Umbilicaria Mammulata
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Umbilicaria Mammulata
''Umbilicaria mammulata'', or smooth rock tripe, is a foliose lichen found on boulders and rock walls. Description ''Umbilicaria mammulata'' is among the largest lichens in the world. The thallus of ''U. mammulata'' is usually in diameter, but specimens have been known to reach in the Smoky Mountains of Tennessee. The smooth upper surface is a reddish-brown to grayish-brown color and the lower surface is pitch black. Ecology This species is found on boulders and steep rock walls in forests and around lakes. It grows on several types of rock substrate, such as acidic rock, sandstone, quartz, and granitic rock.Wisconsin State Herbarium, "Wisconsin Vascular Plants: Details Page." http://www.botany.wisc.edu/Wislichens/scripts/detail.asp?SpCode=UMBMAM (accessed Dec 19, 2008). Like most lichens, ''U. mammulata'' is sensitive to air and water quality. If conditions are optimal, seeing rocks or cliffs covered in dinner plate-sized thalli is not unusual. However, it has been s ...
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Appalachians
The Appalachian Mountains, often called the Appalachians, (french: Appalaches), are a system of mountains in eastern to northeastern North America. The Appalachians first formed roughly 480 million years ago during the Ordovician Period. They once reached elevations similar to those of the Alps and the Rocky Mountains before experiencing natural erosion. The Appalachian chain is a barrier to east–west travel, as it forms a series of alternating ridgelines and valleys oriented in opposition to most highways and railroads running east–west. Definitions vary on the precise boundaries of the Appalachians. The United States Geological Survey (USGS) defines the ''Appalachian Highlands'' physiographic division as consisting of 13 provinces: the Atlantic Coast Uplands, Eastern Newfoundland Atlantic, Maritime Acadian Highlands, Maritime Plain, Notre Dame and Mégantic Mountains, Western Newfoundland Mountains, Piedmont, Blue Ridge, Valley and Ridge, St. Lawrence Valley, Appalac ...
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Granitic Rock
A granitoid is a generic term for a diverse category of coarse-grained igneous rocks that consist predominantly of quartz, plagioclase, and alkali feldspar. Granitoids range from plagioclase-rich tonalites to alkali-rich syenites and from quartz-poor monzonites to quartz-rich quartzolites. As only two of the three defining mineral groups (quartz, plagioclase, and alkali feldspar) need to be present for the rock to be called a granitoid, foid-bearing rocks, which predominantly contain feldspars but no quartz, are also granitoids. The terms ''granite'' and ''granitic rock'' are often used interchangeably for granitoids; however, granite is just one particular type of granitoid. Granitoids are diverse; no classification system for granitoids can give a complete and unique characterization of the origin, compositional evolution, and geodynamic environment for the genesis of a granitoid. Accordingly, multiple granitoid classification systems have been developed such as those based on ...
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Lichens Of Europe
A lichen ( , ) is a composite organism that arises from algae or cyanobacteria living among filaments of multiple fungi species in a mutualistic relationship.Introduction to Lichens – An Alliance between Kingdoms
. University of California Museum of Paleontology.
Lichens have properties different from those of their component organisms. They come in many colors, sizes, and forms and are sometimes plant-like, but are not s. They may have tiny, leafless branches (); flat leaf-like structures (

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Lichens Described In 1814
A lichen ( , ) is a composite organism that arises from algae or cyanobacteria living among filaments of multiple fungi species in a mutualistic relationship.Introduction to Lichens – An Alliance between Kingdoms
. University of California Museum of Paleontology.
Lichens have properties different from those of their component organisms. They come in many colors, sizes, and forms and are sometimes plant-like, but are not s. They may have tiny, leafless branches (); flat leaf-like structures (
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Lichen Species
A lichen ( , ) is a composite organism that arises from algae or cyanobacteria living among filaments of multiple fungi species in a mutualistic relationship.Introduction to Lichens – An Alliance between Kingdoms
. University of California Museum of Paleontology.
Lichens have properties different from those of their component organisms. They come in many colors, sizes, and forms and are sometimes plant-like, but are not s. They may have tiny, leafless branches (); flat leaf-like structures (

Umbilicaria
Rock tripe is the common name for various lichens of the genus ''Umbilicaria'' that grow on rocks. They are widely distributed, including on bare rock in Antarctica, and throughout northern parts of North America such as New England and the Rocky Mountains. They are edible when properly prepared; soaking extensively and boiling with changes of water removes the bitterness and purgative properties. They have been used as a famine food in extreme cases when other food sources were unavailable, as by early American northern explorers. ''Umbilicaria esculenta'' is commonly used as a food in Asian cuisine and a restorative medicine in traditional Chinese medicine. It is called ''shi'er'' (石耳 "rock ear") in Chinese cuisine, ''iwatake'' (岩茸 "rock mushroom") in Japanese cuisine, and ''seogi'' (석이(石耳)) or ''seogibeoseot'' (석이버섯) in Korean cuisine. Species *''Umbilicaria americana'' *''Umbilicaria antarctica'' *''Umbilicaria aprina'' *''Umbilicaria arctica'' *' ...
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Otter Creek Wilderness
The Otter Creek Wilderness is a U.S. Wilderness area located in the Cheat-Potomac Ranger District of Monongahela National Forest in West Virginia, USA. The Wilderness sits in a bowl-shaped valley formed by Otter Creek, between McGowan Mountain and Shavers Mountain in Tucker and Randolph Counties. It is crossed by of hiking trails. Otter Creek Trail is the longest, at . History By 1914, almost all of the virgin forest in the Otter Creek watershed had been timbered, mostly by the Otter Creek Boom and Lumber Company, but also by the owners of several small farms and homesteads. In 1917 key land purchases were made by the U.S. Forest Service as part of the formation of the national forest system. The Otter Creek area was managed as a multiple use forest, including some second growth logging, until the passage of the Eastern Wilderness Act in 1975. The last private in-holding was acquired the same year. 2009 addition The Omnibus Public Lands Management Act of 2009 added to the or ...
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Pratt Mountain
Pratt Mountain is a summit within the Wapack Range of mountains in south-central New Hampshire, United States. It lies within the town of New Ipswich and is traversed by the Wapack Trail. The subordinate peak, Stony Top, , forms the north shoulder of the mountain. Pratt Mountain offers expansive views from rocky ledges along its length. New Ipswich Mountain is located directly to the north along the Wapack ridgeline; to the southeast rise Binney Hill , Emerson Hill , Nutting Hill , and Mount Watatic, the southern terminus of the Wapack Range. The east side of the mountain drains into the Souhegan River watershed, to the Merrimack River thence the Atlantic Ocean; the west and south sides drain into the Millers River watershed, to the Connecticut River, thence into Long Island Sound. Binney Pond, located in Binney Pond State Forest along the Wapack ridgecrest between Pratt Mountain and Binney Hill, is known for a biodiversity of rare plants and salamanders. References * ''Sout ...
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Quartz
Quartz is a hard, crystalline mineral composed of silica (silicon dioxide). The atoms are linked in a continuous framework of SiO4 silicon-oxygen tetrahedra, with each oxygen being shared between two tetrahedra, giving an overall chemical formula of SiO2. Quartz is the second most abundant mineral in Earth's continental crust, behind feldspar. Quartz exists in two forms, the normal α-quartz and the high-temperature β-quartz, both of which are chiral. The transformation from α-quartz to β-quartz takes place abruptly at . Since the transformation is accompanied by a significant change in volume, it can easily induce microfracturing of ceramics or rocks passing through this temperature threshold. There are many different varieties of quartz, several of which are classified as gemstones. Since antiquity, varieties of quartz have been the most commonly used minerals in the making of jewelry and hardstone carvings, especially in Eurasia. Quartz is the mineral defining the val ...
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Erik Acharius
Erik Acharius (10 October 1757 – 14 August 1819) was a Swedish botanist who pioneered the taxonomy of lichens and is known as the "father of lichenology." Acharius was famously the last pupil of Carl Linnaeus. Life Acharius was born in 1757 to Johan Eric Acharius and Catharina Margaretha Hagtorn in Gävle.Sernander., K. “Erik Acharius - Svenskt Biografiskt Lexikon.” Fredrik Teodor Borg - Svenskt Biografiskt Lexikon, sok.riksarkivet.se/sbl/Presentation.aspx?id=5503. He received a private education until he was admitted to Gävle Gymnasium in 1770. Later he matriculated at Uppsala University in 1773 where he studied natural history and medicine under Linnaeus and was the last student to defend a dissertation before him.Thell, A., Kärnefelt, I., Seaward, M., & Westberg, M. (Eds.) (2013). In the footsteps of Erik Acharius. 20th biennial meeting of the Nordic Lichen Society. Vadstena 11–15 August 2013. Programme and Abstracts. Nordic Lichen Society. Acharius's dissert ...
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Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ...
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Acidic Rock
Acidic rock or acid rock refers to the chemical composition of igneous rocks that has 63% wt% SiO2 content. Rocks described as acidic usually contain more than 20% of free quartz. Typical acidic rocks are granite or rhyolite. Term is used in chemical classification of igneous rock based on the content of silica (SiO2). Due to the fact that chemical analyzes are not always available, especially during the fieldwork, classification based on the mineral (modal) composition is more often used (dividing the igneous rocks into felsic/leucocratic, mafic/melanocratic and ultramafic Ultramafic rocks (also referred to as ultrabasic rocks, although the terms are not wholly equivalent) are igneous and meta-igneous rocks with a very low silica content (less than 45%), generally >18% MgO, high FeO, low potassium, and are composed ...). The term "silicic", widely used in North America, has wider meaning, however, is often used as broadly synonymous with "acidic". Terms describing compositi ...
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