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This document lists factors that affect tropical rainforest ecosystems, including whether they are human or physical factors. It provides a template to identify each factor, cite the research source, explain the effects on the rainforest, and propose a question or hypothesis to investigate further. Some example factors given are light intensity, deforestation, and climate.
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Gujerat
This document provides information about an earthquake that occurred in Gujarat, India on January 26, 2001. It summarizes the key details of the earthquake including where it happened in northwestern India near the city of Bhuj, when it occurred, its magnitude of 7.9 on the Richter scale, and the significant damage and loss of life it caused with almost 20,000 confirmed deaths. It also outlines the primary effects such as destruction of buildings and infrastructure as well as secondary effects like homelessness, injuries, and spread of disease. Short and long-term response efforts are summarized.
Chapter 1 gateway 1
The document discusses tectonic hazards from living in areas prone to natural disasters. It describes a deadly 2010 eruption of Mount Merapi in Indonesia that killed over 350 people and forced 300,000 from their homes, despite warnings. Some remained to care for cattle. It also discusses over 600,000 people living near the dangerous Mount Vesuvius volcano in Italy, which last erupted catastrophically in 79 CE. The chapter explores why some areas are more prone to tectonic hazards, landforms at plate boundaries, and earthquake preparedness and response.
Volcano types
There are two main types of volcanoes: shield volcanoes and composite/strato volcanoes. Shield volcanoes erupt basaltic lava at constructive plate margins and have gentle, frequent eruptions. Composite/strato volcanoes erupt acidic lava and ash at destructive plate margins and have irregular, occasionally violent eruptions with long dormant periods.
Volcano types
There are two main types of volcanoes: shield volcanoes and composite/strato volcanoes. Shield volcanoes erupt basaltic lava at constructive plate margins and have gentle, frequent eruptions that emit thin, runny lava. Composite/strato volcanoes erupt acidic lava at destructive plate margins and have potentially explosive, irregular eruptions that emit ash, rock fragments, and thicker lava.
Earthquake’s effect on developing countries
Our teacher asked us to reasearch ''earthquakes effect on deveeloping countries''. This is what i found out...
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.
The alps case study
The Alps were formed by tectonic plate collision and consist of several countries. People have adapted to conditions in the Alps by activities like farming goats well-suited to steep slopes and using hydroelectric power from dammed valleys. Tourism is a major economic driver with over 100 million visitors annually participating in winter sports and summer activities. Infrastructure like roads, tunnels, and villages have been built to accommodate people and connect locations in the mountainous region.
Kobe, japan
The 1995 Kobe earthquake in Japan killed over 6,000 people and left hundreds of thousands homeless. The magnitude 7.2 earthquake struck near the city of Kobe, damaging buildings, roads, and infrastructure. Short-term responses included evacuating survivors to shelters, clearing rubble, and providing emergency aid. Long-term responses rebuilt damaged infrastructure, implemented stronger earthquake-resistant building standards, and improved disaster response coordination.
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Gujerat
This document provides information about an earthquake that occurred in Gujarat, India on January 26, 2001. It summarizes the key details of the earthquake including where it happened in northwestern India near the city of Bhuj, when it occurred, its magnitude of 7.9 on the Richter scale, and the significant damage and loss of life it caused with almost 20,000 confirmed deaths. It also outlines the primary effects such as destruction of buildings and infrastructure as well as secondary effects like homelessness, injuries, and spread of disease. Short and long-term response efforts are summarized.
Chapter 1 gateway 1
The document discusses tectonic hazards from living in areas prone to natural disasters. It describes a deadly 2010 eruption of Mount Merapi in Indonesia that killed over 350 people and forced 300,000 from their homes, despite warnings. Some remained to care for cattle. It also discusses over 600,000 people living near the dangerous Mount Vesuvius volcano in Italy, which last erupted catastrophically in 79 CE. The chapter explores why some areas are more prone to tectonic hazards, landforms at plate boundaries, and earthquake preparedness and response.
Volcano types
There are two main types of volcanoes: shield volcanoes and composite/strato volcanoes. Shield volcanoes erupt basaltic lava at constructive plate margins and have gentle, frequent eruptions. Composite/strato volcanoes erupt acidic lava and ash at destructive plate margins and have irregular, occasionally violent eruptions with long dormant periods.
Volcano types
There are two main types of volcanoes: shield volcanoes and composite/strato volcanoes. Shield volcanoes erupt basaltic lava at constructive plate margins and have gentle, frequent eruptions that emit thin, runny lava. Composite/strato volcanoes erupt acidic lava at destructive plate margins and have potentially explosive, irregular eruptions that emit ash, rock fragments, and thicker lava.
Earthquake’s effect on developing countries
Our teacher asked us to reasearch ''earthquakes effect on deveeloping countries''. This is what i found out...
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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 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.
The alps case study
The Alps were formed by tectonic plate collision and consist of several countries. People have adapted to conditions in the Alps by activities like farming goats well-suited to steep slopes and using hydroelectric power from dammed valleys. Tourism is a major economic driver with over 100 million visitors annually participating in winter sports and summer activities. Infrastructure like roads, tunnels, and villages have been built to accommodate people and connect locations in the mountainous region.
Kobe, japan
The 1995 Kobe earthquake in Japan killed over 6,000 people and left hundreds of thousands homeless. The magnitude 7.2 earthquake struck near the city of Kobe, damaging buildings, roads, and infrastructure. Short-term responses included evacuating survivors to shelters, clearing rubble, and providing emergency aid. Long-term responses rebuilt damaged infrastructure, implemented stronger earthquake-resistant building standards, and improved disaster response coordination.
The himalayas case study
The Himalayas stretch across six countries in South Asia and formed due to the collision of the Indian and Eurasian tectonic plates. The mountain range experiences earthquakes, avalanches, landslides, and floods that endanger human life. While tourism, industry, farming, and hydropower generation provide some economic benefits, they can also damage the fragile environment through pollution, erosion, and habitat destruction. Settlement is challenging due to the extreme climate and difficult terrain.
Reducing the impacts of volcanoes
Predicting volcanic eruptions allows time for evacuation, reducing injuries and deaths. Planning avoids development in high risk areas and prepares emergency responses. Building techniques can strengthen structures against ash or divert lava. Educating the public about evacuation and survival kits helps people get to safety. International aid for poorer countries lessens eruption impacts like hunger.
Impacts of volcanoes
Volcanic eruptions have both primary and secondary impacts. The primary impacts are the immediate destruction caused by lava flows, pyroclastic flows, ash falls, and gases. Secondary impacts occur later and include mudflows that cause additional destruction, fires started by the primary impacts, and shortages of food, water and other resources as crops are damaged and infrastructure is impacted.
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 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.
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.
Plate margin
The document summarizes four types of plate boundaries:
1) Destructive boundaries occur where oceanic crust sinks under continental crust, forming trenches and volcanoes. Examples are the Nazca and South American plate.
2) Constructive boundaries form where plates move apart and new crust is created, like at the Mid-Atlantic Ridge in Iceland.
3) Collision boundaries happen when continental plates crash into each other, pushing the crust upward to form mountain ranges like the Himalayas.
4) Conservative boundaries experience little change as plates slide past each other, such as the Pacific and North American plate along the San Andreas Fault in California.
Plate margin
The document describes four types of plate boundaries: destructive, constructive, collision, and conservative. Destructive boundaries involve one plate sinking under another, forming trenches and volcanoes. Constructive boundaries involve plates moving apart and new crust forming at mid-ocean ridges. Collision boundaries occur when continental plates collide, pushing the crust upward to form fold mountains. Conservative boundaries involve plates sliding past each other without creation or destruction of crust.
Mariana trench
The Mariana Trench is the deepest point on Earth located in the western Pacific Ocean. It is over 7 miles deep and experiences pressures of over 8 tons per square inch at its lowest point. The trench formed as the dense Philippine Plate subducts under the lighter Eurasian Plate, dragging the edge of the continental crust downward. While the trench has been proposed for nuclear waste disposal, international law prohibits ocean dumping and subduction zones are prone to large, unpredictable earthquakes.
Mariana trench
The Mariana Trench is the deepest point on Earth, located in the western Pacific Ocean west of the Mariana Islands. It is over 7 miles deep at its lowest point. The trench formed as the dense Philippine Plate subducts under the lighter Eurasian Plate, dragging the edge of the continental crust downward. While proposed as a nuclear waste disposal site, dumping nuclear waste is prohibited and the large earthquakes of subduction zones make it unpredictable and potentially unsafe. The trench is also used as a passage by submarines circling the Pacific Ocean.
Mariana trench
The Mariana Trench is the deepest point on Earth, located in the western Pacific Ocean east of the Philippines. It measures over 1,500 miles long and has an average width of around 43 miles. The trench formed as the dense Philippine Plate subducts under the lighter Eurasian Plate, dragging the edge of the continental crust downward to a maximum depth of nearly 7 miles at the Challenger Deep. While the trench has been proposed for nuclear waste disposal, international law prohibits ocean dumping and the area is seismically active with large megathrust earthquakes. Scientists are studying trenches further to understand their role in seismic activity.
Mariana Trench
The Mariana Trench is the deepest point on Earth, located in the western Pacific Ocean east of the Philippines. It measures over 1,500 miles long and averages 43 miles wide, with its deepest point, Challenger Deep, reaching nearly 7 miles below the surface. The Mariana Trench formed as the dense Philippine Plate subducted under the lighter Eurasian Plate, dragging the edge of the continental crust downward. While some propose it as a nuclear waste disposal site, international law prohibits dumping waste and the large mega earthquakes of subduction zones pose unpredictable risks. The Trench is also used as a passage by submarines and geologists now believe such trenches influence earthquake activity.
Mariana trench
The Mariana Trench is the deepest point on Earth, located in the western Pacific Ocean east of the Philippines. It measures over 1,500 miles long and averages 43 miles wide, with its deepest point, Challenger Deep, reaching nearly 7 miles below the surface. The Mariana Trench formed as the dense Philippine Plate subducted under the lighter Eurasian Plate, dragging the edge of the continental crust downward. While proposed as a nuclear waste disposal site, international law prohibits dumping nuclear waste in the oceans. The Trench is also used as an underwater passage by submarines and is helping scientists understand earthquake generation at subduction zones.
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The himalayas case study
The Himalayas stretch across six countries in South Asia and formed due to the collision of the Indian and Eurasian tectonic plates. The mountain range experiences earthquakes, avalanches, landslides, and floods that endanger human life. While tourism, industry, farming, and hydropower generation provide some economic benefits, they can also damage the fragile environment through pollution, erosion, and habitat destruction. Settlement is challenging due to the extreme climate and difficult terrain.
Reducing the impacts of volcanoes
Predicting volcanic eruptions allows time for evacuation, reducing injuries and deaths. Planning avoids development in high risk areas and prepares emergency responses. Building techniques can strengthen structures against ash or divert lava. Educating the public about evacuation and survival kits helps people get to safety. International aid for poorer countries lessens eruption impacts like hunger.
Impacts of volcanoes
Volcanic eruptions have both primary and secondary impacts. The primary impacts are the immediate destruction caused by lava flows, pyroclastic flows, ash falls, and gases. Secondary impacts occur later and include mudflows that cause additional destruction, fires started by the primary impacts, and shortages of food, water and other resources as crops are damaged and infrastructure is impacted.
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 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.
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.
Plate margin
The document summarizes four types of plate boundaries:
1) Destructive boundaries occur where oceanic crust sinks under continental crust, forming trenches and volcanoes. Examples are the Nazca and South American plate.
2) Constructive boundaries form where plates move apart and new crust is created, like at the Mid-Atlantic Ridge in Iceland.
3) Collision boundaries happen when continental plates crash into each other, pushing the crust upward to form mountain ranges like the Himalayas.
4) Conservative boundaries experience little change as plates slide past each other, such as the Pacific and North American plate along the San Andreas Fault in California.
Plate margin
The document describes four types of plate boundaries: destructive, constructive, collision, and conservative. Destructive boundaries involve one plate sinking under another, forming trenches and volcanoes. Constructive boundaries involve plates moving apart and new crust forming at mid-ocean ridges. Collision boundaries occur when continental plates collide, pushing the crust upward to form fold mountains. Conservative boundaries involve plates sliding past each other without creation or destruction of crust.
Mariana trench
The Mariana Trench is the deepest point on Earth located in the western Pacific Ocean. It is over 7 miles deep and experiences pressures of over 8 tons per square inch at its lowest point. The trench formed as the dense Philippine Plate subducts under the lighter Eurasian Plate, dragging the edge of the continental crust downward. While the trench has been proposed for nuclear waste disposal, international law prohibits ocean dumping and subduction zones are prone to large, unpredictable earthquakes.
Mariana trench
The Mariana Trench is the deepest point on Earth, located in the western Pacific Ocean west of the Mariana Islands. It is over 7 miles deep at its lowest point. The trench formed as the dense Philippine Plate subducts under the lighter Eurasian Plate, dragging the edge of the continental crust downward. While proposed as a nuclear waste disposal site, dumping nuclear waste is prohibited and the large earthquakes of subduction zones make it unpredictable and potentially unsafe. The trench is also used as a passage by submarines circling the Pacific Ocean.
Mariana trench
The Mariana Trench is the deepest point on Earth, located in the western Pacific Ocean east of the Philippines. It measures over 1,500 miles long and has an average width of around 43 miles. The trench formed as the dense Philippine Plate subducts under the lighter Eurasian Plate, dragging the edge of the continental crust downward to a maximum depth of nearly 7 miles at the Challenger Deep. While the trench has been proposed for nuclear waste disposal, international law prohibits ocean dumping and the area is seismically active with large megathrust earthquakes. Scientists are studying trenches further to understand their role in seismic activity.
Mariana Trench
The Mariana Trench is the deepest point on Earth, located in the western Pacific Ocean east of the Philippines. It measures over 1,500 miles long and averages 43 miles wide, with its deepest point, Challenger Deep, reaching nearly 7 miles below the surface. The Mariana Trench formed as the dense Philippine Plate subducted under the lighter Eurasian Plate, dragging the edge of the continental crust downward. While some propose it as a nuclear waste disposal site, international law prohibits dumping waste and the large mega earthquakes of subduction zones pose unpredictable risks. The Trench is also used as a passage by submarines and geologists now believe such trenches influence earthquake activity.
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The Mariana Trench is the deepest point on Earth, located in the western Pacific Ocean east of the Philippines. It measures over 1,500 miles long and averages 43 miles wide, with its deepest point, Challenger Deep, reaching nearly 7 miles below the surface. The Mariana Trench formed as the dense Philippine Plate subducted under the lighter Eurasian Plate, dragging the edge of the continental crust downward. While proposed as a nuclear waste disposal site, international law prohibits dumping nuclear waste in the oceans. The Trench is also used as an underwater passage by submarines and is helping scientists understand earthquake generation at subduction zones.
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Control assessment
- 1. Factors affecting a Tropical Rainforest Ecosystem (TRF) In the table below list any ‘factors’ HUMAN (H)+ PHYSICAL (P) which have an impact on a TRF ecosystem, note your research page, effects and possible Qns/hypothesis you could investigate. Factor Research Effects on TRF Possible question OR hypothesis to investigate? e.g. Light Intensity (P) Textbook title …… ……. Web address … … … e.g. Deforestation e.g. climate