WASH Cluster – Groundwater Development and Drilling GWD1 Handout GWD1 – Occurrence TABLE OF ROCK TYPES AND POROSITY Aquifer category Crystalline Basement Volcanic rocks Consolidated sedimentary rocks Unconsolidated sediments Example Rock types Granite, granodiorite, gabbro Gneiss, schist, hornfels Basalts Scoria Means of Formation Arrangement of minerals Interlocking crystals Fractures Metamorphic (heat and pressure) Igneous (volcanic) Interlocking crystals Fractures Interlocking crystals Sometimes granular Rhyolite, rhyodacite, pumice Igneous (volcanic) Particles often welded together, Sometimes granular Fractures, layers between different lava flows Fractures, layers within different lava flows sometimes granular Conglomerate, sandstone, siltstone, shale Limestone Deposition of particles by rivers, sea, wind Particles compacted and cemented together Particles cemented together Coal Deposited mainly in swamps Particles bound together Gravel, sand, silt, clay Deposition of particles by rivers, sea,wind Limestone Deposition in the sea Particles generally uncompacted very little cementation Particles weakly cemented together Igneous (plutonic) Deposition in the sea Type of porosity Fractures, bedding planes (depositional layers) Fractures, bedding planes. cavities in caves and solution cracks Fractures, bedding planes Between the particles Between particles, Cavities in caves and solution cracks Aquifers are often referred to by the characteristics of the porosity. Thus: Fractured rock aquifers comprise: crystalline basement rocks , volcanic rocks and consolidated sedimentary rocks Porous media – essentially unconsolidated sedimentary aquifers such as gravel and sand as well as some non consolidated volcanic rocks such as scoria or pumice A more complex yet widespread aquifer type associated with limestone deposits and cave systems is known as “Karst”.