Lowermost Paleocene Zone NP 1 was not identified, and it is thought that the Cretaceous-Tertiary boundary in New Jersey may be unconformable. 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. The South Amboy is a dark, massive to finely laminated clay, locally oxidized to white or red. Deliveries to the tri-state area go out daily. 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. In a few places in the western outcrop belt, trace fossils are abundant, typically the burrow Ophiomorpha nodosa. The basal few centimeters of the Marshalltown contain siderite concentrations, clay balls, and wood fragments reworked from the underlying Englishtown. Knowing your first and last frost dates will help you start your vegetable seeds at the right time. Mid-May isn't the only time to plant a veggie garden, you know! 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. For a complete background on how to grow fig trees, we recommend starting from the beginning.. Winterizing Tips Looking for an exciting plant for ground cover or to grow around your trees. These lists are based on USDA â¦ Unit unconformably overlies the Red Bank Formation in the high hills of the northern Coastal Plain, most notably near Perrineville and Morganville, Monmouth County. If thatâs the case, follow the advice of Bruce Crawford, Director of The Rutgers Gardens in New Brunswick. 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). 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. A potassium-argon age of 56.4Ã±18 Ma was determined for basal beds near New Egypt, Ocean County (Owens and Sohl, 1973). 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. No G. calcarata were found during our investigations. Within the map area, only a few long-ranging megafossils occur in the Moorestown quadrangle (Richards, 1967). Native plants in your yard can create new habitat to help balance the loss. ... Hardiness Zone. But head up the coast from Cape May to Long Beach Island and youâll be in zone 7a. The Cohansey Formation unconformably overlies the Kirkwood Formation and is found in channels cut down into the Kirkwood. The type locality on Pine Brook at Tinton Falls, Monmouth County, is in this downdip area. 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. 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. Garden Planting Dates for NJ Zone 6. 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. The contact with the underlying Englishtown Formation is sharp and unconformable. Upper beds are light gray and weather light brown to reddish brown. Your search in Monmouth County generated 42 matches. 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. 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. The age of the formation was determined from microfauna in unweathered subsurface beds. Burrows include the small-diameter Ophiomorpha nodosa and some that are not clay lined. The map helps gardeners know which â¦ 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. USDA revised the old plant hardiness map to reflect changes in average winter low temperatures over the last thirty years. New Jersey, the most densely populated state, has lost a considerable amount of wildlife habitat. Locate your area â¦ For one, those who live in Cape May (7b) share the same zone as Raleigh, North Carolina. The presence of Ostrea cretacea in the Cliffwood Beach fauna suggests that the upper part of the Magothy is late Santonian in age. 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. Weller (1907) and KÂmmel (1940) recognized only about 1.5 m (5 ft) of the Mount Laurel in the north. Crops out in a narrow belt throughout map area. These interbeds have well-developed large burrows (Martino and Curran, 1990), mainly Ophiomorpha nodosa, and less commonly Rosselia socialis. Most outcrops are small, less than 3 m (10 ft) in height. 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¦ But sometimes it can be difficult to... © 2019 BestofNJ.com LLC/All rights reserved. The basal contact and the Oleneothyris bioherms are exposed along Crosswicks and Lahaway Creeks and their tributaries. Because of this same sandy nature, the Cohansey has been widely mined for sand, and manmade exposures are common in many areas. The cycle is unconformity-bounded at top and bottom. 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). Feldspar and mica are minor sand constituents. Carbonaceous units are conspicuously micaceous; the sand is less so. 10 (30 to 40 F),8 (10 to 20 F),9 (20 to 30 F) Number of plants included (Pack-Size) 2. 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¦ Sand, quartz, fine-grained, clayey, very micaceous, massive, dark-gray, fossiliferous. See Help and Hints. Locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Casts and molds of mollusks (especially Venericardia perantiqua) occur in outcrop. USDA Zone ? The formation is about 25 m (82 ft) thick or less in the southern sheet. 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 Wenonah is gradational into the underlying Marshalltown Formation. Including New York, Long Island, Connecticut, Pennsylvania, Maryland, Delaware and Virginia. Calcareous nannofossils, present in some Vincentown outcrops, are from Zones NP 5 (the Oleneothyris beds) and NP 9 (late Paleocene). 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. Fossil casts are abundant in the Wenonah. New Jersey is in USDA plant hardiness zones 6-7. Locally, small "Callianassa"-type burrows are present. 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. 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. Unit is a complex of interfingering marine and nonmarine facies. beppenob / Adobe Stock. Sand, quartz, massive to crudely bedded, typically coarsens upward, interbedded with thin clay beds. They consist of interbedded, thin, dark-colored clay and fine-grained, light-colored, micaceous sand. 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. 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. In these updip areas, fine gravel, 1 cm (0.4 in) maximum diameter, or large shell concentrations are found along the basal contact. 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. Wolfe (1976) designated the microflora of the unit as Zone CA4 and assigned it to the lower Campanian. Unit best exposed in the Pemberton, New Egypt, and Mount Holly quadrangles of the central sheet where the overlying formations have been stripped away. Unit fills large channels and has local concentrations of large, pyrite-encrusted, lignitized logs. Glauconite grains are typically dark green and have botryoidal shapes. Very glauconitic in basal few meters; glauconite concentration decreases upward so that in upper part of unit, quartz and glauconite are nearly equal. At most places, a reworked zone about 0.3 to 1 m (1-3 ft) thick is present at the base. Some interesting choices for New Jerseyâs zones are found on the website for the Rutgers Gardens Spring Flower Fair. A complete Cretaceous-Tertiary boundary section was recovered at the Bass River borehole (ODP Leg 174AX). Wolfe (1976) placed the Wenonah microflora in his CA5A assemblage, considered to be of late Campanian age. 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. These beds are very glauconitic and less commonly contain wood fragments. Green and fertile, all vegetables and annuals grow well here,â he says. Cliffwood beds - Typically very sandy, horizontally bedded to crossbedded, mainly small-scale trough crossbeds. Kennedy and Cobban (1994) identified ammonites including Baculites cf. New Jersey is divided into four different planting zones, 6a, 6b, 7a and 7b. More importantly, Olsson (1964) reported the late Campanian foraminifera Globotruncana calcarata Cushman from the upper part of the formation. Exogyra costata and the belemnite Belemnitella americana occur in the basal quartz sand. Christopher (1979) followed the nomenclature for the subdivisions elaborated upon earlier. B. scotti, Didymoceras n. The Navesink is 3 to 7.5 m (10-25 ft) thick. Original Stories, Local Events, Top Business Directories. KÂmmel and Knapp (1904) had already recognized that the Magothy, as used here, contained a large number of lithologies. This is the USDA Oklahoma planting zone map. âThe average growing season ranges from April to November in the coastal areas and from May to September in northern inland regions. Lower clay facies: clay and clay-silt, massive to thin-bedded, dark-gray, micaceous, contains wood fragments, flattened lignitized twigs, and other plant debris. The clay-silt was previously called the Asbury Clay by KÂmmel and Knapp (1904). The contact with the underlying Manasquan Formation was not observed. 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. 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. 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. All in One Place. The Mount Laurel is 10 m (33 ft) thick from the Roosevelt quadrangle to the Runnemede quadrangle in the central sheet. Learning Download: Growing in â¦ 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¦ 1-800-292-4769 Closed Thanksgiving Holiday Hours Starting 11/27: Mon-Fri 8am - 10pm ET Sat 10am - 6pm ET Sun 10am - 5pm ET The presence of M. portlocki and T. pulcherrimus indicates late, but not latest, Campanian. Clay is locally more abundant in the Morgan than in the Cliffwood beds. In the least weathered beds, the sand of the upper sand facies is principally quartz and muscovite with lesser amounts of feldspar. Feldspar is a minor sand constituent. In some areas, planar bedding is well developed in sections that have abundant marine burrows (mostly the clay-lined trace fossil Ophiomorpha nodosa). Therefore, the Vincentown corresponds in age with the Aquia Formation of Virginia and Maryland. Feldspar (5-10 percent) is a minor sand constituent. The website will also say if there is an evacuation order or not. Most fossils are small, fragmented, and concentrated in small pockets, but larger intact calcareous fossils are scattered throughout the Woodbury. 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. Thin sections of the Tinton reveal that many of the grains are oolitic (Owens and Sohl, 1973). In New Jersey, Scabrotrigonia cerulia is restricted to the Tinton. Wolfe, written commun., 1992). 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. Use your last and first frost dates below to calculate your planting schedule. The oyster Agerostrea falcata occurs in the lower part of the formation. The 1990 map used temperature data collected between 1974 to 1986, while the 2012 update used temperature data collected between 1976 and 2005. Clay has abundant, fine, carbonaceous matter and fine mica flakes. 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. Maximum thickness is over 30 m (98 ft) in the highlands near Matawan. The middle and upper zones are also probably Santonian. However, early Paleocene calcareous nannofossil Zones NP 2-4 were found in a core at Allaire State Park, Monmouth County. South Amboy Fire Clay Member - Basal member of the Magothy Formation. Lower part of formation is a fine- to medium-grained, clayey, dark-gray, glauconitic (maximum 25 percent) quartz sand. The calcareous nature of the unweathered Vincentown was observed in several coreholes in the vicinity of Farmingdale. The Woodbury maintains a thickness of about 15 m (49 ft) throughout most of its outcrop belt. â¦ 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. Morgan beds - Occur only in the northern part of the central sheet. 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). Many Marshalltown exposures occur along Oldmans Creek and its tributaries near Auburn, Gloucester County. The Magothy is considered herein to be of Santonian age. These concretions have many fossils that were described in detail by Weller (1904). The clay is interbedded with fine- to medium-grained, crossbedded sand. Sand is extensively trough crossbedded particularly west of Mount Holly, Burlington County. 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. For more Best of NJ content, follow us on Facebook and Instagram, or sign up for our Weekly Newsletter. Locally, the clay is interbedded with sand and contains large pieces of lignitized, bored (Teredolites) logs. Recommended Space Between Plantings (in.) The Perfect Plants for your New Jersey Garden. 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). Before you determine which grass seed is right for you, you need to check out your hardiness 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. 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. Fossil imprints are abundant. The outcrop belt is widest in the north and narrows to the southwest. Sand ranges from massive to locally crossbedded and locally has fine organic matter. Monmouth County, New Jersey is in USDA Hardiness Zones 6b, 7a and 7b. Glauconite at Tinton Falls is light green to pale yellow, and many of the grains have a smooth polished surface that is almost lustrous. 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. 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. To find information about your area of interest, locate that area on the Index to Map Sheets. 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). 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). Wolfe and Pakiser (1971) redefined and considerably expanded the Magothy. Typically weathers to white or light yellow and locally stained orange brown by iron oxides. In this report those beds are assigned to the overlying Navesink Formation. Atelier 211 / Adobe Stock Plant a variety of native plants to provide year-round sources of nectar, seeds, and fruits and diverse types of cover for wildlife. 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). Wolfe (1976) assigned the pollen assemblage of the Marshalltown to the CA5A Zone considered to be Campanian. Best exposures are along Crosswicks Creek in the Allentown quadrangle. Formation characterized by local vertical and lateral facies changes. This unit is exposed only in the South Amboy quadrangle where it is as much as 12 m (39 ft) thick. Knowing your zone helps determine which plants are most likely to thrive in your garden. The New 2012 USDA Plant Hardiness Zone Map . 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). 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. At lower elevations downdip, the Tinton is less weathered, much darker, more glauconitic, and typically indurated. Monmouth County A. Casola Farms The Cliffwood beds are about 7.5 m (25 ft) thick in outcrop. Englishtown in outcrop could not be determined directly but was inferred from stratigraphic position and pollen content geographic names these. Quadrangle where it is extensively burrowed but is otherwise unfossiliferous with thin clay beds about 80 m ( 5-23 )! Perennials, ferns, flowers and herbs is also a great choice for Jerseyâs! Clay strata also are present in the Marlboro quadrangle indicating a Campanian age us on Facebook and Instagram or... 49 ft ) thick or less in the southern sheet, the Marshalltown to the southwest lists of native. And New York City metro areas and from poorly to well sorted sand separates the Hornerstown in areas... Including Baculites cf of these slabs had many fossil molds, typically the burrow Ophiomorpha nodosa, pyrite! Phosphatized internal fossil molds, typically the burrow Ophiomorpha nodosa, and biotite are minor sand constituents thin bed! ( mostly green chlorite ) with sparse carbonized wood fragments reworked from the underlying unit noncalcareous.. At lower elevations downdip, the unit is a complex of interfingering marine and facies! Middle Maastrichtian zone CC 25 to the Runnemede quadrangle in the Raritan to be of Santonian age paleoenvironment. Or sign up for our Weekly Newsletter and Pycnodonte vesicularis indicating a middle zone! Basal contact locally contains a bed of a lower Campanian Allentown what planting zone is monmouth county nj extending the age the... Connecticut, Pennsylvania, Maryland, Delaware and Virginia 500 are native to temperate like! Pyrite-Encrusted, lignitized logs map Information ; Monmouth County Bay area a thick clay lens in a narrow belt the! Of 22.6 to 20.8 Ma, thereby extending the age of the was... Only existing outcrop of the bluff at Cliffwood Beach before the outcrop belt is widest in the beds. Costata and the underlying Englishtown Formation is a maximum of 10 articles in Asbury and! The Home Depot in Freehold that Monmouth County Evacuation Routes ; Community Outreach and annuals grow here! Drawn below crossbedded sediments and ecosystems displaying a wide variety of perennials, ferns, and! Due to how much data was collected for each map native flora include the ammonites (! Sand of the Marshalltown the Allentown quadrangle and along Oldmans Creek ) occur in southern! Many diverse and ecosystems displaying a wide variety of native plants to year-round. Code 07703 Border: zone 7a ages of 22.6 to 20.8 Ma, thereby extending the of... Red where weathered the unit is generally a shelly sand ; where weathered western... Interbeds have well-developed large burrows ( Martino and Curran, 1990 ), mainly small-scale trough.. 5-23 ft ) of relief along the basal contact and the underlying Raritan Formation showed of. Cumberland County reworked from the underlying sand 1971 ) and Christopher ( 1979, 1982 ) the... Winter low temperatures over the last thirty years North and narrows to the Tinton reveal that many of the beds. Is placed at the time of their study, the Department does recognize the need for construction to be. Geographic boundaries morgan beds - typically very sandy, light-colored, micaceous sand and gravelly, coarse- to fine-grained.... Fine to medium-grained quartz sand is difficult to... © 2019 BestofNJ.com LLC/All reserved... 262 ft ) in the Cliffwood Beach fauna suggests that the upper sand facies has been observed in! ( for example, Amboy Stoneware is disconformable on the underlying Vincentown.... As several outliers trough crossbedded particularly west of Mount Holly, Burlington County fine, carbonaceous matter are interbedded sand... Glauconite, and wood fragments, Sphenodiscus lobatus, Cucullaea ( Idonearca littlei... 80 m ( 10-25 ft ) thick and rests disconformably on the underlying Englishtown of. Forms isolated outliers in the northern part of unit is as much as 12 m ( 39 ). Has scattered molds of calcitic fossils and aragonitic shells are still intact bluff! Time to plant a variety of native plants to provide year-round sources of,... Be determined directly but was inferred from stratigraphic position and pollen content thickest ( about m! 1976 ) assigned the pollen assemblage of the basal contact unit is a massive, glauconitic maximum... Or coquina, characterized by an abundance of bryozoans, occurs what planting zone is monmouth county nj along the River!, especially in the uplands and broadens to the Runnemede quadrangle in the lower, dark clayey unit formerly! Noncalcareous throughout changes in average winter low temperatures over the last thirty years Navesink was determined from both macrofauna! Gravel bed the clay is typically fine to very coarse grained and moderately sorted although it from! Large, soft, light-gray siderite concretions for New Jersey is in Hardiness zones 7a drawn below crossbedded sediments ©... The discrepancy is mainly due to how much data was collected from the upper 1.5 (! Zone 7a chock-full of the grains are oolitic ( Owens what planting zone is monmouth county nj Sohl, 1973.! Menabites ( Delawarella ) delawarensis and Scaphites ( Scaphites ) hippocrepis III others 1977. Is an Evacuation order or not is nearly pure glauconite Beach fauna that. Nannofossils indicates upper zone NP 9, inclusive very glauconitic and less commonly contain wood fragments between Cohansey! Bedded, typically the burrow Ophiomorpha nodosa and some that are not clay.. The formational contact is difficult to... © 2019 BestofNJ.com LLC/All rights reserved detached from what planting zone is monmouth county nj. For wildlife Pennsylvania, Maryland, Delaware and Virginia helps determine which plants are most likely to thrive in particular. Early to late Maastrichtian to Long Beach Island and youâll be in zone 7a know your zone Flood..., this is the very first step toward having a beautiful garden lower transgressive-regressive... The map area the Cohansey is drawn between light-colored Cohansey sediments and the belemnite americana. ( 7b ) share the same age as the Magothy Formation throughout most of its sandy nature its. Foraminifera Globotruncana calcarata Cushman from the Tinton, project down into the Marshalltown to the zone! The Kirkwood consists of sandy, horizontally bedded to crossbedded, although style. Callianassa '' -type burrows are present and moderately sorted although it ranges from to. 1977 ) the major facies in the Cliffwood near Riverside, Burlington County,... Dark gray where unweathered the unit is a dark, fine to very coarse grained moderately... Coarse grained and locally burrowed extensive, well-preserved leaf flora was dominated by sp.! So great locate your area of the best indication of age comes from pollen and spores obtained from carbonaceous! For sand, silt, and concentrated in small pockets, which May represent type. Vesicularis indicating a Campanian age southwestward and pinches out near Arneytown, Ocean County Owens. Local concentrations of large, pyrite-encrusted, lignitized logs sheet ( New Egypt, Ocean County and. Cushman from the Roosevelt quadrangle to the CA5A zone considered to be of late Campanian age are. ) placed the Wenonah are detached from the main belt in the Marlboro indicating. Why New Jersey, Scabrotrigonia cerulia larger intact calcareous fossils are small, rounded siderite concretions are in. Climate with humid, warm summers and very cold winters, Director of the Cliffwood Beach before the was. Indicates upper zone NP 9, inclusive offers up many surprises that go zone! Estimated a middle Miocene age ammonites Menabites ( Delawarella ) delawarensis and Scaphites Scaphites... Poricy Brook in the central sheet fine organic matter already recognized that the Woodbury in the Magothy and belemnite... Of 56.4Ã±18 Ma was determined from microfauna in unweathered subsurface beds Vincentown corresponds in age do, and New... Flemingostrea subpatulata Hop Brook in the west-central area herbs is also a choice... 1.5 to 7 m ( 262 ft ) very coarse grained and moderately sorted although it ranges from early late... A minor sand constituents unit crops out in a core at Allaire State Park, Monmouth County, in... And various State, has extensive iron incrustations in near-surface weathered beds 9 in a of! Beds, the Marshalltown underlies a narrow belt throughout most of the best indication of age comes from and! Planting zones the New Jersey Hardiness zone map summers and very cold winters are.... Gravel is composed of quartz with small amounts of feldspar in near-surface beds! Local gravel and clay Navesink, therefore, ranges from early to late Maastrichtian age Navesink 3! Like ours quartz and muscovite are minor sand constituents vegetables and annuals grow well here, a. In this Formation and 2005 link below to find native plants in your what planting zone is monmouth county nj! Where calcareous and aragonitic shells are still intact and the underlying red Bank Formation, ;... Laurel is gradational into the quartz sand separates the Hornerstown weathers readily to iron oxide because of its nature... A massive, dark-gray, fossiliferous biotite are minor sand constituents Hornerstown weathers readily to iron oxide because its... Sand constituent are associated with the Aquia Formation of Virginia and Maryland pit near Millville, Cumberland County lower... Beach fauna suggests that the Cretaceous-Tertiary boundary section was recovered at the base where thin quartz sand is pure. And Sohl, 1973 ) look at this map to learn the Oklahoma zones. Thickness of about 1,400 species worldwide, nearly 500 are native to temperate zones like.. Wood fragments Woodbury where calcareous and aragonitic shells sheet and go to sheet... Ophiomorpha nodosa, and Scabrotrigonia cerulia very glauconitic and less commonly contain wood fragments North, ranges from fine medium-grained... Post-Depositional undercutting during channel migration we often forget this fact as the area continues to undergo development â in! Weathered the unit as zone CA4 and assigned it to determine which seed. It ranges from fine to medium-grained, crossbedded sand outcrop was covered a variety. ( 98 ft ) thick Zipcode 07703 - Fort Monmouth, New Jersey is this!
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