
Focus vs epicenter; intensity vs magnitude and active vs inactive fault Self Assessment
Quiz by Angelica Tamang
Feel free to use or edit a copy
includes Teacher and Student dashboards
Measure skillsfrom any curriculum
Tag the questions with any skills you have. Your dashboard will track each student's mastery of each skill.
- edit the questions
- save a copy for later
- start a class game
- automatically assign follow-up activities based on students’ scores
- assign as homework
- share a link with colleagues
- print as a bubble sheet
- Q1
In general, the shallow-focus earthquakes cause mass destruction than deep-focus earthquakes because the seismic waves travel at shorter distance from the focus to the surface. Which of the following is NOT true of the focus of an earthquake?
It is the starting point of the earthquake
It is above the epicenter.
It is where the first break in the rock happens.
It is where the first movement takes place.
60s - Q2
What scale is used to measure the magnitude of an earthquake?
Modified Mercalli Scale
Epicenter Scale
Focus scale
Richter scale
60s - Q3
What intensity of the earthquake based on PHIVOLCS intensity scale is slightly felt?
Intensity I
Intensity III
Intensity II
Intensity IV
60s - Q4
Which of the following pairs of magnitude and general description is NOT true?
6:Very Strong
4: Moderately Strong
2:Devastating
8:VeryDestructive
60s - Q5
At 4:16 AM on27 July 2019, Saturday, a Magnitude 5.4 earthquake shook the Batanes Islands. Its epicenter is located 12 km North of Itbayat, Batanes and originated a depth of 12 km. At 7:37 AM, an earthquake with magnitude 5.9 occurred 21 km North of Itbayat, Batanes at a depth of 7 km. At 9:24, a magnitude 5.8 earthquake occurred, located 11 km North of Itbayat, Batanes with a depth of 11 km. Each event was followed by small-magnitude earthquakes. As of 8:00 PM of 27 July2019, 104 aftershocks have been recorded by the DOST-PHIVOLCS seismic monitoring network. The magnitude 5.4 earthquake generated ground shaking felt at PHIVOLCS earthquake Intensity Scale (PEIS) VI (Very Strong) in Itbayat,Batanes. Intensity III (Weak) was also felt in Basco and Sabtang, Batanes. The larger magnitude 5.9 earthquake generated stronger shaking felt at intensityVII (Destructive) in Itbayat, Batanes, and Intensity IV (Moderately Strong) in Sabtang and Uyugan, Batanes. Both ground shaking events resulted to casualties and damages to buildings and infrastructure near the epicentral area. In addition to the type of building materials used, these earthquake events could have weakened the buildings and structures prior to the M5.9 earthquake event, resulting in greater damage than would have been expected. Prior to the moderated-sized earthquakes on July 27, earthquakes with magnitudes ranging from4.2 to 4.8 occurred from July 22-26, 2019. The maximum reported ground shaking intensity was IV. Where is the epicenter of the earthquake?
Itbayat, Batanes
Sabtang, Batanes
Basco, Batanes
Uyugan, Batanes
300s - Q6
At 4:16 AM on27 July 2019, Saturday, a Magnitude 5.4 earthquake shook the Batanes Islands. Its epicenter is located 12 km North of Itbayat, Batanes and originated a depth of 12 km. At 7:37 AM, an earthquake with magnitude 5.9 occurred 21 km North of Itbayat, Batanes at a depth of 7 km. At 9:24, a magnitude 5.8 earthquake occurred, located 11 km North of Itbayat, Batanes with a depth of 11 km. Each event was followed by small-magnitude earthquakes. As of 8:00 PM of 27 July2019, 104 aftershocks have been recorded by the DOST-PHIVOLCS seismic monitoring network. The magnitude 5.4 earthquake generated ground shaking felt at PHIVOLCS earthquake Intensity Scale (PEIS) VI (Very Strong) in Itbayat,Batanes. Intensity III (Weak) was also felt in Basco and Sabtang, Batanes. The larger magnitude 5.9 earthquake generated stronger shaking felt at intensityVII (Destructive) in Itbayat, Batanes, and Intensity IV (Moderately Strong) in Sabtang and Uyugan, Batanes. Both ground shaking events resulted to casualties and damages to buildings and infrastructure near the epicentral area. In addition to the type of building materials used, these earthquake events could have weakened the buildings and structures prior to the M5.9 earthquake event, resulting in greater damage than would have been expected. Prior to the moderated-sized earthquakes on July 27, earthquakes with magnitudes ranging from 4.2 to 4.8 occurred from July 22-26, 2019. The maximum reported ground shaking intensity was IV. What is/are the effects of earthquake on buildings?
buildings near the epicenter were not damaged
buildings away the epicenter were damaged
buildings away the epicenter were weakened
buildings near the epicenter were damaged
120s - Q7
___________ is a fault that has NOT moved for more than 10,000 years.
tsunamis
earthquakes
inactive fault
active fault
60s - Q8
_________________ is a fault that will likely have another displacement or cause an earthquake sometime in the future.
tsunamis
earthquakes
active faults
inactive faults
60s - Q9
Is there a possibility that an inactive fault becomes an active fault?
No, an inactive fault is already inactive.
No, scientists have already considered it inactive.
Yes, depending on weather patterns.
Yes, an inactive fault can still be considered an active fault in the future.
60s - Q10
Which of the following active faults is nearest Marikina City?
Lubang Fault
Valley Fault System
Philippines Fault Zone
Digdig Fault
60s