Luck Stone - Construction Aggregates

Virginia
Crushed Stone

Bealeton

Berkley Yard

Boscobel

Bull Run

Burkeville

Charlottesville

Culpeper

Fairfax

Gilmerton Yard

Goose Creek

Greene

Leesburg

Massaponax

Powhatan

Rockville

South Richmond

Spotsylvania

Sand & Gravel

Caroline

North Carolina
Crushed Stone

Pittsboro

Massaponax
7730 Jefferson Davis Hwy
Fredericksburg, Virginia 22407

Sales Representative:
Randy Hartman
Phone: (540) 898-3116
Fax: (540) 898-5228

E-mail Randy Hartman

The Massaponax plant has temporarily suspended operations.

We remain committed to providing our Massaponax customers with the highest level of quality products and services from our Spotsylvania location during this suspension. To inquire about our products and services or to schedule a shipment, please contact us at (540) 898-3116.

Thank you for choosing Luck Stone. We appreciate you allowing us to fulfill your crushed stone needs.

The Massaponax Plant is located on Route 1 south of Fredericksburg in Massaponax and is across from Massaponax High School. Production was initiated Massaponax in 2005 and services the growing residential and business communities on the fringes of Northern Virginia.

For the Homeowner: A Guide to Buying Crushed Stone

Areas Served: Counties of Spotsylvania, Louisa, and, Caroline and the City of Fredericksburg.

Luck Stone Credit Application


	Granite Crushed Stone PDF



	The rock quarried for construction use is a complex blend of igneous and metamorphic rock types. It is referred to as the Po River Metamorphic Suite, the term suite meaning more than one type and metamorphic meaning changed from original composition. The overall rock types are granite-gneiss and biotite-gneiss. Many other intrusions of igneous rocks occurred over time in the Po River Complex making it difficult to date as a unit, but some dating has shown rock older than 410 million years. The granite-gneiss can yield a white to gray color stone while the biotite-gneiss can yield dark gray to black stone. One of the later igneous intrusions is distinctly different in appearance- a reddish granite with large mineral crystals that contrast with the surrounding stone. The geologic events that metamorphosed pre-existing rocks and allowed intrusions by magmas were tectonic events involving the movement of continents; collisions of continents causing metamorphism and their separating allowing magmas to rise from below and intrude existing rock.