{"id":19469,"date":"2025-11-13T08:09:27","date_gmt":"2025-11-13T07:09:27","guid":{"rendered":"https:\/\/www.darda.de\/?page_id=19469"},"modified":"2025-11-13T08:09:27","modified_gmt":"2025-11-13T07:09:27","slug":"natural-stone","status":"publish","type":"page","link":"https:\/\/www.darda.de\/en\/knowledge\/natural-stone","title":{"rendered":"Natural stone"},"content":{"rendered":"
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Natural stone is one of the oldest and at the same time most versatile construction materials. Its origin in geological processes shapes properties such as strength, porosity, and cleavability\u2014and thus the way it is extracted, processed, installed, and deconstructed. In practice, natural stone topics touch many fields of application: from natural stone extraction<\/em> in the stone quarry<\/em> through rock excavation and tunnel construction<\/em> to building gutting and cutting<\/em> of masonry. Methods such as controlled splitting or gripping and crushing\u2014for example with hydraulic rock and concrete splitters<\/a> or concrete demolition shears<\/strong> from Darda GmbH\u2014play an important role when precise handling of rock with low vibration levels and in a material-appropriate manner is required.<\/p>\n

Definition: What is meant by natural stone<\/h2>\n

Natural stone refers to naturally formed, solid rocks without artificial binders. They are obtained as raw blocks or bulk material, mechanically processed (e.g., sawn, split, bush\u2011hammered), and used in structures, landscape architecture, civil engineering, and interior fit-out<\/em>. Natural stone includes magmatic (e.g., granite, basalt), sedimentary (e.g., limestone, sandstone), and metamorphic rocks (e.g., gneiss, marble, quartzite). The material\u2011typical combination of high compressive strength and comparatively low tensile and flexural tensile strength leads to brittle fracture behavior. These properties determine how the material can be drilled, cut, split, and broken\u2014and explain why tools for controlled splitting<\/em> and targeted gripping<\/em> are so widespread in extraction and deconstruction<\/em>.<\/p>\n

Formation and the rock cycle<\/h2>\n

Natural stone forms within the geological cycle: solidification of magmatic melts, deposition and lithification of sediments, and transformation of existing rocks under pressure and temperature. These processes produce textures (grain bonding, bedding, joints) and mineral combinations that decisively influence mechanical parameters and workability. For practice, natural zones of weakness\u2014bedding planes, joint systems, stratification\u2014are significant and can be specifically exploited during splitting<\/strong> to detach blocks with low energy input. In compact, joint\u2011poor rock, generating cracks requires peak pressures produced by hydraulic wedge and split systems.<\/p>\n

Geological classification and properties<\/h2>\n

Assigning rocks to magmatic, sedimentary, and metamorphic groups helps estimate behavior and suitable procedures. It is important not only to know the rock by name, but also to assess its bonding, grain structure, porosity, and joint distribution.<\/p>\n

Magmatic rocks<\/h3>\n

Granite, diorite, and gabbro are coarse\u2011grained, strong in compression, and often poor in joints; basalt is fine\u2011grained to dense. They are abrasive<\/em> when drilling and sawing, but respond well to wedge forces if borehole geometry and edge distance<\/em> are suitable. In massive granites, stone and concrete splitters<\/strong> with borehole wedges are a proven way to detach blocks without blasting.<\/p>\n

Sedimentary rocks<\/h3>\n

Limestone and sandstone frequently show bedding and stratification planes. Their porosity varies widely, as do frost and salt resistance. Pronounced bedding planes facilitate wedging and establishing crack lines. In mortared natural stone masonry, concrete demolition shears<\/strong> grip reliably because they engage rock pieces together with mortar joints and produce shear fractures.<\/p>\n

Metamorphic rocks<\/h3>\n

Gneiss, quartzite, slate, and marble are transformed by pressure and temperature. They possess oriented fabrics (foliation, schistosity) that define preferred splitting directions. With proper alignment of wedge forces, precise fracture edges can be produced; with unfavorable alignment, spalling may occur. A well\u2011thought\u2011out drilling pattern is particularly important here.<\/p>\n

Mechanical key values for planning and procedures<\/h2>\n

The selection of procedures and tools is guided by reliable parameters. For practice, the following are especially relevant:<\/p>\n