Open Access Open Access  Restricted Access Subscription Access
Open Access Open Access Open Access  Restricted Access Restricted Access Subscription Access

Morphology of the Volcanic Ash from the Kukadi River Section, Pune District, Maharashtra


Affiliations
1 Department of Geology, University of Pune, Pune-411 007, India
2 Deccan College, Pune-411 006, India
     

   Subscribe/Renew Journal


An ash bed varying in thickness from 20 cm to 2 m occurs within the lower part of 10 m thick yellowish-brown clay and calcareous silt unit that contains occasional lenses of calcrete, gravels and channel lag gravels both at the base and top of the sequence. The volcanic ash has yielded a K/Ar age of 1.4 Ma. The volcanic ash is highly siliceous in composition with SiO2 content varying between 72 to 78%. It is dominantly constituted of silt sized angular glass shards, and pumice fragments with sharp edges. Petrography, SEM and chemical composition of the glass shards helps in relating the ash morphology to magma composition and the type of eruption. On the basis of petrographic and morphological characters displayed by the volcanic ash, the formation of the glass shards is attributed to magmatic processes.

Keywords

Petrology, Pleistocene, Tephra, Maharashtra.
Subscription Login to verify subscription
User
Notifications
Font Size

Abstract Views: 178

PDF Views: 2




  • Morphology of the Volcanic Ash from the Kukadi River Section, Pune District, Maharashtra

Abstract Views: 178  |  PDF Views: 2

Authors

N. R. Karmalkar
Department of Geology, University of Pune, Pune-411 007, India
S. N. Ghate
Deccan College, Pune-411 006, India
Shiella Mishra
Deccan College, Pune-411 006, India
S. N. Rajaguru
Deccan College, Pune-411 006, India

Abstract


An ash bed varying in thickness from 20 cm to 2 m occurs within the lower part of 10 m thick yellowish-brown clay and calcareous silt unit that contains occasional lenses of calcrete, gravels and channel lag gravels both at the base and top of the sequence. The volcanic ash has yielded a K/Ar age of 1.4 Ma. The volcanic ash is highly siliceous in composition with SiO2 content varying between 72 to 78%. It is dominantly constituted of silt sized angular glass shards, and pumice fragments with sharp edges. Petrography, SEM and chemical composition of the glass shards helps in relating the ash morphology to magma composition and the type of eruption. On the basis of petrographic and morphological characters displayed by the volcanic ash, the formation of the glass shards is attributed to magmatic processes.

Keywords


Petrology, Pleistocene, Tephra, Maharashtra.