dolerite (diabase, microgabbro) A dark-coloured, medium-grained igneous rock which contains plagioclase feldspar of labradorite composition and pyroxene of augite or titanaugite composition as essential minerals, and magnetite, titano-magnetite, or ilmenite as accessory minerals. Red mudstone is typically altered to indurated, bluish-gray hornfels with clots or crystals of tourmaline or cordierite. Formation of Diabase is explained below: Diabase forms when molten igneous rock is squeezed up into a vertical crack in other rocks, the crack is usually forced apart and the molten rock cools in the space to form a tabular igneous intrusion cutting across the surrounding rocks and is known as a dike. Figure 3: The diabase in close-up. When they are found on rocks on the continent, it suggests that the continental crust at that location at one point rifted apart at a divergent boundary, allowing the iron-rich mantle below the rift to melt, rise up to fill the breaks in the continental rocks, and cool to leave this rock behind. You might notice some fractures cutting through the rock as well. Description: The small sizes of the dark minerals in the diabase suggest this rock must have cooled quickly; otherwise the minerals would have had time to grow larger. The grain size of diabase is on the smaller side. The longer the molten magma is allowed to cool, the larger the minerals in the resulting rock become. Visiting Students Diabase cools moderately quickly when magma moves up into fractures and weak zones below a volcano. Diabase dikes are found all along the East Coast of North America. It cools under basaltic volcanoes, like those at mid-ocean ridges. Later the magma with the large phenocrysts moved upward quickly, causing more rapid cooling of the rest of the magma and the formation of the small crystals that make up the rest of the rock. In diabase, poorly formed pyroxene crystals wrap around or mold against long, rectangular plagioclase crystals to give it the characteristic texture known as diabasic or ophitic. In the United States, a syn. Buttermilk Falls Park is location in a portion of the Palisades ridge north of the Sparkill Gap.The Palisades are located along the western shoreline of the Hudson River in southeastern New York and in north eastern New Jersey. Diabase is a rock that is very similar in texture and composition to basalt; both are very common in the oceanic crust. It cools under basaltic volcanoes, like those at mid-ocean ridges. Golden Gate National Recreation Area Diabase is a fine-grained igneous rock that would have formed when molten rock material cooled rapidly on or near the surface of the Earth. Granite and diabase are both igneous rocks that form from the cooling of magma. Diabase is a common rock type. Due to the holiday spike in coronavirus cases, most spring classes are currently online. 94123-0022, Diabase is an intrusive igneous rock with the same mineral composition as basalt. The moderate cooling rate allows small visible crystals to form in the rock. Topic. Future Students a fine-grained igneous rock. Minor amounts of hornblende, olivine, magnetite, and quartz can be found in some diabase rocks. Diabase is a synonym of dolerite. Diabase is subsurface volcanic rock formed by injecting gabbroic magma or lava as shallow dykes and sills under the surface of the Earth. About one-third to two-thirds of the rock is calcium-rich plagioclase feldspar; the remainder is mostly pyroxene or hornblende. Diabase cools moderately quickly when magma moves up into fractures and weak zones below a volcano. Diabase is similar to these topics: Variolite, Volcanic rock, Gabbro and more. The dark colors of the minerals in diabase indicate that they contain a high concentration of iron and magnesium, which are elements that are common on Earth, but that are not common in the continental crust. Streak is the color of rock when it is crushed or powdered. From: Platinum-Nickel … Laboratory experiments have demonstrated that when molten rock material cools quickly, minerals in the resulting rock are very small, often microscopic. It grades to basalt when it solidifies rapidly and to gabbro when more time is given to the crystals to grow. Instead, the basaltic magma cooled slowly in fractures under the seafloor. Recent Examples on the Web It’s made of diabase traprock, which contains iron that causes the cliffs to look lumpen and rusty in the wrong light, precise and resplendent in the right one. The quarry where we found the diabase considers it a waste rock, as they are more interested in the granite that it cuts through. The magma cooled quickly to form the diabase dikes. Diabase is a subvolcanic rock equivalent to volcanic basalt or plutonic gabbro. It can include microgabbro, basalt, andesite, microdiorite and other rock types. As nouns the difference between diabase and dolerite is that diabase is (geology) a fine-grained igneous rock composed mostly of pyroxene and feldspar while dolerite is (geology) a fine-grained basaltic rock. Why does the diabase have large and small crystals? Iron and magnesium are very common inside the Earth and in the oceanic crust. The crystals formed diabase can be seen with naked eyes but in some conditions porphyritic rocks in which their basaltic combination is pyroxene or especially plagioclase phenocrysts stones can be named as diabase. Fractures formed in the granite were later filled by molten rock (magma). Luster of Diabase is not available. This boulder is dark gray to black and has a rough, rectangular prism shape. If you plan to dig a well in our area, look for outcrops of this black rock and dig your well in to the diabase in order to have a good supply of water. The term “microgabbro” is sometimes used to refer to such rocks. Sedimentary rocks within about 300 m (984 ft) above and 200 m (656 ft) below major diabase sheets are thermally metamorphosed. When molten rock cools slowly, crystals can form. Diabase (also known as dolerite or microgabbro) is an igneous rock that is often blue in colour. Dolerite is a synonym of diabase. Diabase is an intrusive igneous rock with the same mineral composition as basalt. All words formed from diabase by changing one letter The streak of Diabase is black whereas its fracture is conchoidal. In diabase, poorly formed pyroxene crystals wrap around ormold against long, rectangular plagioclase crystals to give it the characteristic texture known asdiabasic or ophitic. Diabase dikes occur in regions of crustal extension and often occur in dike swarms of hundreds of individual dikes or sills radiating from a single volcanic center. Diabase is not commercially viable for construction purposes because of how dense it is, due to the high content of iron. Alumni The high density means that when sand from these rocks is incorporated into cement, it sinks out of the mixture, resulting in poor-quality concrete. dolerite; Translations . How would a geologist figure out how it … When they cool from molten to a solid, both contract strongly. Because of how easily diabase cracks, in the Piedmont it is a major aquifer stone, storing and transmitting an incredible amount of groundwater under our feet. There, it forms dikes (tabular igneous rock bodies that cut across pre-existing rock layers or bodies) or sills (tabular igneous rock bodies that form parallel to pre-existing rock layers). Formed when magma penetrates existing rock, crystallizes and solidifies underground to form intrusions, for example plutons, batholiths, dikes, sills, laccoliths, and volcanic necks. This contraction causes the rock to break in a particular pattern called “columnar jointing.” The unique shape of the diabase boulder (a rectangular prism) is a result of breaking through columnar jointing. In the United States, an intrusive rock whose main components are labradorite and pyroxene and that is characterized by ophitic texture. These igneous rocks formed as Virginia’s crust thinned and ripped apart, labor pains at the birth of the Atlantic Ocean. Igneous rock with some large crystals among the smaller crystals is called a porphyry. Diabase dikes occur in regions of crustal extension and often occur in dike swarms of hundreds of individual dikes or sills radiating from a single volcanic center. Diabase or dolerite or microgabbro is a mafic, holocrystalline, subvolcanic rock equivalent to volcanic basalt or plutonic gabbro. Current Students Some 195 million years later William & Mary alum R. Lee Aston (’50) began quarrying diabase (black granite in the trade) for dimension stone near Rapidan. There, it forms, Igneous rock with some large crystals among the smaller crystals is called a. The different crystal sizes are the result of different rates of cooling as the magma body moved upward. Likewise, the soil formed from these rocks does not readily transmit or soak up water. Figure 5: Two images of sides of different diabase boulders. In fact, our diabase was formed in response to the stretching and eventual breakup of the supercontinent Pangea, and the opening of … Granite is an example of a felsic intrusive rock, while gabbro and diabase are examples of mafic intrusive rocks. Black ballpoint pen for scale. The hardness of Diabase is 7 whereas its compressive strength is 225.00 N/mm 2. Diabase is an intrusive igneous rock. Diabase dikes occur in regions of crustal extension and often occur in dike swarms of hundreds of individual dikes or sills radiating from a single volcanic center. Building 201, Fort Mason Diabase and gabbro have the same general mineral composition as basalt, but they have a larger grain size. A second rock type commonly occurs in the Triassic basins. Military & Veterans Dolerite and the synonym diabase are not root names but usually defined as medium grained mafic intrusive rocks. There is a surface pattern that shows how the iron-rich and crumbly diabase is continuing to break down through weathering. diabase (countable and uncountable, plural diabases) A fine-grained igneous rock composed mostly of pyroxene and feldspar. At Schoodic Point, the granite was formed first as one large mass. Diabase Dike Diabase dikes, such as the one pictured in Gwinnett County, are composed of a fine-grained igneous rock. You can see that the boulders have a roughly rectangular prism shape, which is due to how this rock contracts (and therefore breaks) as it cools from molten lava. i. Diabase typically has a mineral composition that is dominated by the plagioclase feldspar known as labradorite (approximately 40% to 70% of the rock). In Franciscan rocks, diabase formed from magma (molten rock) that didn’t erupt into seawater. Rocks found in the Palisades are known as diabase and were formed during the Triassic period around 200 million years ago. Diabase. Other interesting information? The Palisades Sill which makes up the New Jersey Palisades on the Hudson River, near New York City, is an example of a diabase sill. It cools under basaltic volcanoes, like those at mid-ocean ridges. Synonyms . Diabase cools moderately quickly when magma moves up into fractures and weak zones below a volcano. Dikes and sills in igneous rock are often made of diabase.. References Hybrid courses will transition to include face-to-face instruction on or after January 19. They are considered evidence of the rifting that broke Pangaea apart about 275 million years ago. They were formed between 180 and 230 million years ago as rifts opened in the Atlantic Ocean basin. Early Jurassic activity resulted in the formation of dolerite intrusion on Prospect Hill in Sydney, and quarrying of basalt for roadstone and other building materials has been an important activity there for over 180 years. Figure 2: One of two diabase boulders located at Southern Wake Campus. Diabase is usually found in smaller relatively shallow intrusive bodies such as dikes and sills. Diabase is an intrusive igneous rock with the same mineral composition as basalt. The large crystals, called phenocrysts, in diabase are feldspar crystals that grew as the magma cooled slowly deep in a magma chamber. The molten rock (magma) crystallizes as it cools, the most common dike rocks being diabase (or dolerite), basalt, and fine-grained granitic rocks. Diabase is actually a variety of gabbro which consists mainly of labradorite feldspar, augite, magnetite, and olivine. Businesses Note that no distinct minerals are visible. DIABASE, in petrology, a rock which is a weathered form of dolerite. Diabase was formed when magma from the earth’s interior penetrated into cracks in the primary rock and then solidified. Community It is rich in magnesium and iron, and originally found under the crust of volcanoes. List all words starting with diabase, words containing diabase or words ending with diabase. Figure 4: Another close-up of the surface of the diabase, showing the dark colors of the microscopic minerals. The USGS has a good set of graphics on their website. How did it form? Most of the remainder is made up of pyroxene minerals (usually augite). Diabase is subsurface volcanic rock formed by injecting gabbroic magma or lava as shallow dykes and sills under the surface of Earth. San Francisco, CA Diabase is typically fine grained having chilled margin. Diabase definition is - diorite. Parents Sedimentary rocks are formed by the gradual consolidation of organic or inorganic solid fragments, carried by, suspended in, or dropped by wind, water, or ice and deposited horizontally in layers. Words formed from any letters in diabase, plus an optional blank or existing letter. Diabase is a hypabyssal rock that is interspersed throughout the primary rock in Sweden. It occurs mostly in shallow intrusions (dikes and sills) of basaltic composition. Figure 1: The diabase boulder at Northern Wake Campus. Diabase tends to be found in long vertical sheets called dikes that cut through other, more common continental rocks. Luster of Diabase is the interaction of light with the surface of Diabase. Photograph by Pamela J. W. Gore Diabase is a fine-grained igneous rock that would have formed when molten rock material cooled rapidly on or near the surface of the Earth. Diabase in the map area was derived primarily from high-titanium, quartz-tholeiite magma. The Palisades Sill which makes up the New Jersey Palisades on the Hudson River, near New York City, is an example of a diabase sill. of diabase Ref: AGI Unique features to look for: Very fine grains, very dark color. The only place on Earth that is cool enough for rapid cooling like this is near the surface of the Earth, so the diabase must have erupted from a volcano before it cooled to become a rock. Diabases mostly formed with the composition of plagioclase feldspar ( mostly labrador ) and pyroxenes ( augite ). Employees, © 2020 Wake Technical Community College | 9101 Fayetteville Road, Raleigh, North Carolina 27603 | Main Tel: 919-866-5000. How would a geologist figure out how it formed using rock characteristics? The age of the diabase in our region has been determined quite precisely; it is almost exactly 200 Ma (million years old). Diabase. Where does diabase form? It is an igneous rock called diabase that is Jurassic in age, younger than the Triassic sedimentary rocks. The diabase has been compressed by the surrounding … Despite its high density, diabase has a very important role to play in North Carolina geology.