There is as much as 18 m (59 ft) of relief along the basal contact. sp., Menuites portlocki, Nostoceras (Nostoceras) puzosiforme n. This is the only locality in New Jersey where Zone NP 2 was observed; otherwise, the Hornerstown is confined to Zones â¦ Best exposures occur along Crosswicks Creek in the Allentown quadrangle and along Oldmans Creek. Zone 6b: -5°F to 0°F: Monmouth Beach: Zone 7a: 0°F to 5°F: Monmouth Junction: Zone 6b: -5°F to 0°F: Monroe Township: Zone 6b: -5°F to 0°F: Monroeville: Zone 7a: 0°F to 5°F: Montague: Zone 5b: -15°F to -10°F: Montclair: Zone 6b: -5°F to 0°F: Montvale: Zone 6b: -5°F to 0°F: Montville: Zone 6b: -5°F to 0°F: Moonachie: Zone â¦ Lower clay facies: clay and clay-silt, massive to thin-bedded, dark-gray, micaceous, contains wood fragments, flattened lignitized twigs, and other plant debris. At Tinton Falls, 7 to 8 m (23-26 ft) of the Tinton is exposed and has a higher glauconite content than in the updip area. The Hornerstown is 1.5 to 7 m (5-23 ft) thick. The age of the Englishtown in outcrop could not be determined directly but was inferred from stratigraphic position and pollen content. Strontium-isotope analysis on calcareous shells from the Tinton yielded ages of 66.2 to 65.6 Ma or a late Maastrichtian age (Sugarman and others, 1995). The Farmingdale Member and the Deal Member (of Enright, 1969) are not used on this map because they are not continuous through the outcrop belt or in the subsurface. Planting calendars for places in New Jersey. Such marine-influenced beds (largely foreshore deposits) occur on the central sheet west of Asbury Park, near Adelphia, Monmouth County, north of the Lakehurst Naval Air Station, Ocean County, and at Juliustown, Burlington County (Owens and Sohl, 1969), and on the southern sheet as far north as Salem, Salem County. The clay-silt was previously called the Asbury Clay by KÂmmel and Knapp (1904). Small cylindrical burrows are abundant in this unit. Winterizing Fig Trees. We often forget this fact as the area continues to undergo development â especially in Asbury Park and Red Bank. The Marshalltown is the basal transgressive unit of a sedimentation cycle that includes the regressive deposits of the overlying Wenonah and Mount Laurel Formations resembling the overlying Red Bank Formation to Navesink Formation cycle in its asymmetry. In short, we aim to be The Best of New Jersey, All in One Place. Zip Code 07703 Border: Zone 7a 0°F to 5°F: View the Full New Jersey Hardiness Zone Map. Zone : Port Monmouth: Zone 7b: Port Murray: Zone 6a: Port Norris: Zone 7a: Port Reading: Zone 7a: Port Republic: Zone 7a: Presidential Lakes Estates: Zone 6b: Princeton: Zone 6b, 7a: Princeton Junction: Zone 6b, 7a: Princeton Meadows: Zone 6b: Prospect Park: Zone : Quinton: Zone 7a: Rahway: Zone 7a: Ramblewood: Zone â¦ Our free planting guide calculates the best dates for sowing seeds indoors and outdoors, and for transplanting seedlings to the gardenâall customized to your location. Isolated outliers of the Wenonah are detached from the main belt in the central sheet area. Consists of several lithologies. Thickness is about 10 m (33 ft) in the northern part of the central sheet, 20 m (66 ft) in the southwestern part of the central sheet, and 7.5 m (25 ft) in the southern sheet. Also Washington D.C., Philadelphia and New York City metro areas and Westchester County. To find information about your area of interest, locate that area on the Index to Map Sheets. A hardiness zone is a geographically defined area in which a specific category of plant life is capable of growing, as defined by climatic conditions, including its ability to withstand the minimum temperatures of the zone. Monmouth County residents can log on to the âKnow Your Zoneâ website to find out which zone they are located in. The New 2012 USDA Plant Hardiness Zone Map . The Shark River is about 18 m (59 ft) thick and consists of two fining-upward cycles: a glauconite sand is present at the base and a clay or silt is present at the top of each cycle. Fine-grained pyrite abundant throughout formation. Upper beds of the Vincentown are as much as 12 m (39 ft) thick and are mostly silty, darkgray to green-gray, massive, glauconite sand that contains a small percentage of quartz. Sand, quartz and mica, fine-grained, silty and clayey, massive to thick-bedded, dark-gray to medium-gray; weathers light brown to white, extensively bioturbated, very micaceous, locally contains high concentrations of sand-sized lignitized wood and has large burrows of Ophiomorpha nodosa. It is poorly exposed because of its sandy nature. These beds are mainly sand, as are those at Cliffwood Beach, but they tend to have more crossbedding than the typical Cliffwood strata and no burrows or marine fossils. The clay is interbedded with fine- to medium-grained, crossbedded sand. In spite of its widespread nature, the Cohansey is poorly exposed because of its loose sandy composition, which causes it to erode easily (Newell and others, in press). Where unweathered the unit is generally a shelly sand; where weathered the unit is largely a massive quartz sand. Sand, quartz, massive to crudely bedded, typically coarsens upward, interbedded with thin clay beds. Feldspar, glauconite, and muscovite are minor sand constituents. The contact with the underlying Englishtown Formation is sharp and unconformable. Locally, the glauconite content of this interval is variable, and the unit becomes almost a bluegreen clay-silt, especially near Pemberton, Burlington County (Owens and Minard, 1964a). South Amboy Fire Clay Member - Basal member of the Magothy Formation. Shells in the bioherms are typical of a restricted environment and contain the brachiopod Oleneothyris harlani (Morton) in the lower beds and the oyster Pycnodonte dissimilaris in the upper beds. Cliffwood beds - Typically very sandy, horizontally bedded to crossbedded, mainly small-scale trough crossbeds. âThe average growing season ranges from April to November in the coastal areas and from May to September in northern inland regions. However, early Paleocene calcareous nannofossil Zones NP 2-4 were found in a core at Allaire State Park, Monmouth County. The Amboy Stoneware is disconformable on the underlying sand. But when it comes to gardening, there is a far more clear-cut way of defining New Jersey. The contact with the underlying Manasquan Formation was not observed. The Cliffwood and Morgan beds, and, presumably the upper thin-bedded sequence, would include the youngest pollen zone; the Amboy Stoneware Clay Member and perhaps the uppermost part of the Old Bridge Sand Member, the middle pollen zone; and the lower part of the Old Bridge Sand Member and South Amboy Fire Clay Member, the oldest pollen zone. The Navesink is 3 to 7.5 m (10-25 ft) thick. Because of this same sandy nature, the Cohansey has been widely mined for sand, and manmade exposures are common in many areas. The unweathered sand of the Vincentown is exposed intermittently along the Manasquan River near Farmingdale, Monmouth County. In the least weathered beds, the sand of the upper sand facies is principally quartz and muscovite with lesser amounts of feldspar. Wolfe (1976) indicated that the Merchantville microflora was distinct from overlying and underlying units and designated it Zone CA2 of early Campanian age. Know Your Zone; Flood Map Information; Monmouth County Evacuation Routes; Community Outreach. Morgan beds - Occur only in the northern part of the central sheet. Wolfe (1976) designated the microflora of the unit as Zone CA4 and assigned it to the lower Campanian. The basal contact with the underlying Woodbury Formation or Merchantville Formation is transitional over several meters. The lower contact of the Magothy in the Delaware River valley is difficult to place because the lower part of the Magothy is lithically similar to the underlying Potomac Formation. The oldest zone, originally considered to be as old as Turonian, was subsequently considered to be post-Coniacian Christopher, 1982). The Shrewsbury is extensively burrowed but is otherwise unfossiliferous. The Best of NJ. Very micaceous at base. Basal quartz sand is fine- to coarse-grained, pebbly, massive, light-yellow, and somewhat glauconitic, as much as 2 m (7 ft) thick and formed by the reworking of the underlying Mount Laurel Formation (Owens and others, 1977). The best indication of age comes from pollen and spores obtained from dark carbonaceous clay. No calcareous fossils were found in outcrop. There are very few rules in gardening, but perhaps the most important one is to work within your zone. In the southern sheet, the Marshalltown underlies a narrow belt in the uplands and broadens to the southwest. Muscovite and feldspar are minor sand constituents. Learning Download: Growing in â¦ Find the best dates for planting and transplanting vegetables and fruit! Clay is locally more abundant in the Morgan than in the Cliffwood beds. Many burrows, some filled with glauconite, project downward into the Englishtown for about one meter (3 ft) giving a spotted appearance to the upper part of the Englishtown (Owens and others, 1970). These designations might come as a surprise to New Jersey gardeners with longer memories, who were accustomed to buying plants in accordance with the 1990 USDA Plant Hardiness Zone Map, which was in use up until 2012. Upper sand facies: sand, typically fine- to medium-grained, massive to thick-bedded, locally crossbedded, light-yellow to white, locally very micaceous and extensively stained by iron oxides in near-surface beds. You can look at this map to learn the Oklahoma climate zones and which one you live in. Locally, very micaceous (mostly green chlorite) with sparse carbonized wood fragments. Sand, quartz, fine- to coarse-grained, locally gravelly (especially at the base), white; weathers yellow brown or orange brown, interbedded with thin-bedded clay or dark-gray clay-silt mainly at the top of the formation. Locally, has extensive iron incrustations in near-surface weathered beds. Monmouth County, New Jersey is in USDA Hardiness Zones 6b, 7a and 7b. The basal beds have a reworked zone 0.3 to 1.2 m (1-4 ft) thick that contains fine- to very coarse grained sand and, locally, gravel. The Woodbury maintains a thickness of about 15 m (49 ft) throughout most of its outcrop belt. Richards (1958) recorded 30 species of mollusks from the Tinton in this area. A Cretaceous age was assigned to this unit by Koch and Olsson (1977) based, in part, on a vertebrate fauna found at Sewell, Gloucester County. The massive character of the basal bed is the result of extensive bioturbation. An extensive Woodbury macrofauna was described by Weller (1907) from siderite concretions from a tributary to the Cooper River in the Camden quadrangle. The Hornerstown weathers readily to iron oxide because of its high glauconite content. With all the variance in zones, itâs likely that your garden might fall on the border of two different zones. Clay-silt, dark-gray; weathers brown and orange pink. The unit has been extensively eroded and stripped from large areas of the New Jersey Coastal Plain, particularly in the central sheet where outliers are common. Feldspar (5-10 percent) is a minor sand constituent. Wolfeâs recommendations include petunias and geraniums for annuals or daylilies and daisies for perennials. Unit forms a broad belt in the central sheet from Sandy Hook Bay, southwest to area around East Greenwich, Gloucester County, where it pinches out or changes facies. Most outcrops are small, less than 3 m (10 ft) in height. âHowever, there are often micro climates in every garden (a protected spot next to a building or wall for example) that would be conducive for a warmer zone plant to thrive.â. sp., Nostoceras (Nostoceras) aff. Exogyra costata and the belemnite Belemnitella americana occur in the basal quartz sand. Large slabs of pyrite-cemented sand are associated with the woody beds. In New Jersey, Scabrotrigonia cerulia is restricted to the Tinton. The contact with the underlying Hornerstown Formation is disconformable; locally shell beds (bioherms) up to 1.5 m (5 ft) thick are found along the contact. Unit crops out in a narrow belt from Sandy Hook Bay on the central sheet and pinches out southwest of Oldmans Creek, Salem County, on the southern sheet. Locate your area â¦ It grades downward into underlying clay. To the south, in the type area, Weller (1907) reported diverse molluskan assemblages indicating a Campanian age. Locally, as near Lakehurst, thick, dark-gray, very lignitic clay was uncovered during the mining of ilmenite and is informally called the Legler lignite (Rachele, 1976). Calcareous nannofossils in subsurface Shark River sections indicate Zones NP 14 through NP 18 (Martini, 1971) (middle Eocene and early late Eocene). The upper part contains the mollusks Exogyra costata, Sphenodiscus lobatus, and Pycnodonte vesicularis indicating a middle to late Maastrichtian age. Your search in Monmouth County generated 42 matches. The formation is best exposed in the central sheet from the Fort Dix Military Reservation, Burlington County, southwestward to the Medford Lakes quadrangle. The discrepancy is mainly due to how much data was collected for each map. The South Amboy is a dark, massive to finely laminated clay, locally oxidized to white or red. In general, glauconite beds of the Vincentown are darker gray than glauconite beds of the Hornerstown, and the Vincentown has more quartz sand. Some interesting choices for New Jerseyâs zones are found on the website for the Rutgers Gardens Spring Flower Fair. The basal contact with the underlying Raritan is well exposed in the Sayre and Fisher Pit in Sayreville, Middlesex County, where the contact is marked by a deeply weathered gravel zone. These lists are based on USDA â¦ It contained the uppermost Maastrichtian calcareous nannofossil Micula prinsii Zone below a spherule layer and the basal Danian planktonic foraminiferal Guembeletria cretacea P0 Zone just above the layer (Olsson and others, 1997). Feldspar is a minor sand constituent. Unit is best exposed in the central sheet in the South Amboy quadrangle and in the Delaware River valley at the base of the bluffs at Florence.