AGGREGATES
Aggregate material
Rattlesnake Redstone in Idaho is formed from iron-rich natural rock deposits created over millions of years through volcanic activity, mineral oxidation, and geological pressure. The stone’s distinctive red and rust-colored tones come from naturally occurring iron minerals within the rock. After being quarried from local Idaho deposits, the stone is crushed and screened to create a decorative landscape rock known for its bold color variation and rugged natural appearance.
Summer Glacier Cobble is naturally formed from stone deposits shaped over thousands of years by glacial movement, river flow, and weathering throughout the region. As the rock was carried by water and ice, the stones became smooth and rounded while developing soft natural color variation inspired by glacier tones.
Rattlesnake Red Boulders are formed from iron-rich volcanic and sedimentary rock deposits shaped over millions of years through geological pressure, mineral oxidation, and weathering. Their distinctive red and rust-colored tones come from naturally occurring iron minerals within the stone.
Brown Painted Mulch in Idaho is produced from recycled wood materials that are ground into mulch and color-enhanced using environmentally safe dyes. The wood is processed into consistent pieces, cleaned of debris, and treated to create a rich brown color designed to maintain its appearance over time. Made from natural wood products, brown painted mulch offers a uniform texture and long-lasting color inspired by Idaho’s natural landscapes.
Kinnikinic Creek Cobble in Idaho is naturally formed through centuries of water movement, erosion, and geological weathering in mountain streams and creek beds. As water flows over the stone, the rocks are gradually smoothed and rounded into naturally shaped cobbles with unique color variation and texture. Sourced from Idaho deposits, the material is cleaned and sorted by size to create a durable decorative stone with a naturally polished appearance.
Malad Brown Stone in Idaho is formed from natural rock deposits created over millions of years through volcanic activity, mineral-rich sediment buildup, and geological pressure. The stone’s warm brown tones developed naturally from iron and mineral content within the rock over time.
Large Boulders in Idaho are naturally formed over millions of years through volcanic activity, mountain uplift, erosion, and geological weathering. As rock formations broke apart and were shaped by natural forces such as water, ice, and pressure, massive stone pieces developed their rugged texture and unique appearance.
Black Painted Mulch is made from recycled wood materials that are ground into mulch and treated with environmentally safe black coloring. The wood is processed into uniform pieces and cleaned before being color-enhanced to create a bold, consistent appearance. Produced from natural wood products sourced in the region, black painted mulch delivers rich color contrast and a clean finished look inspired by Idaho’s rugged landscape.
In Idaho, ballast rock is formed from natural volcanic and sedimentary stone deposits that developed over millions of years through lava flows, mountain uplift, and geological pressure. Much of the region’s rock comes from ancient volcanic activity that created dense, durable stone ideal for crushing. The rock is quarried from local deposits, then crushed, screened, and cleaned into angular pieces to produce high-quality ballast rock with consistent size and strength.
Snake River Plain Cobble is formed from volcanic rock deposits shaped over thousands of years by the movement of the Snake River and regional geological activity. As the river carried and rolled the stone downstream, the rocks became naturally rounded and smoothed through erosion and water flow.
Malad Greystone is formed from dense natural stone deposits created over millions of years through volcanic activity, mineral compression, and geological weathering. The stone’s natural gray tones and rugged texture developed through layers of pressure and erosion unique to the region.
Black Lava Rock Nuggets are formed from ancient volcanic lava flows that cooled rapidly and hardened into lightweight, porous stone. As molten lava cooled on the earth’s surface, trapped gases created the rock’s distinctive texture and natural black coloring. Sourced from Idaho volcanic deposits, the rock is crushed and sorted into nugget-sized pieces that highlight its rugged appearance and unique volcanic character.
In Idaho, washed rock is produced from natural stone deposits shaped over millions of years by volcanic activity, mountain erosion, and river movement. Rock is quarried from local deposits and crushed into various sizes before being thoroughly washed to remove dirt, dust, and fine materials. This process reveals the stone’s natural color and texture while creating a clean, durable rock product with a consistent appearance.
Challis Ledger Rock is formed from natural stone deposits created over millions of years through volcanic activity, sediment buildup, and geological pressure in the Challis region. Over time, the rock developed into layered formations that naturally break into flat, stacked pieces known as ledger stone.
Basalt Boulders are formed from ancient volcanic lava flows that cooled and hardened into dense, durable stone over millions of years. As the volcanic rock weathered and broke apart through natural geological processes, large basalt formations developed their rugged texture and dark natural coloring.
Small Chunk Bark in Idaho is made from natural wood bark collected during the milling and processing of regional timber. The bark is screened and processed into smaller, consistent pieces while maintaining its natural texture and rich wood tones.
Need options in pocatello OR IDAHO FALLS?
Click the link below!