SIMPANG PULAI MARBLE
Marble rock in Thematic 4 originates from Simpang Pulai , Kinta valley. These limestones deposit have evolved over millions of years by gradually accumulating marine sediments rich in calcium carbonate. The formation of this marble rock can be traced back to the Devonian period, spanning from approx...
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2025
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oai:utpedia.utp.edu.my:302382025-02-14T07:16:32Z http://utpedia.utp.edu.my/id/eprint/30238/ SIMPANG PULAI MARBLE Instructional Teaching Materials Marble rock in Thematic 4 originates from Simpang Pulai , Kinta valley. These limestones deposit have evolved over millions of years by gradually accumulating marine sediments rich in calcium carbonate. The formation of this marble rock can be traced back to the Devonian period, spanning from approximately 419 million to 359 million years ago, reflecting the intricate natural processes that have shaped the Kinta Valley landscape. 2025-01 Instructional Teaching Materials NonPeerReviewed image en http://utpedia.utp.edu.my/id/eprint/30238/1/R3-2.jpg Instructional Teaching Materials (2025) SIMPANG PULAI MARBLE. [Instructional Teaching Materials] https://youtu.be/3MiWLSGPdeg?si=dodpriR33QGuQMOv |
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Marble rock in Thematic 4 originates from Simpang Pulai , Kinta valley. These limestones deposit have evolved over millions of years by gradually accumulating marine sediments rich in calcium carbonate. The formation of this marble rock can be traced back to the Devonian period, spanning from approximately 419 million to 359 million years ago, reflecting the intricate natural processes that have shaped the Kinta Valley landscape. |
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Instructional Teaching Materials |
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Instructional Teaching Materials |
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Instructional Teaching Materials SIMPANG PULAI MARBLE |
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SIMPANG PULAI MARBLE |
title_short |
SIMPANG PULAI MARBLE |
title_full |
SIMPANG PULAI MARBLE |
title_fullStr |
SIMPANG PULAI MARBLE |
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SIMPANG PULAI MARBLE |
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simpang pulai marble |
publishDate |
2025 |
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http://utpedia.utp.edu.my/id/eprint/30238/1/R3-2.jpg http://utpedia.utp.edu.my/id/eprint/30238/ https://youtu.be/3MiWLSGPdeg?si=dodpriR33QGuQMOv |
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