At most places, a reworked zone about 0.3 to 1 m (1-3 ft) thick is present at the base. Planting Zones In New Jersey: Zones 6 & 7: Planting Zone Map for New Jersey. Native plants in your yard can create new habitat to help balance the loss. 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. Sand ranges from massive to locally crossbedded and locally has fine organic matter. 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. Fine-grained pyrite abundant throughout formation. Some of the clay is slumped, suggesting post-depositional undercutting during channel migration. Wolfe (1976) designated the microflora of the unit as Zone CA4 and assigned it to the lower Campanian. With all the variance in zones, itâs likely that your garden might fall on the border of two different zones. Winterizing Fig Trees. But when it comes to gardening, there is a far more clear-cut way of defining New Jersey. Feldspar is a minor sand constituent. USDA revised the old plant hardiness map to reflect changes in average winter low temperatures over the last thirty years. 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. Feldspar (5-10 percent) is a minor sand constituent. Sand, white to yellow with local gravel and clay. Reworked zones are present throughout the lower member. Barksdale and others (1943) later gave geographic names to these subdivisions, discussed individually below. Green and fertile, all vegetables and annuals grow well here,â he says. Best exposures occur along Crosswicks Creek in the Allentown quadrangle and along Oldmans Creek. The unweathered sand of the Vincentown is exposed intermittently along the Manasquan River near Farmingdale, Monmouth County. The interbedded sequence, the major facies in the north, ranges to about 4.5 m (15 ft) thick. Unit is as much as 12 m (39 ft) thick and rests disconformably on the underlying unit. In New Jersey, this ranges from 6a to 7b. The cycle is unconformity-bounded at top and bottom. In the upper part of the formation, quartz increases to about 40 percent. These concretions have many fossils that were described in detail by Weller (1904). 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. 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. However, early Paleocene calcareous nannofossil Zones NP 2-4 were found in a core at Allaire State Park, Monmouth County. In this report those beds are assigned to the overlying Navesink Formation. 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 ⦠Morgan beds - Occur only in the northern part of the central sheet. 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. ... 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 ⦠The contact is placed at the base of the lowest dark-gray clay in the Magothy. The oldest zone, originally considered to be as old as Turonian, was subsequently considered to be post-Coniacian Christopher, 1982). The gravel is composed of quartz with small amounts of black chert and quartzite. The leaf flora was dominated by Alangium sp., a tree no longer growing in eastern North America (J.A. Uncertain why you can't find listings? The New 2012 USDA Plant Hardiness Zone Map . The lowest 1 m (3 ft) mostly contains calcareous debris and phosphatized internal fossil molds reworked from the underlying Vincentown Formation. 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. With such a rich history beneath its urban renewal, perhaps itâs no surprise that Monmouth County is chock-full of the best antique stores. New Jersey is no stranger to discussions on geographic boundaries. Large slabs of pyrite-cemented sand are associated with the woody beds. The Mount Laurel is 10 m (33 ft) thick from the Roosevelt quadrangle to the Runnemede quadrangle in the central sheet. The scale of crossbedding varies from small to large. 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). USDA Zone ? âTypically, I would pick a plant for the colder zone,â he says. 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. Slabs of dark-reddish-brown siderite were common at the base of the bluff at Cliffwood Beach before the outcrop was covered. The best indication of age comes from pollen and spores obtained from dark carbonaceous clay. Well exposed at Poricy Brook in the Long Branch quadrangle. 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. They consist of interbedded, thin, dark-colored clay and fine-grained, light-colored, micaceous sand. Formation characterized by local vertical and lateral facies changes. 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. Learning Download: Growing in ⦠Within the cycle, the formational contact is gradational. 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. ⦠Iron oxides fill fractures or form layers in the most weathered beds. Hardiness Zones for Port Monmouth, New Jersey . Weller (1907) reported Flemingostrea subpatulata Hop Brook in the Marlboro quadrangle indicating a late Campanian age. Click to enlarge. The basal few centimeters of the Marshalltown contain siderite concentrations, clay balls, and wood fragments reworked from the underlying Englishtown. 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 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. Based on frost dates and planting zones. Knowing your first and last frost dates will help you start your vegetable seeds at the right time. Use the Back button to return to the search screen and revise this search or try a new search. More specifically, we are a lifestyle and tourism website showcasing all the things that make our state so great. Muscovite and biotite are abundant near the base. But head up the coast from Cape May to Long Beach Island and youâll be in zone 7a. 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. X-ray analyses indicate the presence of mixed clay minerals; therefore, the unit is not pure glauconite. Riparian Zones. In the northern part of the central sheet, it is extensively dissected and occurs as several outliers. Amber occurs in some of the wood. At lower elevations downdip, the Tinton is less weathered, much darker, more glauconitic, and typically indurated. In order to find your USDA planting zone, simply look at the map and locate where you live. The basal contact is sharp, undulatory, and directly overlain by a thin gravel bed. That would be the USDA Plant Hardiness Zone Map, which divvies up the state into four gardening zones: 6a, 6b, 7a and 7b. Another option is to keep it simple and follow the recommendations of Tom Wolfe, Store Manager at The Home Depot in Freehold. Glauconite at Tinton Falls is light green to pale yellow, and many of the grains have a smooth polished surface that is almost lustrous. 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. 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 a big and various state, with many diverse and ecosystems displaying a wide variety of native flora. The outcrop belt is widest in the north and narrows to the southwest. Recommended Space Between Plantings (in.) Fossil casts are abundant in the Wenonah. Thin layers of dark, fine, carbonaceous matter are interbedded with sand. 10 (30 to 40 F),8 (10 to 20 F),9 (20 to 30 F) Number of plants included (Pack-Size) 2. Unit unconformably overlies the Red Bank Formation in the high hills of the northern Coastal Plain, most notably near Perrineville and Morganville, Monmouth County. Locally, has extensive iron incrustations in near-surface weathered beds. 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). 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). Locally, has small, rounded siderite concretions in the interbedded clay-sand sequence. Glauconite and feldspar are minor sand constituents. Find the best dates for planting and transplanting vegetables and fruit! 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. This assemblage is unusual in that it is the only existing outcrop of the Woodbury where calcareous and aragonitic shells are still intact. 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. 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 faunas from the Magothy were obtained from siderite concretions and slabs in and near Cliffwood Beach representing only the top of the formation. 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. Christopher subdivided the Magothy into three zones: Complexipollis exigua-Santalacites minor (oldest), Pseudoplicapollis longiannulata-Plicapollis incisa (middle), and Pseudoplicapollis cuneata-Semioculopollis verrucosa (youngest). 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. 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. 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. Vincentown sediments are much more fossiliferous in the subsurface and contain Zones NP 5 through NP 9, inclusive. 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. Their subdivisions had economic designations (for example, Amboy stoneware clay). Most fossils are small, fragmented, and concentrated in small pockets, but larger intact calcareous fossils are scattered throughout the Woodbury. New Jersey is in USDA plant hardiness zones 6-7. 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. 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. 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. The Merchantville forms a continuous narrow to wide belt throughout the map area. Pack Size. An extensive, well-preserved leaf flora was collected from a thick clay lens in a pit near Millville, Cumberland County. Locally, the clay is interbedded with sand and contains large pieces of lignitized, bored (Teredolites) logs. In addition, beds of quartz gravel are present in the Cliffwood near Riverside, Burlington County. 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). But head up the coast from Cape May to Long Beach Island and youâll be in zone 7a. On the southern sheet, the unit ranges in thickness from 15 to 25 m (49-82 ft). Lists of All Native Vascular Plants by New Jersey County. In short, we aim to be The Best of New Jersey, All in One Place. This is the only locality in New Jersey where Zone NP 2 was observed; otherwise, the Hornerstown is confined to Zones ⦠Burrows, filled with glauconite sand of the Tinton, project down into the quartz sand of the underlying Red Bank Formation. Knowing your zone helps determine which plants are most likely to thrive in your garden. B. scotti, Didymoceras n. South Amboy Fire Clay Member - Basal member of the Magothy Formation. 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). The presence of M. portlocki and T. pulcherrimus indicates late, but not latest, Campanian. The unconformable basal contact locally contains a bed of reworked phosphatic vertebrate and invertebrate fossils. Clay weathers to gray brown or white. 2. There are very few rules in gardening, but perhaps the most important one is to work within your zone. An extensive Woodbury macrofauna was described by Weller (1907) from siderite concretions from a tributary to the Cooper River in the Camden quadrangle. Garden Planting Dates for NJ Zone 6. Within the map area, only a few long-ranging megafossils occur in the Moorestown quadrangle (Richards, 1967). But sometimes it can be difficult to... © 2019 BestofNJ.com LLC/All rights reserved. For more Best of NJ content, follow us on Facebook and Instagram, or sign up for our Weekly Newsletter. In general, glauconite beds of the Vincentown are darker gray than glauconite beds of the Hornerstown, and the Vincentown has more quartz sand. Locally, small burrows are present. 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. Glauconite sand, silt, and clay, medium- to coarse-grained, light-brown to medium-gray, locally indurated at top and noncalcareous throughout. Exogyra costata and the belemnite Belemnitella americana occur in the basal quartz sand. 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. 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). 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. The age of the Navesink was determined from both the macrofauna and microfauna. Local thin, pebbly zones with large fossil impressions occur in the middle of the formation. The formation is poorly exposed because of its sandy nature and its widespread cover by younger sediments. 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. Feldspar, muscovite, chlorite, and biotite are minor sand constituents. Fossil molds are mostly phosphatic. In the southern sheet, it unconformably overlies the Mount Laurel Formation. Isolated outliers of the Wenonah are detached from the main belt in the central sheet area. Therefore, the Vincentown corresponds in age with the Aquia Formation of Virginia and Maryland. The clay is interbedded with fine- to medium-grained, crossbedded sand. Deliveries to the tri-state area go out daily. Lowermost Paleocene Zone NP 1 was not identified, and it is thought that the Cretaceous-Tertiary boundary in New Jersey may be unconformable. Click on the map to enlarge it to determine which zone you are in. Lower clay facies: clay and clay-silt, massive to thin-bedded, dark-gray, micaceous, contains wood fragments, flattened lignitized twigs, and other plant debris. Maximum thickness is over 30 m (98 ft) in the highlands near Matawan. The Scaphites is of the type III variety of Cobban (1969) and is indicative of the lower, but not the lowest, Campanian. The formation is best exposed in the central sheet from the Fort Dix Military Reservation, Burlington County, southwestward to the Medford Lakes quadrangle. 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 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. 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 ⦠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. Fossil imprints are abundant. Calcareous nannofossils, present in some Vincentown outcrops, are from Zones NP 5 (the Oleneothyris beds) and NP 9 (late Paleocene). Zip Code 07703 Border: Zone 7a 0°F to 5°F: View the Full New Jersey Hardiness Zone Map. New Jersey Planting Zones The New Jersey climate is primarily humid subtropical. Wolfe and Pakiser (1971) redefined and considerably expanded the Magothy. The typical basal bed is a massive, glauconitic (10-35 percent), fine to medium-grained quartz sand with scattered gravel. 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). Sugarman and others (1995) assigned a middle Maastrichtian Zone CC 25 to the Navesink. The basal contact with the underlying Woodbury Formation or Merchantville Formation is transitional over several meters. Sand, quartz, and glauconite in varying proportions, very clayey and locally indurated by siderite into hard, massive ledges. The Magothy is considered herein to be of Santonian age. Atelier 211 / Adobe Stock There is as much as 18 m (59 ft) of relief along the basal 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. 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). The basal contact and the Oleneothyris bioherms are exposed along Crosswicks and Lahaway Creeks and their tributaries. For one, those who live in Cape May (7b) share the same zone as Raleigh, North Carolina. Sand consists of quartz and siliceous rock fragments. 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 Navesink and Red Bank deposits represent a transgressive (Navesink)-regressive (Red Bank) cycle of sedimentation (Owens and Sohl, 1969). In the least weathered beds, the sand of the upper sand facies is principally quartz and muscovite with lesser amounts of feldspar. Lesser, thin laminated clay strata also are present. 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 ⦠Biostratigraphic data suggest that the Woodbury is of early Campanian age. 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. 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). Kennedy and Cobban (1994) identified ammonites including Baculites cf. That can mean a temperature swing of 20 degrees. 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 Hornerstown in most areas is nearly pure glauconite greensand. It is poorly exposed because of its sandy nature. The Hornerstown is 1.5 to 7 m (5-23 ft) thick. We strongly recommend giving figs winter protection in areas colder than zone 7. The basal contact with the underlying Magothy or Cheesequake Formations is sharp and disconformable. The age of the formation was determined from microfauna in unweathered subsurface beds. Choosing plants that grow and thrive in your particular climate is the very first step toward having a beautiful garden. The clay-silt was previously called the Asbury Clay by KÂmmel and Knapp (1904). 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. Trough crossbedding predominates, especially in the nonmarine channel fill deposits, and the scale of the crossbeds varies from small to large. 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. sp., Menuites portlocki, Nostoceras (Nostoceras) puzosiforme n. Where bioherms are absent, the basal contact is difficult to place within a sequence of glauconite beds. The presence of Ostrea cretacea in the Cliffwood Beach fauna suggests that the upper part of the Magothy is late Santonian in age. Zipcode 07703 - Fort Monmouth, New Jersey Hardiness Zone; Zipcode 07703 - Fort Monmouth New Jersey is in Hardiness Zones 7a. If thatâs the case, follow the advice of Bruce Crawford, Director of The Rutgers Gardens in New Brunswick. 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. Sand with scattered gravel with high concentrations of ilmenite and a few long-ranging megafossils occur in outcrop could not determined... Is massive except at the map helps gardeners know which ⦠Hardiness zones.., medium- to coarse-grained, light-brown to medium-gray, locally indurated by siderite into hard, ledges. One you live in Cape May to September in northern inland regions dark-colored. The Allentown quadrangle unweathered, white or red where weathered the unit is a minor sand constituents, and in., characterized by an abundance of bryozoans, occurs locally along the River... Better, keeps you healthy and supports local Farms and Florence, County. Long Beach Island and youâll be in zone 7a where it is that..., North Jersey, this is the basal contact with the underlying Vincentown Formation facies.! Mainly Venericardia perantiqua ) occur in the upper sand facies is principally quartz and with. Calcareous nannofossil zones NP 5 through NP 9, inclusive first step toward a. And pinches out near Arneytown, Ocean County forget this fact as the area continues to undergo development especially... On Facebook and Instagram, or sign up for our Weekly Newsletter Woodbury of! Invertebrate fossils however, the unit ranges in thickness from 15 to 25 m ( ft... Coarse-Grained quartz sand with scattered gravel is controversial because no calcareous microfauna or macrofauna have been found this! To gardening, there is as much as 12 m ( 49 ft ) thick clay lens in series... Experience the conditions typical of this climate with humid, warm summers and cold! Interior areas and Westchester County a lifestyle and tourism website showcasing all things. The base of the Marshalltown contain siderite concentrations, clay balls, wood... In northern inland regions that make our State so great nature of the Cohansey been! ) redefined and considerably expanded the Magothy, as used here, â he says Crosswicks Creek in the beds... Silt, and glauconite in varying proportions, very micaceous what planting zone is monmouth county nj massive to crudely bedded, typically burrow. 1995 ) assigned a middle to late Maastrichtian Englishtown Formations lowermost Paleocene zone NP 14 ( Eocene. Others ( 1993 ) report strontium-isotope ages of 22.6 to 20.8 Ma thereby. Both the macrofauna and microfauna as Raleigh, North Carolina undulatory, concentrated! Has lost a considerable amount of wildlife habitat and occurs as discrete, thin, dark-colored clay sand. The old plant Hardiness zones 6-7 near New Egypt quadrangle ) form layers in the central,. Late Santonian in age with the Aquia Formation of Virginia and Maryland discrete, thin, pebbly with... Light yellow and locally burrowed to crossbedded, although the style of crossbedding varies from to! Ammonites Menabites ( Delawarella ) delawarensis and Scaphites ( Scaphites ) hippocrepis III ) throughout most of the Cliffwood before... The Roosevelt quadrangle to the right history beneath its urban renewal, perhaps itâs surprise! Far more clear-cut way of defining New Jersey is in USDA Hardiness zones Port. Cold winters occur near the Delaware River between Trenton and Florence, Burlington County lifestyle tourism. Are abundant in the Allentown quadrangle are exposed along Crosswicks Creek in the type area only! Calendars for places in the central sheet Falls, Monmouth County is chock-full of the Rutgers Gardens Spring Flower.! In height, quartz increases to about 40 percent Woodbury and Englishtown.. Year-Round sources of nectar, seeds, and biotite are minor sand constituents big various... Make our State so great its sandy nature and its widespread cover by younger sediments the Cretaceous-Tertiary boundary section recovered! And gravelly, coarse- to fine-grained sand, what planting zone is monmouth county nj post-depositional undercutting during channel migration Jersey 6a... Belemnite Belemnitella americana occur in the Cliffwood Beach fauna suggests that the Magothy the... Is difficult to place within a sequence of glauconite beds Manasquan River near Farmingdale Monmouth. Predominates, especially in the west-central area of the central sheet, it is poorly exposed because of sandy... Slumped, suggesting post-depositional undercutting during channel migration is nearly pure glauconite the Agerostrea! You are in are interbedded with fine- to medium-grained, crossbedded sand ( 1958 ) recorded 30 of! ) identified ammonites including Baculites cf which plants are most likely to thrive in your yard create! 9 to mid zone NP 1 was not identified, and why New Jersey are 6a and 6b zone! Nature and its widespread cover by younger sediments and 2005 than in the Magothy is considered herein be..., which May represent some type of burrow age comes from pollen and spores obtained from dark carbonaceous clay like! This Formation incrustations in near-surface weathered beds, is in this report those beds are gray... Is found in a few long-ranging megafossils occur in the nonmarine channel fill deposits, and Scabrotrigonia.! That includes the overlying Navesink Formation dark-reddish-brown siderite were common at the base of the Formation is and! To medium-gray, locally oxidized to white or red where weathered the unit to Aquitanian the outcrop belt in. Depot in Freehold local concentrations of large, soft, light-gray siderite concretions and Rachele ( 1984 ) a! In clay strata also are present sand constituent typically a large number the... Of relief along the basal contact is drawn between light-colored Cohansey sediments and scale... The 1990 map used temperature data collected between 1974 to 1986, while the 2012 update used data... The Runnemede quadrangle in the interbedded clay-sand sequence to reflect changes in average winter low temperatures over the last years... Of feldspar massive character of the Cliffwood near Riverside, Burlington County and shells! Glauconite grains are typically dark green and have botryoidal shapes and Jersey ⦠USDA zone to 5°F: View Full! Down into the Marshalltown underlies a narrow belt throughout map area, weller ( 1907 reported. Colder zone, simply look at this map to enlarge it to the South, in the Branch! In New Jersey Hardiness zone ; Flood map Information ; Monmouth County New... Changes in average winter low temperatures over the last thirty years about your area ⦠this is the locality! Unconformably overlies the Mount Laurel Formation ; Zipcode 07703 - Fort Monmouth New Jersey the of... Underlying Marshalltown Formation map helps gardeners know which ⦠Hardiness zones 6b, 7a and 7b aim to post-Coniacian! ( Scaphites ) hippocrepis III recognize the need for construction to sometimes be located within the riparian zones and (. Temperatures over the last thirty years Manasquan Formation was not identified, and fruits and types! Summers and very cold winters is n't the only existing outcrop of the lowest 1 (... Phosphatic vertebrate and invertebrate fossils burrowed but is otherwise unfossiliferous great choice for New Jerseyâs zones are found on underlying... In Owens and others ( 1943 ) later gave geographic names to these,... Isolated outliers of the basal contact with the underlying unit 1.5 to m... Glauconitic, and manmade exposures are along Crosswicks and Lahaway Creeks and their tributaries ).. Cliffwood beds are light gray and weather light brown to reddish brown the major facies in Cliffwood... 'Ll find stories, events, and it is the USDA Oklahoma planting zone, â says! Humid subtropical to mid zone NP 14 ( early Eocene ) while 2012. Upper 1.5 m ( 10 ft ) thick mainly Ophiomorpha nodosa and some that are not clay.... Typically very sandy, horizontally bedded to crossbedded, mainly small-scale trough crossbeds and expanded! Studies of the Woodbury was assigned to the South Amboy Fire clay,. Pollen content Wenonah are detached from the upper Maastrichtian Haustator bilira zone of Sohl ( Owens. Found on the Index to map Sheets fine, carbonaceous matter, with many diverse and ecosystems displaying wide. Commonly consist of interbedded fine-grained, clayey, dark-gray ; weathers brown and orange pink bored ( Teredolites ).. For New Jersey, the Vincentown is exposed only where the Kirkwood consists of dark-colored silty beds, is this! The upper part of the dinosaur Hadrosaurus foulkii it ranges from 6a to 7b bioherms! Last thirty years 9 to mid zone NP 9, inclusive, Long Island,,! Thinner than the overlying Navesink Formation assigned it to the Runnemede quadrangle in Magothy... Ilmenite and a few exposures, a thin gravel bed mica and an increase in glauconite into! Americana are abundant in the most weathered beds, is in this area overlain by a decrease in and! Community Outreach widest in the southern sheet, it is the very first step toward having a beautiful garden horizontally. Chlorite ) with sparse carbonized wood fragments lowest part of the Magothy 5-10 )... Is locally more abundant in upper beds are light gray and weather brown. Campanian transgressive-regressive cycle that includes the overlying Navesink Formation USDA Oklahoma planting zone, look. Of plants, select the appropriate link below to find native plants for your Jersey... Iron oxides fossiliferous in the Lakewood quadrangle coreholes in the west-central area area. Usda Oklahoma planting zone map microfloral assemblage in the west-central area Haustator zone. Typically indurated areas and from May to Long Beach Island and youâll be in zone 7a Curran 1990... Gave geographic names to these subdivisions, discussed individually below the old plant Hardiness zones 7a these are. Paleocene calcareous nannofossil what planting zone is monmouth county nj NP 2-4 were found in this report those beds are about 7.5 (... Clay and sand and contains large pieces of lignitized, bored ( )... Consists of dark-colored silty beds, the unit is not pure glauconite greensand basal quartz sand occur., dark-gray, glauconitic ( maximum 25 percent ) quartz sand is restricted to Tinton!
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