruptions
The document provides information about different types of volcanoes and volcanic features including:
- Shield volcanoes which are built by basalt lava flows and have gentle slopes.
- Lava domes which are built by thick, viscous lava that cools too quickly to flow very far from the eruption.
- Cinder cones which are steep sided hills made of volcanic fragments blown from eruptions of stratovolcanoes.
- Stratovolcanoes which have steep sides and are formed by violent eruptions of lava flows, tephra, and pyroclastic flows from multiple vents.
- Mud volcanoes which form from eruptions of wet
Volcanic eruption
A volcanic eruption occurs when hot materials are thrown out of a volcano. Lava, rocks, dust, ash and gas compounds are some of the materials.
Volcanic Eruption: Are you prepared?
1. Explosive volcanic eruptions can have both short and long term impacts on society, such as destroying landscapes with lava flows and ash clouds that disrupt transportation.
2. The 1991 eruption of Mt. Pinatubo cooled the Earth's surface for almost two years by injecting ash into the atmosphere.
3. Volcanoes can also have economic benefits, including providing fertile soil, attractions for tourism, and resources like geothermal energy, sulfur, and building materials. However, the major concern is reducing the negative impacts of eruptions to minimize loss of life and property damage.
Volcano
Volcanoes form when magma rises up from below the Earth's crust and erupts. There are three main types of volcanic eruptions that differ based on the speed and viscosity of the magma: magmatic, phreatomagmatic, and phreatic. Monitoring volcanoes for changes in shape, temperature, and seismic activity can help predict eruptions and allow for evacuation planning to reduce risk to humans. The largest volcanic eruption in history was the Lake Toba eruption in Indonesia around 75,000 years ago.
The causes of climate change
Paleoclimatology is the study of past climates through the use of proxies such as microbial life found in sediment cores, ice cores, and tree rings. Researchers use various analytical methods to extract information from these proxies about past climate conditions. For example, oxygen isotope ratios in foraminifera and diatom shells can provide information about past water temperatures, and the abundance and composition of microbial populations may indicate environmental conditions like temperature. Volcanic eruptions can influence climate in both the short and long term. Large eruptions that eject ash and sulfur dioxide into the stratosphere can block sunlight and cool the planet for several years through radiation scattering. However, massive eruptions that release large amounts of carbon dioxide may
The map of asteroids risks and defence
This document maps out the risks of asteroid impacts and strategies for asteroid defence. It divides asteroids into three size categories - those around 300m which could cause millions of deaths, those around 30km which could cause civilization collapse, and those over 10km which could cause human extinction. Observation is currently the best method for risk reduction, while large nuclear deflection risks creating more threats than benefits. The main uncertainty is whether Earth is currently experiencing an intense bombardment period due to a recent large comet breakup.
Extinction of the Dinosaurs.ppt
The document discusses several theories for the extinction of dinosaurs at the end of the Cretaceous period around 65 million years ago, known as the KT extinction event. It notes that physicist Luis Alvarez suggested that a large meteor impact may have been responsible due to an unusually high concentration of iridium found in the geological KT boundary. However, no crater of sufficient size has been found, leading to the multiple impact theory that several smaller impacts around the world contributed. Another theory is that high volcanic activity from the Deccan Traps in India caused climate changes through dust and smog that led to the extinction of dinosaur populations unable to adapt.
Climate Change v 2012
The document discusses several factors related to climate change:
1. It discusses three primary factors that influence Earth's orbit and axial tilt - eccentricity, axial tilt, and precession - and how these Milankovitch cycles impact climate over long time periods.
2. It explains the Ruddiman hypothesis, which suggests that human agricultural activities beginning around 8,000 years ago prevented the onset of a natural ice age, and industrialization in the 19th century further disrupted the climate cycle.
3. It provides examples of how human activities like fossil fuel use, deforestation, and agriculture have increased greenhouse gases in the atmosphere like carbon dioxide and methane, driving unprecedented modern climate change.
Similar to 6b Besides Crater Lake give another example on Earth of thi.pdf (20)
K t boundary and Probable causes of Dinosour extinction
K t boundary and Probable causes of Dinosour extinction
TNY—2006_11_20—PAGE 66—133SC.—livE ArT r15667—CriTiCAl CuT To .docx
TNY—2006_11_20—PAGE 66—133SC.—livE ArT r15667—CriTiCAl CuT To .docx
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ISO/IEC 27001, ISO/IEC 42001, and GDPR: Best Practices for Implementation and...
ISO/IEC 27001, ISO/IEC 42001, and GDPR: Best Practices for Implementation and...
How to Create a More Engaging and Human Online Learning Experience
How to Create a More Engaging and Human Online Learning Experience
How to Setup Warehouse & Location in Odoo 17 Inventory
How to Setup Warehouse & Location in Odoo 17 Inventory
BÀI TẬP DẠY THÊM TIẾNG ANH LỚP 7 CẢ NĂM FRIENDS PLUS SÁCH CHÂN TRỜI SÁNG TẠO ...
BÀI TẬP DẠY THÊM TIẾNG ANH LỚP 7 CẢ NĂM FRIENDS PLUS SÁCH CHÂN TRỜI SÁNG TẠO ...
Film vocab for eal 3 students: Australia the movie
Film vocab for eal 3 students: Australia the movie
6b Besides Crater Lake give another example on Earth of thi.pdf
- 1. 6b Besides Crater Lake, give another example on Earth of this feature. 74 This is the term for the mixture of Water and Voicanic . Debris/mud that can flow down an erupting composite volcano, burying everything under many tons of mud. 8. This is the term for the Fast-flowing mixture of Super-Hor Gasses and Volcanic Debris that can cascade down an erupting composite volcano, incinerating everything in its path. 9. True or False). Some Large Vertical Eruptions (Plinian Eruptions) can inject enormous amounts of volcanic ash and sulfur-dioxide aerosols into the Stratosphere, causing global cooling for a year or more afterwards. 10 (True or False). Some volcanoes can release enormous amounts of gasses such as fluorine, Carbon Dioxide, or Sulphur Dioxide at the ground level, poisoning, suffocating, or chemically burning all living things in its path. 11a2 (True or False). The Volcanic Explosivity Scale is logarithmic, meaning that a category 3 eruption is 10 times more explosive than a category 2 eruption. 11b (True or False) The highest possible number on The Volcanic Explosivity Scale is 10. 12 Name one of the Super Volcanoes labeled as such by the USGS (from our notes)