Seismicity had returned to baseline levels, no significant deformation had been detected since August 2016, sulfur dioxide emissions were low, and no steaming had been observed since 29 September 2016. The Alert Level was lowered to 0 (on a scale of 0-5), though the public was warned to not enter the 4-km-radius Permanent Danger Zone (PDZ). [less]

(Source: Smithsonian / USGS Weekly Volcanic Activity Report 20-26 July 2016) [less]

According to PHILVOLCS, the eruption which lasted less than 30 minutes was entirely steam-driven (phreatic or hydrothermal), i.e. caused by overheated ground water flashing into steam inside the hydrothermal system overlying a (probably small) body of magma, but no magma itself was projected to the surface.
A small plume of ash rose approx. 400 m and caused minor ash fall in San Miguel, Gintubdan and Araal in La Carlota, Negros Occidental. [less]

Light ash falls occurred in areas northwest from the volcano in up to 35 km distance including Bago City. Whether the explosions were caused by fresh (juvenile) magma that had risen or were the result of overheated ground water flashing to steam (phreatic explosions) is impossible to say without a more detailed analysis of the erupted ash.
The volcano has been showing signs of unrest for several months, including slight inflation of the edifice and increased earthquake activity. A nearby magnitude 3.0 quake was felt on 18 March and might have a relation with the new volcanic activity as well. [less]

According to PHILVOLCS, this explosive activity was followed by increased seismicity and volcanic tremor probably caused by degassing.
An exclusion zone of 4 km radius around the crater was put in place, to prevent similar accidents as when 3 climbers were killed by a sudden explosion in the 1990s. [less]

According to PHILVOLCS, the Philippine volcano monitoring agency, the cracks were caused by the earthquake and are not likely a precursor for a new eruption, which would be the first since 2006, although Canalon is one of the country's most active volcanoes. A more detailed investigation is planned and the mountain was for now closed for climbers.
Erik Klemetti on his more detailed post on Eruptions Blog mentions rightly that a major hazard from Canlaon volcano are landslides and mud flows, and that these are not necessarily related to an eruption, but can be triggered as well by heavy rain and gravitational instability caused by earthquake movements. In this context, the cracks should be examined and monitored carefully. [less]

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Source: PHILVOLCS and GVP/USGS Weekly Volcanic Activity Report 19-25 July  20

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As PHILVOLCS reports, brief periods of ash and steam emissions continue at Kanlaon Volcano.  This is a manifestation of the ongoing low-level unrest.  Alert Level 1 remains enforced.   For the latest significant event and bulletin issued, see the Chronology of Events file published by PHILVOLCS.

Weak activity continues at Kanlaon volcano: Between 3 and 12 June, 4 small phreatic explosions occurred at the summit crater of Kanlaon volcano (3 June, 10 June, 2 times on 12 June). The explosions produced mainly steam and gas as well as small quantities of ash to heights up to 1000 m. Light ash-fall occurred on the upper slopes of the volcano. An exclusion zone of 4 km around the crater is being maintained. --->more on Kanlaon volcano

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3 May, 2005:
Canlaon continues to produce mild steam and ash clouds, which rise up to around 5-700 m above the active crater and sometimes causing problems with local air traffic and shutdown of nearby airports. 

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