Boulders of various sizes are routinely sold by gravel pits, material suppliers, and landscapers. So yes, boulders of milky quartz have value.
Basalt boulders are large rocks composed of basaltic lava that solidified over time. These boulders can hold significance culturally, geologically, or aesthetically depending on the context in which they are found. They are often used for landscaping, construction, and as natural monuments due to their durability and unique appearance.
An unsorted mixture of small particles to large boulders is called a conglomerate. It is a type of sedimentary rock characterized by its diverse range of grain sizes and is typically formed through the deposition and cementation of various rock fragments.
Rocks and boulders are not the same thing, though both are solid mineral materials. A rock is a general term that refers to a natural substance composed of one or more minerals, while a boulder specifically refers to a large rock, typically defined as being greater than 256 millimeters (10 inches) in diameter. Essentially, all boulders are rocks, but not all rocks qualify as boulders.
The boulders, sand, clay, and silt that are deposited by a glacier as it slows down and melts are called glacial till. This material is unsorted and varies in size, ranging from large boulders to fine silt. Glacial till is often found as moraines, which are accumulations of debris along the edges or at the terminus of a glacier.
Quartz is extracted through a mining process where large machinery and equipment are used to extract the quartz from the earth's surface. The quartz is then crushed and separated from other minerals before being processed further for various industrial uses. mining operations can vary depending on the location and type of deposit.
Till looks like anything from fine rock, to large boulders in a cluster in which are picked up and carried by a glacier
Till looks like anything from fine rock, to large boulders in a cluster in which are picked up and carried by a glacier
Large boulders and smaller rocks can be carried by a river. When rocks and sediment are displaced, it's called erosion.
Meteors
Large boulders fell on highway 40 near Asheville, NC, causing traffic to come to a standstill. It will take several weeks to clear the boulders from the highway. Local residents must use secondary road 332 to get around Big High Mountain. There were boulders in every shape and size everywhere.
Large boulders in steep mountain streams are often the result of erosion and transportation by the powerful force of fast-flowing water. The steep gradient of the stream allows for a high energy flow that can dislodge and move large rocks downstream. These boulders can get trapped or deposited in the streambed due to the turbulent flow dynamics.
Quartz
Erratic blocks or "erratics" for short.
Lemon quartz is a large crystalline quartz wherein individual crystals are distinguishable with the naked eye. Its transparent to translucent yellow color comes from iron.
Large granite boulders form from the slow cooling and solidification of molten magma deep within the Earth's crust. As the magma cools underground, it crystallizes and forms granite, which later gets exposed at the surface through processes like erosion. Over time, weathering and erosion gradually break down the surrounding rock, leaving behind large granite boulders.
Granite is a common rock that is composed of several different minerals, such as feldspar, quartz, and mica. These minerals form large crystals and give granite its distinct speckled appearance.
You are possibly thinking of the Moeraki Boulders, on the coast about 50km north of Dunedin. These are spherical concretions up to 1.5m diameter, naturally growing in clays derived from volcanic ash. Still quietly emerging as the coast erodes. In the mountains, giant boulders are frequently found, and some are huge. The biv rock in the Upper Arawhata is several tens of metres lin each dimension. In the Troyte, a small valley off the Karangarua, (Westland) the boulders may even be seen in satellite photos! These are all ex-glacial erratics.