Presentation on Hurricanes Hurricanes are severe tropical storms that form in the southern Atlantic Ocean, Caribbean Sea, Gulf of Mexico, and in the eastern Pacific Ocean. Hurricanes gather heat…
Snowflake Symmetry: Rotations and Translations in Nature This lecture introduce on Snowflake Symmetry: Rotations and Translations in Nature. Snowflakes are all six sided because of their chemistry. They are made of water molecules. Water molecules are…
Lecture on Lightning Principle objective of this lecture is to present on Lightning. The action of rising and descending air within a thunderstorm separates positive and negative charges. Water and ice…
Earth’s Weather: Oceans and Air Temperature This lecture introduce on Earth’s Weather: Oceans and Air Temperature. Here briefly focus on how do oceans affect temperature on land. The ocean plays a fundamental role…
Volcano Monitoring and Hazard Mitigation Volcanoes can be extremely hazardous natural phenomena. That is why it is important to understand as much as possible about them, in an attempt to…
Lecture on Noxious Gas Lake Nyos is a crater lake inside a dormant volcano. The lake had become laden with carbon dioxide gas. This gas had suddenly bubbled out of…
Gas Monitoring in Volcano This lecture introduce on Gas Monitoring in Volcano. Commonly gas output from a volcano increases or changes composition before an eruption. As magma rises to the surface it…
Deformation Monitoring Principle objective of this lecture is to present on Deformation Monitoring. “Tiltmeters” are used to measure the deformation of the volcano. The tiltmeters measure changes in slope…
Lecture on Seismic Activity Seismic activity is defined as the types, frequency and size of earthquakes that happen over a period of time in a certain area. Many erupts are…
Lecture on Volcano Monitoring Major purpose of this lecture is to present on Volcano Monitoring. Volcano Observatories are set up on all active volcanoes that threaten the human population. These are…
Presentation on Lava Flow Lava flows although generally slower moving and less catastrophic than pyroclastic flows still remain dangerous. It have temperatures in excess of 200 degrees Celsius. Therefore…
How do Pyroclastic Flows cause devastation? The aim of this lecture is to present on How do Pyroclastic Flows cause devastation? The direct force of a pyroclastic flow traveling at 10’s of metres…