what planting zone is monmouth county nj
In the northern part of the central sheet, it is extensively dissected and occurs as several outliers. Zip Code 07703 Border: Zone 7a 0°F to 5°F: View the Full New Jersey Hardiness Zone Map. 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). Barksdale and others (1943) later gave geographic names to these subdivisions, discussed individually below. New Jersey has the unique distinction of being a leading industrial state, having the highest population density in the U.S., and yet also still possesses the title of âThe Garden â¦ sp., Menuites portlocki, Nostoceras (Nostoceras) puzosiforme n. Kennedy and Cobban (1994) identified ammonites including Baculites cf. For more Best of NJ content, follow us on Facebook and Instagram, or sign up for our Weekly Newsletter. The Amboy Stoneware is disconformable on the underlying sand. sp., and Trachyscaphites pulcherrimus. Sand, quartz and glauconite, fine- to medium-grained, silty and clayey, massive, dark-gray; weathers light brown or pale red, extensively bioturbated. The Englishtown underlies a broad belt throughout the map area and ranges from about 45 m (148 ft) thick in the northern part of the central sheet to 30 m (98 ft) thick in the western part of the central sheet to 15 m (49 ft) in the southern sheet. Calcareous nannofossils, present in some Vincentown outcrops, are from Zones NP 5 (the Oleneothyris beds) and NP 9 (late Paleocene). Wolfe, written commun., 1992). The basal contact is sharp, undulatory, and directly overlain by a thin gravel bed. Some of these slabs had many fossil molds, typically a large number of pelecypods. All in One Place. N. colubriformus, Parasolenoceras sp., Placenticeras placenta, P. minor n. Granules and gravel are abundant in the upper 1.5 m (5 ft). Riparian Zones. Casts and molds of mollusks (especially Venericardia perantiqua) occur in outcrop. 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. There is as much as 18 m (59 ft) of relief along the basal contact. Sand, quartz, fine- to coarse-grained, somewhat clayey and micaceous, mostly massive with local small-scale crossbedding, light-yellow to red or dark-brown, slightly glauconitic at the base. Locate your area â¦ 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. The Marshalltown has most recently been assigned to Zone CC 20-21 (Sugarman and others, 1995) of middle and late Campanian age (Perch-Nielsen, 1985). At most places, a reworked zone about 0.3 to 1 m (1-3 ft) thick is present at the base. The Hornerstown crops out in a narrow belt throughout most of the western outcrop area. We're glad you asked! All three species are common to the upper Maastrichtian Haustator bilira Zone of Sohl (in Owens and others, 1977). Soil Survey of Cumberland County, New Jersey How To Use This Soil Survey The detailed soil maps can be useful in planning the use and management of small areas. Maximum thickness is over 30 m (98 ft) in the highlands near Matawan. Know Your Zone is a public education campaign implemented by the Monmouth County Office of Emergency Management to inform the residents, businesses and visitors of Monmouth County of the new hurricane evacuation zones and their vulnerability to storm surge. Within the cycle, the formational contact is gradational. Knowing your zone helps determine which plants are most likely to thrive in your garden. Amboy Stoneware Clay Member - Crops out only in the South Amboy quadrangle in the central sheet and is mainly dark-gray, white-weathering, interbedded clay and silt to fine-grained quartz sand. The Cohansey was markedly thinned because of erosion prior to deposition of overlying units in the western and southern parts of the southern sheet (Owens and Minard, 1975). Sand, glauconite, medium-grained, clayey and silty, massive, dark-gray to dark-gray-green, extensively bioturbated, locally contains large calcareous shells; sand-size mica, locally abundant; weathers light brown or red brown. Where the Kirkwood consists of dark-colored silty beds, the basal contact is drawn between light-colored Cohansey sediments and the underlying dark-colored sediments. Amber occurs in some of the wood. 2. A transition zone of 1.5 m (5 ft) is marked by an increase in clay, silt, and mica into the Wenonah, especially in the west-central area of the central sheet. That would be the USDA Plant Hardiness Zone Map, which divvies up the state into four gardening zones: 6a, 6b, 7a and 7b. It is poorly exposed because of its sandy nature. Subsequent pollen studies of the Magothy and the underlying Raritan Formation showed most of the Raritan to be the same age as the Magothy. The contact is placed at the base of the lowest dark-gray clay in the Magothy. Clay weathers to gray brown or white. Upper beds are light gray and weather light brown to reddish brown. The clay-silt was previously called the Asbury Clay by KÂmmel and Knapp (1904). Gravel beds occur locally, especially in updip areas such as near New Egypt, Ocean County, in the Atlantic Highlands and in the highlands west of Barnegat, Ocean County, in the southern part of the central sheet and in mixed marine and nonmarine facies in the northeastern part of the southern sheet where gravel occurs in well-defined channels. The light-mineral fraction of the dark-colored clay has significantly more feldspar (10-15 percent) and rock fragments (10-15 percent) than the upper sand facies, where the feldspar was probably leached during weathering. The Perfect Plants for your New Jersey Garden. We strongly recommend giving figs winter protection in areas colder than zone 7. These interbeds have well-developed large burrows (Martino and Curran, 1990), mainly Ophiomorpha nodosa, and less commonly Rosselia socialis. Find the best dates for planting and transplanting vegetables and fruit! For some history and details on the Departments regulatory authority over freshwater wetlands in New Jersey, please check out our web page entitled "The United States Environmental Protection Agency and its relationship with the New Jersey Department of Environmental Protection". 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. The Cohansey Formation unconformably overlies the Kirkwood Formation and is found in channels cut down into the Kirkwood. 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. Wolfe and Pakiser (1971) and Christopher (1979, 1982) discussed the microfloral assemblage in the Magothy. Mica, feldspar, and pyrite are minor sand constituents. Isolated outliers of the Wenonah are detached from the main belt in the central sheet area. The Mount Laurel Formation is of late Campanian age based on the assignment of Zone CC 22b to the formation by Sugarman and others (1995) and the occurrence of Exogyra cancellata near Mullica Hill, Gloucester County. ... Rutgers Cooperative Extension assists New Jersey residents who spend significant time and money coping with the challenges that can occur while gardening-but they are not alone, thanks to the vast array of services offered by Rutgers New Jersey Agricultural Experiment Station â¦ The Magothy is considered herein to be of Santonian age. Unit crops out in a narrow belt throughout the map area and forms isolated outliers in the central sheet. 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¦ Uncertain why you can't find listings? Formation characterized by local vertical and lateral facies changes. Locally, very micaceous (mostly green chlorite) with sparse carbonized wood fragments. ... Hardiness Zone. In the southern sheet, the lower clay facies is exposed only where the Coastal Plain was deeply entrenched and stripped away. Richards (1958) recorded 30 species of mollusks from the Tinton in this area. Wetland Delineations. At the time of their study, the Magothy was extensively mined for clay and sand and was well exposed. Planktic foraminifera from the upper part represent the Gansserina gansseri Subzone of middle Maastrichtian age (Smith, in Owens and others, 1977). The cycle is unconformity-bounded at top and bottom. Some beds are intensely burrowed. The typical basal bed is a massive, glauconitic (10-35 percent), fine to medium-grained quartz sand with scattered gravel. The best faunas from the Magothy were obtained from siderite concretions and slabs in and near Cliffwood Beach representing only the top of the formation. 1-800-292-4769 Closed Thanksgiving Holiday Hours Starting 11/27: Mon-Fri 8am - 10pm ET Sat 10am - 6pm ET Sun 10am - 5pm ET More importantly, Olsson (1964) reported the late Campanian foraminifera Globotruncana calcarata Cushman from the upper part of the formation. The massive character of the basal bed is the result of extensive bioturbation. The formation is poorly exposed because of its sandy nature and its widespread cover by younger sediments. Looking for an exciting plant for ground cover or to grow around your trees. Burrows, filled with glauconite sand of the Tinton, project down into the quartz sand of the underlying Red Bank Formation. The plant hardiness zone is 7a with an average annual extreme minimum air temperature of 3.6 °F (â15.8 °C). Wolfe (1976) designated the microflora of the unit as Zone CA4 and assigned it to the lower Campanian. The interbedded sequence, the major facies in the north, ranges to about 4.5 m (15 ft) thick. This assemblage is unusual in that it is the only existing outcrop of the Woodbury where calcareous and aragonitic shells are still intact. Very glauconitic in basal few meters; glauconite concentration decreases upward so that in upper part of unit, quartz and glauconite are nearly equal. These faunas were discussed in detail by Weller (1904, 1907) and supplemented by Sohl (in Owens and others, 1977). The calcareous nature of the unweathered Vincentown was observed in several coreholes in the vicinity of Farmingdale. Where bioherms are absent, the basal contact is difficult to place within a sequence of glauconite beds. Clay-silt, dark-gray; weathers brown and orange pink. Best exposures are along Crosswicks Creek in the Allentown quadrangle. Sand and clay. 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. 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. The upper sand facies has been observed only in pits and roadcuts. Numerous studies of the foraminifera of the Vincentown from calcareous beds in the western outcrop belt indicate that the Vincentown includes the planktic foraminifera Zones P3b through P6a (Olsson and others, 1988). More specifically, we are a lifestyle and tourism website showcasing all the things that make our state so great. The old geologic map of New Jersey (Lewis and KÂmmel, 1910-1912, revised 1950) showed the Magothy to consist of only one lithology (Cliffwood beds at Cliffwood Beach, Monmouth County). 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). New gardeners who are looking to expand beyond tomatoes and cucumbers may be interested to learn which crops should be planted at what time of year - spring, summer, and fall. The unweathered sand of the Vincentown is exposed intermittently along the Manasquan River near Farmingdale, Monmouth County. Unit best exposed in the Pemberton, New Egypt, and Mount Holly quadrangles of the central sheet where the overlying formations have been stripped away. New Jersey is no stranger to discussions on geographic boundaries. Your search in Monmouth County generated 42 matches. Unit fills large channels and has local concentrations of large, pyrite-encrusted, lignitized logs. The best indication of age comes from pollen and spores obtained from dark carbonaceous clay. The middle and upper zones are also probably Santonian. 10 (30 to 40 F),8 (10 to 20 F),9 (20 to 30 F) Number of plants included (Pack-Size) 2. Including New York, Long Island, Connecticut, Pennsylvania, Maryland, Delaware and Virginia. Sand, glauconite, fine- to medium-grained, locally clayey, massive, dark-gray to dusky-green; weathers dusky yellow or red brown, extensively bioturbated, locally has a small amount of quartz at base. Unit is approximately 7.5 m (25 ft) thick, but pinches out along strike. Unit is a complex of interfingering marine and nonmarine facies. 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. An extensive, well-preserved leaf flora was collected from a thick clay lens in a pit near Millville, Cumberland County. The website will also say if there is an evacuation order or not. Wolfe (1976) indicated that the Merchantville microflora was distinct from overlying and underlying units and designated it Zone CA2 of early Campanian age. The age of the Navesink was determined from both the macrofauna and microfauna. 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. The gravel is composed of quartz with small amounts of black chert and quartzite. Lower clay facies: clay and clay-silt, massive to thin-bedded, dark-gray, micaceous, contains wood fragments, flattened lignitized twigs, and other plant debris. Sugarman and others (1995) assigned a middle Maastrichtian Zone CC 25 to the Navesink. USDA revised the old plant hardiness map to reflect changes in average winter low temperatures over the last thirty years. The presence of M. portlocki and T. pulcherrimus indicates late, but not latest, Campanian. Locally, small "Callianassa"-type burrows are present. Weller (1907) recorded 57 species from this locality. Iron oxides fill fractures or form layers in the most weathered beds. Planting Zones In New Jersey: Zones 6 & 7: Planting Zone Map for New Jersey. See Help and Hints. Feldspar (5-10 percent) is a minor sand constituent. Sand consists of quartz and siliceous rock fragments. 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. Their subdivisions had economic designations (for example, Amboy stoneware clay). A transition zone of several meters is marked by a decrease in mica and an increase in glauconite sand into the Marshalltown. Macrofossils occur as internal and external molds and include the ammonites Menabites (Delawarella) delawarensis and Scaphites (Scaphites) hippocrepis III. Maximum thickness in the map area is about 60 m (197 ft); however, thickness is difficult to determine because of the irregular basal contact and extensive post-depositional erosion. Winterizing Fig Trees. 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. 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. The oldest zone, originally considered to be as old as Turonian, was subsequently considered to be post-Coniacian Christopher, 1982). KÂmmel and Knapp (1904) had already recognized that the Magothy, as used here, contained a large number of lithologies. Lower in the section, between high and low tide level, there is a pale-gray clay-silt about 1.5 m (5 ft) thick with many small reddish-brown siderite concretions. Most outcrops are small, less than 3 m (10 ft) in height. The discrepancy is mainly due to how much data was collected for each map. Deliveries to the tri-state area go out daily. Wolfe and Pakiser (1971) redefined and considerably expanded the Magothy. Original Stories, Local Events, Top Business Directories. These lists are based on USDA â¦ The New 2012 USDA Plant Hardiness Zone Map . The Navesink, therefore, ranges from early to late Maastrichtian. Locally, thin stringers of pale-greenish-brown, smooth-surface glauconite occur near the top. If thatâs the case, follow the advice of Bruce Crawford, Director of The Rutgers Gardens in New Brunswick. The type locality on Pine Brook at Tinton Falls, Monmouth County, is in this downdip area. Become part of the Best of NJ community and get new restaurant updates, entertainment picks, and upcoming event details delivered straight to your inbox weekly! In these updip areas, fine gravel, 1 cm (0.4 in) maximum diameter, or large shell concentrations are found along the basal contact. Greller and Rachele (1984) estimated a middle Miocene age. Unit thins southwestward and pinches out near Arneytown, Ocean County. Sand is typically fine to medium grained and locally burrowed. The age of the Englishtown in outcrop could not be determined directly but was inferred from stratigraphic position and pollen content. Exogyra costata and the belemnite Belemnitella americana occur in the basal quartz sand. A potassium-argon age of 56.4Ã±18 Ma was determined for basal beds near New Egypt, Ocean County (Owens and Sohl, 1973). The thick-bedded strata commonly consist of interbedded fine-grained, micaceous sand and gravelly, coarse- to fine-grained sand. Locally, has small, rounded siderite concretions in the interbedded clay-sand sequence. Glauconite grains are typically dark green and have botryoidal shapes. But head up the coast from Cape May to Long Beach Island and youâll be in zone 7a. Another option is to keep it simple and follow the recommendations of Tom Wolfe, Store Manager at The Home Depot in Freehold. However, early Paleocene calcareous nannofossil Zones NP 2-4 were found in a core at Allaire State Park, Monmouth County. Clay has abundant, fine, carbonaceous matter and fine mica flakes. The Hornerstown is 1.5 to 7 m (5-23 ft) thick. Mollusk impressions (mainly Venericardia perantiqua) were observed in the Farmingdale quadrangle. Lesser, thin laminated clay strata also are present. The Navesink is 3 to 7.5 m (10-25 ft) thick. Most of the gravel is 1.3 to 2.5 cm (0.5-1.0 in) in diameter, but pieces as long as 10 cm (4 in) are present. 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 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. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Also all areas of New Jersey including South Jersey, North Jersey, Central Jersey and Jersey â¦ Then, match the color of that location to the legend to the right. Merchantville faunas were analyzed by Sohl (in Owens and others, 1977) who concluded that northern fauna represented deposition on a lower shoreface or in the transition to an inner shelf, whereas the southern fauna was a deeper water assemblage, probably inner shelf. Given the many important ecological functions that a healthy riparian zone provides, adequately preserving such areas is essential to protecting New Jersey's natural resources and water supply. In the upper part of the formation, quartz increases to about 40 percent. A complete Cretaceous-Tertiary boundary section was recovered at the Bass River borehole (ODP Leg 174AX). Sand, quartz, fine-grained, clayey, very micaceous, massive, dark-gray, fossiliferous. Plant a variety of native plants to provide year-round sources of nectar, seeds, and fruits and diverse types of cover for wildlife. Hero (Top) Feature Image: Â© lily / Adobe Stock In a few places in the western outcrop belt, trace fossils are abundant, typically the burrow Ophiomorpha nodosa. Exogyra cancellata and Belemnitella americana are abundant in upper beds in the west-central area of the central sheet (New Egypt quadrangle). Based on frost dates and planting zones. In general, glauconite beds of the Vincentown are darker gray than glauconite beds of the Hornerstown, and the Vincentown has more quartz sand. In some areas, planar bedding is well developed in sections that have abundant marine burrows (mostly the clay-lined trace fossil Ophiomorpha nodosa). On the southern sheet, the unit ranges in thickness from 15 to 25 m (49-82 ft). Ager's (in Owens and others, 1988) analysis of the Cohansey from a corehole at Mays Landing also suggests a middle Miocene (Serravallian) age. âThe average growing season ranges from April to November in the coastal areas and from May to September in northern inland regions. For a complete background on how to grow fig trees, we recommend starting from the beginning.. Winterizing Tips Monmouth County A. Casola Farms Make a bold, dramatic statement in your garden with huge elephant ears from the tropics. You can look at this map to learn the Oklahoma climate zones and which one you live in. Unit conspicuously micaceous throughout and contains finely dispersed pyrite, carbonaceous matter, and small pieces of carbonized wood as much as 30 cm (12 in) in length. 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 Scaphites is of the type III variety of Cobban (1969) and is indicative of the lower, but not the lowest, Campanian. The age of the formation was determined from microfauna in unweathered subsurface beds. Rachele (1976) analyzed the microflora from the Legler site and noted that the Cohansey had a rich and varied assemblage including several genera labeled "exotics" which no longer occur in the northeastern United States: Engelhardia, Pterocarya, Podocarpus, and Cyathea. Use the Back button to return to the search screen and revise this search or try a new search. Wolfeâs recommendations include petunias and geraniums for annuals or daylilies and daisies for perennials. Pollen in the Navesink and Sandy Hook Member of the Red Bank are similar; the Navesink microflora is a CA6/MA-1 Zone in Wolfe's (1976) classification. Weller (1907) reported Flemingostrea subpatulata Hop Brook in the Marlboro quadrangle indicating a late Campanian age. 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. Cliffwood beds - Typically very sandy, horizontally bedded to crossbedded, mainly small-scale trough crossbeds. Locally, the clay is interbedded with sand and contains large pieces of lignitized, bored (Teredolites) logs. The Wenonah is gradational into the underlying Marshalltown Formation. Feldspar, muscovite, chlorite, and biotite are minor sand constituents. Pack Size. The contact with the underlying Englishtown Formation is sharp and unconformable. More recently, Kennedy and Cobban (1993), detailing the ammonite assemblage that includes Baculites haresi, Chesapeakella nodatum, Cryptotexanites paedomorphicus sp., Glyptoxoceras sp., Menabites (Delawarella) delawarensis, M. (Delawarella) vanuxemi, Menabites (Bererella) sp., Pachydiscus (Pachydiscus) sp., Placenticeras placenta, Pseudoscholenbachia cf. Zipcode 07703 - Fort Monmouth, New Jersey Hardiness Zone; Zipcode 07703 - Fort Monmouth New Jersey is in Hardiness Zones 7a. The basal contact with the underlying Woodbury Formation or Merchantville Formation is transitional over several meters. But head up the coast from Cape May to Long Beach Island and youâll be in zone 7a. Suggested varieties include the April Blush Camellia (zone 6), the yellow-flowering Stachyurus praecox (zone 6), the silvery Artemisia âPowis Castleâ (zone 7) and the dark green Cast Iron Aspidistra (zone 7). The Shrewsbury is extensively burrowed but is otherwise unfossiliferous. Lowest part of unit is a massive sand that contains small to large, soft, light-gray siderite concretions. Sand, quartz, fine- to coarsegrained, gravelly, massive, bioturbated, medium- to dark-gray; weathers light brown, yellow, or reddish brown, locally interbedded with thin to thick beds of dark clay. In addition, beds of quartz gravel are present in the Cliffwood near Riverside, Burlington County. Monmouth County, New Jersey is in USDA Hardiness Zones 6b, 7a and 7b. Christopher (1979) followed the nomenclature for the subdivisions elaborated upon earlier. Lists of All Native Vascular Plants by New Jersey County. Fine-grained pyrite abundant throughout formation. In this report those beds are assigned to the overlying Navesink Formation. The Sandy Hook is much thinner than the overlying Shrewsbury Member and is a maximum of 10 m (33 ft) thick. Best exposures occur along Crosswicks Creek in the Allentown quadrangle and along Oldmans Creek. Lower part of formation is a fine- to medium-grained, clayey, dark-gray, glauconitic (maximum 25 percent) quartz sand. Locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. New Jersey is divided into four different planting zones, 6a, 6b, 7a and 7b. These fossiliferous beds, 6 to 7.5 m (20-25 ft) thick, are best exposed along Shingle Run in the New Egypt quadrangle area and in streams that cross the Vincentown outcrop belt in the Pemberton quadrangle. With such a rich history beneath its urban renewal, perhaps itâs no surprise that Monmouth County is chock-full of the best antique stores. 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). 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. An extensive Woodbury macrofauna was described by Weller (1907) from siderite concretions from a tributary to the Cooper River in the Camden quadrangle. In short, we aim to be The Best of New Jersey, All in One Place. It tastes better, keeps you healthy and supports local farms. Monmouth County residents can log on to the âKnow Your Zoneâ website to find out which zone they are located in. 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). Of about 1,400 species worldwide, nearly 500 are native to temperate zones like ours. Small pebbles scattered throughout, especially in the west-central area. To find information about your area of interest, locate that area on the Index to Map Sheets. The Merchantville forms a continuous narrow to wide belt throughout the map area. Mapping Out New Jerseyâs Gardening Zones, Hot Topics in NJ Presented by Caucus Educational Corporation, Digital/Promotional Services for Local Businesses, The Best Antique Stores in Monmouth County, The Best CSA Programs to Join this Spring, OC Grilled Cheese & Quesadilla Co. Comes to Ocean City, The Best NJ Hiking Trails: Schooleyâs Mountain, The Best Limited-Time-Only Holiday Markets in New Jersey. They consist of interbedded, thin, dark-colored clay and fine-grained, light-colored, micaceous sand. Christopher subdivided the Magothy into three zones: Complexipollis exigua-Santalacites minor (oldest), Pseudoplicapollis longiannulata-Plicapollis incisa (middle), and Pseudoplicapollis cuneata-Semioculopollis verrucosa (youngest). Sand is extensively trough crossbedded particularly west of Mount Holly, Burlington County. Throughout its outcrop belt in the central sheet, the Hornerstown unconformably overlies several formations: the Tinton Formation in the extreme northern area; the Red Bank Formation in the northwestern and west-central areas; and the Navesink Formation in the west-central and southern areas. Most burrows project downward into the underlying formations. New Jersey is a big and various state, with many diverse and ecosystems displaying a wide variety of native flora. X-ray analyses indicate the presence of mixed clay minerals; therefore, the unit is not pure glauconite. Slabs of dark-reddish-brown siderite were common at the base of the bluff at Cliffwood Beach before the outcrop was covered. Lowermost Paleocene Zone NP 1 was not identified, and it is thought that the Cretaceous-Tertiary boundary in New Jersey may be unconformable. Of importance are Sphenodiscus lobatus, Cucullaea (Idonearca) littlei, and Scabrotrigonia cerulia. Additional Gardening Related Data for Zipcode 07703 - Fort Monmouth, New Jersey . The northeast, central and southern regions experience the conditions typical of this climate with humid, warm summers and very cold winters. Local thin, pebbly zones with large fossil impressions occur in the middle of the formation. The clay is interbedded with fine- to medium-grained, crossbedded sand. â¦ In New Jersey, this ranges from 6a to 7b. 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. Wolfe (1976) assigned the pollen assemblage of the Marshalltown to the CA5A Zone considered to be Campanian. The Woodbury maintains a thickness of about 15 m (49 ft) throughout most of its outcrop belt. In the northern part of the central sheet, unit consists of a lower, clayey, quartz-glauconite sand, which is exposed intermittently along the Manasquan River near Farmingdale, Monmouth County, and an upper, finegrained quartz sand or silt, which is exposed along Hog Swamp Brook west of Deal, Monmouth County. New Jersey Planting Zones The New Jersey climate is primarily humid subtropical. In the least weathered beds, the sand of the upper sand facies is principally quartz and muscovite with lesser amounts of feldspar. Crops out in a narrow belt throughout map area. In the southern sheet, the Marshalltown underlies a narrow belt in the uplands and broadens to the southwest. Click to enlarge. Reworked zones are present throughout the lower member. The Tinton Formation at Tinton Falls has scattered molds of calcitic fossils and aragonitic shells. Well exposed at Poricy Brook in the Long Branch quadrangle. The Vincentown Formation is as much as 30 m (98 ft) thick and averages 3 to 15 m (10-49 ft) in its subcrop belt. Small siderite concretions are abundant in the Woodbury in the northern part of the outcrop belt. Vincentown sediments are much more fossiliferous in the subsurface and contain Zones NP 5 through NP 9, inclusive. The formation is best exposed in the Trenton East quadrangle, mainly in the tributaries on the western side of Blacks Creek and south of Bordentown, Burlington County, where the entire thickness of the formation can be seen in gullies (Owens and Minard, 1964b). Some interesting choices for New Jerseyâs zones are found on the website for the Rutgers Gardens Spring Flower Fair. There are plenty of plants that are easy to grow and you can see our picks in this article below along with some first hand experience, tips, a link to finding your gardening zone, ideas for super cute kids activities, and a special code for Monmouth County, NJ families to order from Rising Up Gardens. The lowest 1 m (3 ft) mostly contains calcareous debris and phosphatized internal fossil molds reworked from the underlying Vincentown Formation. The Hornerstown in most areas is nearly pure glauconite greensand. Within the map area, only a few long-ranging megafossils occur in the Moorestown quadrangle (Richards, 1967). 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. In the southern sheet, it unconformably overlies the Mount Laurel Formation. Calcareous nannofossils indicates upper Zone NP 9 to mid Zone NP 14 (early Eocene). Biostratigraphic data suggest that the Woodbury is of early Campanian age. 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¦ Native plants in your yard can create new habitat to help balance the loss. The upper part contains the mollusks Exogyra costata, Sphenodiscus lobatus, and Pycnodonte vesicularis indicating a middle to late Maastrichtian age. A good variety of perennials, ferns, flowers and herbs is also a great choice for New Jersey gardens. The presence of Ostrea cretacea in the Cliffwood Beach fauna suggests that the upper part of the Magothy is late Santonian in age. Feldspar is a minor sand constituent. The Navesink and Red Bank deposits represent a transgressive (Navesink)-regressive (Red Bank) cycle of sedimentation (Owens and Sohl, 1969). Where unweathered the unit is generally a shelly sand; where weathered the unit is largely a massive quartz sand. Large wood fragments occur in many clay layers. The formation is about 25 m (82 ft) thick or less in the southern sheet. sp., Nostoceras (Nostoceras) aff. Fossil casts are abundant in the Wenonah. Garden Planting Dates for NJ Zone 6. The Hornerstown weathers readily to iron oxide because of its high glauconite content. But sometimes it can be difficult to... © 2019 BestofNJ.com LLC/All rights reserved. Additional Images (in Order) Courtesy: However, early Paleocene calcareous nannofossil Zones NP 2-4 were found in a core at Allaire State Park, Monmouth County. That can mean a temperature swing of 20 degrees. Because of this same sandy nature, the Cohansey has been widely mined for sand, and manmade exposures are common in many areas. Trough crossbedding predominates, especially in the nonmarine channel fill deposits, and the scale of the crossbeds varies from small to large. In a few exposures, a thin layer of medium- to coarse-grained quartz sand separates the Hornerstown from the underlying unit. Unit is as much as 12 m (39 ft) thick and rests disconformably on the underlying unit. Thickness varies in the northern part of the map area due, in part, to extensive interfingering of this formation with the underlying Wenonah Formation. In addition, this is the same locality that contains fossils of the dinosaur Hadrosaurus foulkii. This prior map had New Jersey broken into zones 5, 6 and 7. The South Amboy is a dark, massive to finely laminated clay, locally oxidized to white or red. Feldspar, glauconite, and muscovite are minor sand constituents. Thin sections of the Tinton reveal that many of the grains are oolitic (Owens and Sohl, 1973). Sand, quartz, and glauconite in varying proportions, very clayey and locally indurated by siderite into hard, massive ledges. Weller (1907) and KÂmmel (1940) recognized only about 1.5 m (5 ft) of the Mount Laurel in the north. Learning Download: Growing in â¦ Locally, small burrows are present. Sand, quartz, medium-grained, well- to poorly sorted, dusky-yellow to pale-gray; weathers orange brown or red brown, typically very glauconitic and clayey near base; glauconite decreases up section. Pollen collected from the Woodbury was assigned to the CA3 Zone by Wolfe (1976). At lower elevations downdip, the Tinton is less weathered, much darker, more glauconitic, and typically indurated. To the south, in the type area, Weller (1907) reported diverse molluskan assemblages indicating a Campanian age. Here are just a few ways to spend a fun afternoon road trip sampling the different sites each town on the Northern Monmouth Coast has to offer. There are very few rules in gardening, but perhaps the most important one is to work within your zone. 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. These zones are generally very good for fruit production; to that end, many types of fruit are very easy to grow in New Jersey. Calcareous nannofossils in subsurface Shark River sections indicate Zones NP 14 through NP 18 (Martini, 1971) (middle Eocene and early late Eocene). Hardiness Zones for Port Monmouth, New Jersey . Fossils typically occur in siderite concretions. The 1990 map used temperature data collected between 1974 to 1986, while the 2012 update used temperature data collected between 1976 and 2005. This is the USDA Oklahoma planting zone map. The formation is best exposed in the central sheet from the Fort Dix Military Reservation, Burlington County, southwestward to the Medford Lakes quadrangle. On the central sheet, the lower member ranges in thickness from 20 to 30 m (66-98 ft) along strike, but thickens to over 60 m (197 ft) to the southeast. The basal contact with the underlying Magothy or Cheesequake Formations is sharp and disconformable. In general, the sand is crossbedded, although the style of crossbedding varies significantly with the paleoenvironment. The Shark River is exposed only at a few localities in the central sheet near Farmingdale, Monmouth County, along the Manasquan and Shark Rivers and in several tributaries to Deal Lake near Asbury Park in the Asbury Park quadrangle (Sugarman and Owens, 1994). Unit resembles the Amboy Stoneware Clay Member, particularly in its lensing character. Some of the clay is slumped, suggesting post-depositional undercutting during channel migration. Sand is dark gray to dark yellow where unweathered; where weathered, siderite changes color of unit to orange brown because of iron oxides, and the formation is stained or cemented in exotic patterns. NOTE: This is part 9 in a series of 10 articles. 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. The Tinton crops out in the northern part of the central sheet from Sandy Hook, Monmouth County, to the northernmost part of the Roosevelt quadrangle, near Perrineville. Mid-May isn't the only time to plant a veggie garden, you know! Fossil imprints are abundant. Sand, quartz, massive to crudely bedded, typically coarsens upward, interbedded with thin clay beds. Thin layers of dark, fine, carbonaceous matter are interbedded with sand. It grades downward into underlying clay. 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. New Jersey is in USDA plant hardiness zones 6-7. Burrows include the small-diameter Ophiomorpha nodosa and some that are not clay lined. The outcrop belt is widest in the north and narrows to the southwest. Small cylindrical burrows are abundant in this unit. Most fossils are small, fragmented, and concentrated in small pockets, but larger intact calcareous fossils are scattered throughout the Woodbury. 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). P. chispaensis, Scaphites (Scaphites) hippocrepis III, Submortoniceras punctatum, S. uddeni, and Texanites (Texanites) sp., concluded that the Merchantville is of late early Campanian age. The average date of â¦ Glauconite sand, silt, and clay, medium- to coarse-grained, light-brown to medium-gray, locally indurated at top and noncalcareous throughout. The oyster Agerostrea falcata occurs in the lower part of the formation. These concretions have many fossils that were described in detail by Weller (1904). Note the number of the map sheet and go to that sheet. Sugarman and others (1993) report strontium-isotope ages of 22.6 to 20.8 Ma, thereby extending the age of the unit to Aquitanian. The age of the Cohansey is controversial because no calcareous microfauna or macrofauna have been found in this formation. We are your one-stop shop for where to go, what to do, and why New Jersey is the best! Old Bridge Sand Member - Predominantly a light-colored sand, extensively crossbedded and locally interbedded with dark-gray laminae; clay is highly carbonaceous, woody, in discontinuous beds, especially near the base. This is the only locality in New Jersey where Zone NP 2 was observed; otherwise, the Hornerstown is confined to Zones â¦ 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. B. scotti, Didymoceras n. Sand, glauconite, locally has high quartz content, very clayey and silty, massive to thick-bedded, grayish-olive-green to dark-greenish-gray; weathers moderate brown or moderate yellow brown. Calcarenite or coquina, characterized by an abundance of bryozoans, occurs locally along the western belt. The basal contact and the Oleneothyris bioherms are exposed along Crosswicks and Lahaway Creeks and their tributaries. In the southwesternmost part of the southern sheet, for example, the Cohansey Formation and much of the upper sand facies were stripped away by successive entrenchments of the Delaware River. Planting calendars for places in New Jersey. Feldspar, mica, pyrite, and phosphatic fragments are minor sand constituents. Glauconite at Tinton Falls is light green to pale yellow, and many of the grains have a smooth polished surface that is almost lustrous. With all the variance in zones, itâs likely that your garden might fall on the border of two different zones. Typically, the interior areas and northern regions of New Jersey are 6a and 6b. This basal bed contains reworked lignitized wood, siderite concretions as much as 13 cm (5 in) in diameter, scattered pebbles and coarse-grained quartz sand and is burrowed. 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. Consists of several lithologies. Clay commonly occurs as discrete, thin, discontinuous beds, is dark gray where unweathered, white or red where weathered. From our Original Series spotlighting NJ Vocabulary and Historic Landmarks, to our Statewide Events Calendar; to our Business Directory full of the best local eateries, entertainment and services. Click on the map to enlarge it to determine which zone you are in. 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). In order to find your USDA planting zone, simply look at the map and locate where you live. The scale of crossbedding varies from small to large. The Cliffwood beds are about 7.5 m (25 ft) thick in outcrop. In New Jersey, Scabrotrigonia cerulia is restricted to the Tinton. No G. calcarata were found during our investigations. The contact with the underlying Manasquan Formation was not observed. 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). The basal few centimeters of the Marshalltown contain siderite concentrations, clay balls, and wood fragments reworked from the underlying Englishtown. New Jersey, the most densely populated state, has lost a considerable amount of wildlife habitat. Some beds are locally micaceous, and in the Lakehurst area, Ocean County, some beds have high concentrations of "black" sand (pseudorutile) that was once extensively mined. The 2012 map offers up many surprises that go beyond zone changes. The Magothy is best exposed and thickest (about 80 m (262 ft)) in the Raritan Bay area. However, the Department does recognize the need for construction to sometimes be located within the riparian zones. Here the lower part of the formation consists of 5 m (16 ft) of medium- to coarse-grained, massive, dark-grayish-green, glauconite-quartz sand. A pocket of Southern New Jersey around the Swedesboro area and the northern Monmouth County coast near Keansburg and Leonardo fall within this zone too. In the central sheet, the lower clay facies is exposed in pits north of Farmingdale, Monmouth County; in a few cuts along the Manasquan River, north of Farmingdale; and along the Shark River, northeast of Farmingdale. For instance, the age-old debate on what separates âNorth Jerseyâ and âSouth Jerseyâ wages on, along with whether or not âCentral Jerseyâ should be part of the debate as well. This is the only locality in New Jersey where Zone NP 2 was observed; otherwise, the Hornerstown is confined to Zones NP 3 and NP 4. 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. The age of the lower member is based on the presence of the diatom Actinoptychus heliopelta, which was recovered from an exposure southwest of Farmingdale near Oak Glen, Monmouth County (Goldstein, 1974). These beds are very glauconitic and less commonly contain wood fragments. Planktic foraminifera from the lower part of the Navesink are indicative of the Rugotruncana subcircumnodifera Subzone of early Maastrichtian age (Smith, in Owens and others, 1977). Unweathered clay is typically dark gray, but commonly weathers white where interbedded with thin beds of ironstone. âTypically, I would pick a plant for the colder zone,â he says. Choosing plants that grow and thrive in your particular climate is the very first step toward having a beautiful garden. The map helps gardeners know which â¦ Know Your Zone; Flood Map Information; Monmouth County Evacuation Routes; Community Outreach. Also Washington D.C., Philadelphia and New York City metro areas and Westchester County. The transition to the underlying Sandy Hook Member occurs within several feet and is characterized by an increase in clay, quartz, silt, mica, and fine pieces of wood downward. Atelier 211 / Adobe Stock The upper part of the formation is approximately 8 m (26 ft) thick and is mostly a very clayey, blue-green to pale-gray, quartz-glauconite (about 20 percent glauconite) sand. Therefore, the Vincentown corresponds in age with the Aquia Formation of Virginia and Maryland. This unit is exposed only in the South Amboy quadrangle where it is as much as 12 m (39 ft) thick. Fossil molds are mostly phosphatic. The Mount Laurel is gradational into the underlying Wenonah Formation. Green and fertile, all vegetables and annuals grow well here,â he says. The latest update for The Best Antique Stores in Monmouth County is written by Lindsay Podolak.. N ew Jerseyâs Monmouth County is rich in history. Feldspar and mica are minor sand constituents. Very micaceous at base. Sand ranges from massive to locally crossbedded and locally has fine organic matter. Gianfranco Bella / Adobe Stock Unit is pyritic, especially in the carbonaceous-rich beds where pyrite is finely disseminated grains or pyritic masses as much as 0.6 m (2 ft) in diameter. 9-1-1 Outreach; Homeland Security; ACES 9-1-1; Ident-Adult ID Card Program; Bicycle & Helmet Safety; Internet Safety; Child Seat Safety Checkpoint/Safe CARGO; MCSO/Neptune High School Explorer Post #1; Citizen â¦ Morgan beds - Occur only in the northern part of the central sheet. Glauconite and feldspar are minor sand constituents. Trough crossbedded strata with high concentrations of ilmenite and a few burrows are most commonly seen in the Lakewood quadrangle. Thereâs nothing better than fresh-picked, seasonal produce. The Mount Laurel is 10 m (33 ft) thick from the Roosevelt quadrangle to the Runnemede quadrangle in the central sheet. Use your last and first frost dates below to calculate your planting schedule. But when it comes to gardening, there is a far more clear-cut way of defining New Jersey. Unit unconformably overlies the Red Bank Formation in the high hills of the northern Coastal Plain, most notably near Perrineville and Morganville, Monmouth County. Typically weathers to white or light yellow and locally stained orange brown by iron oxides. This diatom places the lower member in the lower part of the ECDZ 1 of Andrews (1987), indicative of an early Miocene (Burdigalian) age (Andrews, 1988). A pocket of Southern New Jersey around the Swedesboro area and the northern Monmouth County coast near Keansburg and Leonardo fall within this zone too. To help you navigate this vast array of plants, select the appropriate link below to find native plants for your New Jersey county. Muscovite and feldspar are minor sand constituents. The unconformable basal contact locally contains a bed of reworked phosphatic vertebrate and invertebrate fossils. Recommended Space Between Plantings (in.) Before you determine which grass seed is right for you, you need to check out your hardiness zone. New Jersey ranges from United States Department of Agriculture (USDA) Hardiness Zones 5b through 7b, with most of the state falling squarely in Hardiness Zone 6. Wolfe (1976) placed the Wenonah microflora in his CA5A assemblage, considered to be of late Campanian age. South Amboy Fire Clay Member - Basal member of the Magothy Formation. The unit is about 6 m (20 ft) thick in the northern part of the central sheet, about 20 m (66 ft) thick in the Trenton area, and 12 to 15 m (39-49 ft) thick throughout the southern sheet. beppenob / Adobe Stock. 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. Abundant carbonaceous matter, with large lignitized logs occur locally, especially in clay strata. Large slabs of pyrite-cemented sand are associated with the woody beds. Carbonaceous units are conspicuously micaceous; the sand is less so. 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. Sand, white to yellow with local gravel and clay. The lower member consists of a lower finegrained, clayey, dark-colored, micaceous sand (transgressive) and an upper massive or thick-bedded to crossbedded, light-colored sand (regressive). For the most part, however, the basal contact is characterized by an intensely bioturbated zone in which many burrows filled with bright green glauconite sand from the Hornerstown Formation project down into the dark-gray matrix of the underlying Navesink Formation. USDA Zone ? For one, those who live in Cape May (7b) share the same zone as Raleigh, North Carolina. The leaf flora was dominated by Alangium sp., a tree no longer growing in eastern North America (J.A. For one, those who live in Cape May (7b) share the same zone as Raleigh, North Carolina. The lower, dark clayey unit was formerly called the Asbury Park Member. Fresh exposures occur along tributaries of Raccoon Creek near Mullica Hill, Gloucester County. Knowing your first and last frost dates will help you start your vegetable seeds at the right time. Equivalents of the Cliffwood beds are exposed near the Delaware River between Trenton and Florence, Burlington County. No calcareous fossils were found in outcrop. Locally, the clay has irregularly shaped sand pockets, which may represent some type of burrow. Clay is locally more abundant in the Morgan than in the Cliffwood beds. Muscovite and biotite are abundant near the base. Locally, has extensive iron incrustations in near-surface weathered beds. Many Marshalltown exposures occur along Oldmans Creek and its tributaries near Auburn, Gloucester County. Unit is massive except at the base where thin quartz sand layers occur. We often forget this fact as the area continues to undergo development â especially in Asbury Park and Red Bank. The Merchantville is the basal bed of a lower Campanian transgressive-regressive cycle that includes the overlying Woodbury and Englishtown Formations. The Best of NJ. Where the Kirkwood consists of sandy, light-colored sediments, the basal contact of the Cohansey is drawn below crossbedded sediments. 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