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Bookmark or Share- Sill (geology) - WikipediaIn geology, a sill is a tabular sheet intrusion that has intruded between older layers of sedimentary rock, beds of volcanic lava or tuff, or along the direction of foliation in metamorphic rock. A sill is a concordant intrusive sheet, meaning that it does not cut across preexisting rock beds.
- Sill plate - WikipediaSill plates are usually composed of lumber but can be any material. The timber at the top of a wall is often called a top plate, pole plate, mudsill, wall plate or simply "the plate".
- Sill | Igneous Rock, Intrusive Layer & Magma Chamber | Britannicasill, flat intrusion of igneous rock that forms between preexisting layers of rock. Sills occur in parallel to the bedding of the other rocks that enclose them, and, though they may have vertical to horizontal orientations, nearly horizontal sills are the most common.
- Sills + Co | Women's designer clothing by Caroline Sills & Sills | NZSills + Co is a curated boutique of long established and emerging New Zealand and international fashion brands alongside accessories, homeware, footwear and more. Welcome to Sills + Co. Online home of Caroline Sills and Sills.
- 9.13: Reading- Dikes and Sills - Geosciences LibreTextsIn geology, a sill is a tabular sheet intrusion that has intruded between older layers of sedimentary rock, beds of volcanic lava or tuff, or even along the direction of foliation in metamorphic rock. The term sill is synonymous with concordant intrusive sheet.
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