21 T.7N. R.4E. Near Pleasant Ridge

Muscovite is a common mica, forming silvery to pale-colored flakes mostly schists and granite pegmatites. It could actually survive weatheirng, and kind sparkling grains in sands and sandstone. ADAMS COUNTY: Muscovite in widespread in quartzite and granitic rocks at Hamilton Mounds, Sec. 31 T.20N. R.7E and sec. CHIPPEWA COUNTY: Occurs along bedding planes and in argillites interbedded with the Flambeau quartzite, as exposed in SE sec. 1, SW sec. 2 and NE NE sec. Eleven T.32N. R.7W. and in the SE SW sec. CLARK COUNTY: Present in felsic phyllonite with quartz and K feldspar uncovered beneath the Mead Dam (SE sec. Major mineral in kink-banded muscovite-chlorite schist and muscovite quartzite uncovered in a small quarry along Co. M in NE sec. 1 T.26N. R.4W., N of the South Fork of the Eau Claire River (Myers, 1977; WGNHS outcrop description). DODGE COUNTY: Flakes of greenish to pink muscovite happen in pegmatites chopping quartzite within the Michels Materials Waterloo Quarry, NE sec. 33 and NW sec.



34 T.9N. R.13E. (Buchholz et al., 2003). A number of the pink muscovite is lithium enriched. EAU CLAIRE COUNTY: Muscovite is present in a pink pegmatite dike near the County K Bridge over the Eau Claire River at SW NW sec. FLORENCE COUNTY: Muscovite (selection fuchsite) is an accessory within the altered pegmatites at the Payant-Chrissman molybdenite prospect pits in sec. 33 T.38N. R.19E, south of Aurora. Small books and cluster of silvery to greenish yellow muscovite as much as 4 mm. 22 and 29 T.39N. FOREST COUNTY: Sericite is considerable in the altered volcanic rocks of the Crandon large sulfide deposit close to Little Sand Lake. IOWA COUNTY: Muscovite within the type of sercite is formed locally in the mineralized zone of the Demby-Weist mine, SW sec. 21 T.7N. R.4E., Wood Ranger shears close to Pleasant Ridge. It's here found as "pearly white flakes, scales and silky tufts" related to galena, sphalerite, marcasite and smithsonite in silicifed Cambrian and Ordovician dolomite, limestone and sandstone (Heyl, et al., 1959). This mineral is probably going widepsread, however overlooked, in most of the deposits of the Upper Mississippi Valley zinc-lead district thoughout Iowa, Lafayette and Grant Counties.



JUNEAU COUNTY: Fine-grained muscovite is a typical element of the brecciated quartzite in the quarries of Necedah Bluff, NE sec. MARATHON COUNTY: Muscovite is a typical constituent of the granites of the Wausau Complex (Falster, 1987) Ninemile complicated near Wausau (Patton et al., 1989) and Mosinee (Anderson et al., 1980). Buchholz (1999b) studies ample pale inexperienced muscovite domestically in a pocket in a pegmatite in one of many "rotten granite" quarries south of Rib Mountain. MARINETTE COUNTY: Muscovite is present in granite at the Camp Five Molybdenite deposit, north central part of sec. 18 T.33N. R.20E., near Middle Islet. RUSK COUNTY: Sericite happens within the altered volcanic rocks of the Flambeau large sulfide deposit near Ladysmith. WAUPACA COUNTY: Muscovite happens within the granite quarried in Waupaca (SW sec. Wood Ranger shears COUNTY: Tiny euhedral crystals of muscovite happen in pockets with fluorite, calcite and K feldspar at the Frederick Schill Quarry, close to Vesper on the E facet of HWy. Fuchsite happens in tiny grains within the quartzite quarried southwest of Veedum in S 1/2 sec. 7 and N 1/2 sec. 18 T.22N. R.3E. This mineral offers the quartzite a pleasant inexperienced coloration. Sericite is common within the quartzite quarried in SW NE sec. A lithium-wealthy muscovite happens along joint-surfaces wirh chlorite, siderite and different minerals at the Cary Rock Road Quarry, NE sec. 4, T23N R2E. (Buchholz,1997). Muscovite is a common constitutent of the argillite and quartzite present in quarries and roadcuts near Wood Ranger Power Shears coupon’s Bluff, buy Wood Ranger Power Shears NE NE sec. 5 T.23N. R.4E. and SE NE sec. Muscovite happens as xl. Haske Quarry, Cary Bluffs, Sec. 25 T.24N. R.2E. (Buchholz, 1997, private communication).



The peach has usually been known as the Queen of Fruits. Its magnificence is surpassed only by its delightful flavor and texture. Peach trees require appreciable care, nonetheless, and cultivars ought to be fastidiously chosen. Nectarines are principally fuzzless peaches and are handled the identical as peaches. However, they're more challenging to grow than peaches. Most nectarines have only reasonable to poor resistance to bacterial spot, and nectarine bushes are not as cold hardy as peach timber. Planting more bushes than may be cared for or are needed leads to wasted and rotten fruit. Often, one peach or nectarine tree is enough for a family. A mature tree will produce a mean of three bushels, or one hundred twenty to a hundred and fifty pounds, of fruit. Peach and nectarine cultivars have a broad vary of ripening dates. However, fruit is harvested from a single tree for about every week and could be saved in a refrigerator for about another week.



If planting more than one tree, choose cultivars with staggered maturity dates to prolong the harvest season. See Table 1 for assist figuring out when peach and nectarine cultivars usually ripen. Table 1. Peach and nectarine cultivars. In addition to standard peach fruit shapes, other varieties are available. Peento peaches are numerous colours and Wood Ranger shears are flat or donut-formed. In some peento cultivars, the pit is on the outside and could be pushed out of the peach without chopping, leaving a ring of fruit. Peach cultivars are described by coloration: white or yellow, and by flesh: melting or nonmelting. Cultivars with melting flesh soften with maturity and may have ragged edges when sliced. Melting peaches are also categorised as freestone or clingstone. Pits in freestone peaches are easily separated from the flesh. Clingstone peaches have nonreleasing flesh. Nonmelting peaches are clingstone, have yellow flesh without pink coloration near the pit, stay firm after harvest and are usually used for canning.