Showing posts with label igneous rocks. Show all posts
Showing posts with label igneous rocks. Show all posts

Friday, April 3, 2026

The rock formation along the highway in San Jose, Dulag, Leyte

Have you ever wondered about the rock along the highway in San Jose, Dulag, Leyte? Especially where the road runs close to the sea, travelers see a striking, dark-colored rock formation exposed by the ongoing road widening. 

The andesite rock along the highway in San Jose, Dulag, Leyte

Formed by volcanism between 2.6 and 23 million years ago during the Miocene and Pliocene epochs, this rock in Dulag is known as andesite. Andesite is an intermediate type of volcanic rock, with silica (SiO2) content ranging between 52% and 63%, commonly found in areas with past or present volcanic activity. 

The Dulag andesite belongs to the Pliocene-Miocene intermediate rocks (Jahn & Asio, 2006)

Andesite got its name from the Andes Mountains in South America, where it is abundant. It is also widespread in volcanic regions around the world, especially along the Pacific Ring of Fire, where many volcanoes produce this type of rock. It is an extrusive (volcanic type) and the most widespread igneous rock in the Philippines. 

Andesite typically appears fine-grained, sometimes with small visible crystals embedded in it called phenocrysts. These crystals are often made of minerals like feldspar and dark-colored minerals such as pyroxene or biotite. Because of this, andesite can look gray, pinkish, or slightly dark, depending on its composition. 

Mineral composition of the andesite in Abuyog: Amp- amphibole; Cpx- clinopyroxene;
Opq-opaque minerals; Pl-plagioclase feldspar

Laboratory examination of thin sections using a petrographic microscope (above photo) revealed that the andesite in Dulag, Leyte, consists primarily of plagioclase feldspar (45% of the mineral content), clinopyroxene (20%), and amphibole (5%), along with minor amounts of secondary minerals. It is darker in color compared to the younger andesite rocks (Quaternary volcanics) in the central highlands of Leyte.

The typical andesite rock in the central highlands of Leyte formed by volcanism during the Quaternary period (2 million years ago up to the present). The sample comes
from Cabintan, Ormoc at an elevation of 900 m above sea level.

Acknowledgement

I thank the National Institute of Geological Sciences (NIGS) at UP Diliman for conducting the thin section analysis of my rock samples.

References

Britannica Editors. "andesite". Encyclopedia Britannica, 5 Jul. 2015, https://www.britannica.com/science/andesite. Accessed 3 April 2026.

Jahn, R., & Asio, V. B. (2006). Climate, geology and soils of the tropics with special reference to Southeast Asia and Leyte (Philippines). In Proceedings of the 11th International Seminar-Workshop on Tropical Ecology (pp. 21-25).





Tuesday, March 31, 2026

The Rock, Mineral, and Soil Collection at VSU: An essential Instructional Resource

The Rock, Mineral, and Soil Collection at the Pedology and Geoecology Laboratory of the Department of Soil Science, Visayas State University, Baybay City, is a popular educational attraction for students in Eastern Visayas. It contains hundreds of specimens, including different types of rocks (igneous, metamorphic, sedimentary), minerals (e.g. quartz, feldspar, calcite, amethyst, jade, jasper, mica, pyrite, etc), as well as sands and soils collected from different places in the Philippines and abroad. It is the only one of its kind in the Visayas and Mindanao.



In 2026, new additions to the collection include red sandstones from Utah (USA), peridotite and andesite rocks from Eastern Samar and Southern Leyte, and various mineral specimens donated by some alumni of the department.

Soil samples from across the Philippines are also on display. The collection is an essential resource for the teaching of soil science, agricultural science, environmental science, and earth science. Most soils (except peat soils) originate from weathered rocks, and the mineral composition of these rocks strongly affects soil properties and fertility. Rocks also serve as a source of nutrients that are gradually released into the soil through weathering.

A few of the many igneous rocks in the collection


Some of the metamorphic rocks on the display in the collection


Some samples of sedimentary rocks in the collection

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Note: The Rock, Mineral, and Soil Collection was established and is maintained by Dr. V.B. Asio. For more information or if you want to visit it, please email him at: vbasio@vsu.edu.ph