Volcano with accounts of eruption documented within 10,000 years
Active volcano
Big body of land on the globe
Continent
Vibration of Earth due to the rapid release of energy
Earthquake
Location on the Earth's surface directly above the focus of an earthquake
Epicenter
Exact site of the origin of an earthquake, below the epicenter
Focus
Liquid rock below the Earth's surface
Magma
Landmass that projects well above its surroundings; higher than a hill
Mountain
Chain of mountains
Mountain ranges
First type of seismic wave to be recorded in a seismic station, these compression waves are the fastest and travel through solids, liquids, and gases
Primary waves
Second type of earthquake wave to be recorded in a seismic station; these shearing waves are stronger than P-waves, but only move through solids
Secondary waves
Graphical record of an earthquake
Seismogram
Measuring instrument for detecting and measuring the intensity and direction and duration of movements of an earthquake
Seismograph
Japanese term for "big wave in the port;" generated during undersea quakes
Tsunami
Mountain or hill, typically conical, having a crater or vent through which lava, rock fragments, hot vapor and gas is being or have been erupted from the earth's crust
Volcano
Our Earth has four layers consisting of different materials, namely, crust, mantle, inner, and outer core. For this module, we will focus on the lithosphere which is composed of the crust and the upper mantle.
The lithosphere is said to be in constant but very slow motion. These motions are not the same everywhere. This movement of the lithosphere is called tectonics.
Plates are in constant motion. As they interact along their margins, important geologic processes take places, such as the formation of major mountain ranges, active volcanoes, and earthquake epicenters.
Plate Tectonics
Theory that the entire lithosphere of the Earth is broken into numerous segments called plates that move very slowly but constantly
Lithosphere consists of crust and the upper portion of the mantle. The crust is made of a variety of solid rocks like sedimentary, metamorphic,and igneous. It has an average density of 2.8 g/cm3 and its thickness ranges from 5 to 50 km.
Continental crust is thicker but less dense than the oceanic crust. Because of the difference in density, continental crust floats higher than the oceanic crust.
The Seven Continents
North America
Europe
Asia
South America
Antarctica
Africa
Australia
Plate movements may result in earthquakes. Earthquakes may happen anytime, either on land or underwater. Earthquakes on land can be caused either by tectonic plates movement or volcanic eruptions. Earthquakes under the sea can cause a tsunami.
The Philippines is situated in the Pacific Ring of Fire, a long chain of volcanoes and other tectonically active structures that surround the Pacific Ocean. The Ring of Fire is one of the most geologically active areas on Earth and a site for frequent earthquakes and powerful volcanic eruptions.
Triangulation method
Scientists use triangulation to find the epicenter of an earthquake. When seismic data is collected from at least three different locations, it can be used to determine the epicenter by where it intersects.
Top ten provinces at risk to earthquakes in the Philippines
Surigao Del Sur
La Union
Benguet
Pangasinan
Pampanga
Tarlac
Ifugao
Davao Oriental
Nueva Vizcaya
Nueva Ecija
Top ten provinces at risk to earthquake-induced shallow landslides in the Philippines
Ifugao
Lanao Del Sur
Sarangani
Benguet
Mountain Province
Bukidnon
Aurora
Davao del Sur
Davao Oriental
Rizal
Top ten provinces at risk to volcanic eruptions in the Philippines
Camiguin
Sulu
Biliran
Albay
Bataan
Sorsogon
South Cotabato
Laguna
Camarines Sur
Batanes
Top ten provinces at risk to tsunamis in the Philippines
Sulu
Tawi-tawi
Basilan
Batanes
Guimaras
Romblon
Siquijor
Surigao del Norte
Camiguin
Masbate
Magma chambers are found beneath volcanic mountains, such as Mount Fujiyama in Japan or Mauna Loa in Hawaii.