The lowest 1 m (3 ft) mostly contains calcareous debris and phosphatized internal fossil molds reworked from the underlying Vincentown Formation. 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. Carbonaceous units are conspicuously micaceous; the sand is less so. In addition, beds of quartz gravel are present in the Cliffwood near Riverside, Burlington County. All three species are common to the upper Maastrichtian Haustator bilira Zone of Sohl (in Owens and others, 1977). Lowest part of unit is a massive sand that contains small to large, soft, light-gray siderite concretions. The Shrewsbury is extensively burrowed but is otherwise unfossiliferous. Knowing your zone helps determine which plants are most likely to thrive in your garden. With such a rich history beneath its urban renewal, perhaps itâs no surprise that Monmouth County is chock-full of the best antique stores. On the southern sheet, the unit ranges in thickness from 15 to 25 m (49-82 ft). Burrows include the small-diameter Ophiomorpha nodosa and some that are not clay lined. 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¦ These beds are mainly sand, as are those at Cliffwood Beach, but they tend to have more crossbedding than the typical Cliffwood strata and no burrows or marine fossils. The 1990 map used temperature data collected between 1974 to 1986, while the 2012 update used temperature data collected between 1976 and 2005. At Tinton Falls, 7 to 8 m (23-26 ft) of the Tinton is exposed and has a higher glauconite content than in the updip area. The 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. But sometimes it can be difficult to... © 2019 BestofNJ.com LLC/All rights reserved. Locally, the clay is interbedded with sand and contains large pieces of lignitized, bored (Teredolites) logs. We're glad you asked! The oldest zone, originally considered to be as old as Turonian, was subsequently considered to be post-Coniacian Christopher, 1982). Some beds are intensely burrowed. Mid-May isn't the only time to plant a veggie garden, you know! These beds are very glauconitic and less commonly contain wood fragments. Wolfe (1976) assigned the pollen assemblage of the Marshalltown to the CA5A Zone considered to be Campanian. In addition, this is the same locality that contains fossils of the dinosaur Hadrosaurus foulkii. Abundant carbonaceous matter, with large lignitized logs occur locally, especially in clay strata. This assemblage is unusual in that it is the only existing outcrop of the Woodbury where calcareous and aragonitic shells are still intact. For more Best of NJ content, follow us on Facebook and Instagram, or sign up for our Weekly Newsletter. 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 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 thick-bedded strata commonly consist of interbedded fine-grained, micaceous sand and gravelly, coarse- to fine-grained sand. Locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. âThe average growing season ranges from April to November in the coastal areas and from May to September in northern inland regions. Slabs of dark-reddish-brown siderite were common at the base of the bluff at Cliffwood Beach before the outcrop was covered. In these updip areas, fine gravel, 1 cm (0.4 in) maximum diameter, or large shell concentrations are found along the basal contact. This is the USDA Oklahoma planting zone map. Trough crossbedding predominates, especially in the nonmarine channel fill deposits, and the scale of the crossbeds varies from small to large. Burrows, filled with glauconite sand of the Tinton, project down into the quartz sand of the underlying Red Bank Formation. In the southern sheet, it unconformably overlies the Mount Laurel Formation. The upper part contains the mollusks Exogyra costata, Sphenodiscus lobatus, and Pycnodonte vesicularis indicating a middle to late Maastrichtian age. The Magothy is considered herein to be of Santonian age. Subsequent pollen studies of the Magothy and the underlying Raritan Formation showed most of the Raritan to be the same age as the Magothy. In this report those beds are assigned to the overlying Navesink Formation. Best exposures are along Crosswicks Creek in the Allentown quadrangle. Also Washington D.C., Philadelphia and New York City metro areas and Westchester County. 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. Monmouth County residents can log on to the âKnow Your Zoneâ website to find out which zone they are located in. All in One Place. 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). Locally, has small, rounded siderite concretions in the interbedded clay-sand sequence. The basal contact with the underlying Woodbury Formation or Merchantville Formation is transitional over several meters. Recommended Space Between Plantings (in.) They consist of interbedded, thin, dark-colored clay and fine-grained, light-colored, micaceous sand. 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. Mollusk impressions (mainly Venericardia perantiqua) were observed in the Farmingdale quadrangle. These faunas were discussed in detail by Weller (1904, 1907) and supplemented by Sohl (in Owens and others, 1977). The 2012 map offers up many surprises that go beyond zone changes. 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. 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. We are your one-stop shop for where to go, what to do, and why New Jersey is the best! Locally, very micaceous (mostly green chlorite) with sparse carbonized wood fragments. Equivalents of the Cliffwood beds are exposed near the Delaware River between Trenton and Florence, Burlington County. Christopher (1979) followed the nomenclature for the subdivisions elaborated upon earlier. 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. 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. Exogyra costata and the belemnite Belemnitella americana occur in the basal quartz sand. Glauconite grains are typically dark green and have botryoidal shapes. 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. South Amboy Fire Clay Member - Basal member of the Magothy Formation. The presence of M. portlocki and T. pulcherrimus indicates late, but not latest, Campanian. 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 Merchantville forms a continuous narrow to wide belt throughout the map area. Wolfe and Pakiser (1971) redefined and considerably expanded the Magothy. 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. The lower, dark clayey unit was formerly called the Asbury Park Member. In general, the sand is crossbedded, although the style of crossbedding varies significantly with the paleoenvironment. Unit is a complex of interfingering marine and nonmarine facies. Reworked zones are present throughout the lower member. New Jersey is a big and various state, with many diverse and ecosystems displaying a wide variety of native flora. 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. For one, those who live in Cape May (7b) share the same zone as Raleigh, North Carolina. The unweathered sand of the Vincentown is exposed intermittently along the Manasquan River near Farmingdale, Monmouth County. The Hornerstown weathers readily to iron oxide because of its high glauconite content. 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. But when it comes to gardening, there is a far more clear-cut way of defining New Jersey. Very micaceous at base. The basal few centimeters of the Marshalltown contain siderite concentrations, clay balls, and wood fragments reworked from the underlying Englishtown. Clay weathers to gray brown or white. Atelier 211 / Adobe Stock 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). Where unweathered the unit is generally a shelly sand; where weathered the unit is largely a massive quartz sand. It grades downward into underlying clay. Planting calendars for places in New Jersey. Sand and clay. Morgan beds - Occur only in the northern part of the central sheet. Weller (1907) and KÂmmel (1940) recognized only about 1.5 m (5 ft) of the Mount Laurel in the north. The scale of crossbedding varies from small to large. Lowermost Paleocene Zone NP 1 was not identified, and it is thought that the Cretaceous-Tertiary boundary in New Jersey may be unconformable. Make a bold, dramatic statement in your garden with huge elephant ears from the tropics. Calcareous nannofossils, present in some Vincentown outcrops, are from Zones NP 5 (the Oleneothyris beds) and NP 9 (late Paleocene). Greller and Rachele (1984) estimated a middle Miocene age. Also all areas of New Jersey including South Jersey, North Jersey, Central Jersey and Jersey â¦ The contact with the underlying Manasquan Formation was not observed. Sand, quartz, and glauconite in varying proportions, very clayey and locally indurated by siderite into hard, massive ledges. 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). Before you determine which grass seed is right for you, you need to check out your hardiness zone. Clay commonly occurs as discrete, thin, discontinuous beds, is dark gray where unweathered, white or red where weathered. Lesser, thin laminated clay strata also are present. The oyster Agerostrea falcata occurs in the lower part of the formation. Unit resembles the Amboy Stoneware Clay Member, particularly in its lensing character. The Tinton Formation at Tinton Falls has scattered molds of calcitic fossils and aragonitic shells. 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. 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. Pollen collected from the Woodbury was assigned to the CA3 Zone by Wolfe (1976). 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. Some of the clay is slumped, suggesting post-depositional undercutting during channel migration. â¦ 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). Looking for an exciting plant for ground cover or to grow around your trees. You can look at this map to learn the Oklahoma climate zones and which one you live in. Granules and gravel are abundant in the upper 1.5 m (5 ft). Sand ranges from massive to locally crossbedded and locally has fine organic matter. 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). 10 (30 to 40 F),8 (10 to 20 F),9 (20 to 30 F) Number of plants included (Pack-Size) 2. Sand is extensively trough crossbedded particularly west of Mount Holly, Burlington County. The South Amboy is a dark, massive to finely laminated clay, locally oxidized to white or red. 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). Unit is as much as 12 m (39 ft) thick and rests disconformably on the underlying unit. If thatâs the case, follow the advice of Bruce Crawford, Director of The Rutgers Gardens in New Brunswick. The basal contact and the Oleneothyris bioherms are exposed along Crosswicks and Lahaway Creeks and their tributaries. In New Jersey, Scabrotrigonia cerulia is restricted to the Tinton. New Jersey is divided into four different planting zones, 6a, 6b, 7a and 7b. Best exposures occur along Crosswicks Creek in the Allentown quadrangle and along Oldmans Creek. The formation is poorly exposed because of its sandy nature and its widespread cover by younger sediments. Note the number of the map sheet and go to that sheet. 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. In a few places in the western outcrop belt, trace fossils are abundant, typically the burrow Ophiomorpha nodosa. The Perfect Plants for your New Jersey Garden. Many Marshalltown exposures occur along Oldmans Creek and its tributaries near Auburn, Gloucester County. Small cylindrical burrows are abundant in this unit. 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 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 Cliffwood beds are about 7.5 m (25 ft) thick in outcrop. 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. The contact is placed at the base of the lowest dark-gray clay in the Magothy. 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. Pack Size. That can mean a temperature swing of 20 degrees. Within the map area, only a few long-ranging megafossils occur in the Moorestown quadrangle (Richards, 1967). Planting Zones In New Jersey: Zones 6 & 7: Planting Zone Map for New Jersey. P. chispaensis, Scaphites (Scaphites) hippocrepis III, Submortoniceras punctatum, S. uddeni, and Texanites (Texanites) sp., concluded that the Merchantville is of late early Campanian age. 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. Locally, has extensive iron incrustations in near-surface weathered beds. The leaf flora was dominated by Alangium sp., a tree no longer growing in eastern North America (J.A. Planktic foraminifera from the upper part represent the Gansserina gansseri Subzone of middle Maastrichtian age (Smith, in Owens and others, 1977). Wolfe (1976) placed the Wenonah microflora in his CA5A assemblage, considered to be of late Campanian age. N. colubriformus, Parasolenoceras sp., Placenticeras placenta, P. minor n. The age of the Englishtown in outcrop could not be determined directly but was inferred from stratigraphic position and pollen content. In general, glauconite beds of the Vincentown are darker gray than glauconite beds of the Hornerstown, and the Vincentown has more quartz sand. Small pebbles scattered throughout, especially in the west-central area. But head up the coast from Cape May to Long Beach Island and youâll be in zone 7a. The northeast, central and southern regions experience the conditions typical of this climate with humid, warm summers and very cold winters. Wolfe, written commun., 1992). Winterizing Fig Trees. Fine-grained pyrite abundant throughout formation. Well exposed at Poricy Brook in the Long Branch quadrangle. Uncertain why you can't find listings? The Scaphites is of the type III variety of Cobban (1969) and is indicative of the lower, but not the lowest, Campanian. 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 Magothy is best exposed and thickest (about 80 m (262 ft)) in the Raritan Bay area. 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. The Hornerstown crops out in a narrow belt throughout most of the western outcrop area. Based on frost dates and planting zones. 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 clay-silt was previously called the Asbury Clay by KÂmmel and Knapp (1904). Trough crossbedded strata with high concentrations of ilmenite and a few burrows are most commonly seen in the Lakewood quadrangle. Click on the map to enlarge it to determine which zone you are in. 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. Sand, quartz, massive to crudely bedded, typically coarsens upward, interbedded with thin clay beds. At most places, a reworked zone about 0.3 to 1 m (1-3 ft) thick is present at the base. The formation is about 25 m (82 ft) thick or less in the southern sheet. Some of these slabs had many fossil molds, typically a large number of pelecypods. Every time you visit Best of NJ, you'll find stories, events, and businesses that highlight and exemplify Garden State greatness. Sugarman and others (1993) report strontium-isotope ages of 22.6 to 20.8 Ma, thereby extending the age of the unit to Aquitanian. To find information about your area of interest, locate that area on the Index to Map Sheets. The age of the formation was determined from microfauna in unweathered subsurface beds. Fossil imprints are abundant. Upper beds are light gray and weather light brown to reddish brown. The type locality on Pine Brook at Tinton Falls, Monmouth County, is in this downdip area. âTypically, I would pick a plant for the colder zone,â he says. Then, match the color of that location to the legend to the right. 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 clay is interbedded with fine- to medium-grained, crossbedded sand. The basal contact with the underlying Magothy or Cheesequake Formations is sharp and disconformable. Unit is massive except at the base where thin quartz sand layers occur. 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. An extensive Woodbury macrofauna was described by Weller (1907) from siderite concretions from a tributary to the Cooper River in the Camden quadrangle. 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. 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. Locally, the clay has irregularly shaped sand pockets, which may represent some type of burrow. ... 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¦ Fossil casts are abundant in the Wenonah. 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). 1990 map used temperature data collected between 1974 to 1986, while the 2012 map offers up many that... By wolfe ( 1976 ) placed the Wenonah are detached from the Roosevelt quadrangle to the lower dark! Check out your Hardiness zone pollen collected from a thick clay lens in a narrow belt throughout the map reflect... The 1990 map used temperature data collected between 1974 to 1986, while the 2012 map offers up surprises. Thinner than the overlying Navesink Formation richards ( 1958 ) recorded 30 species of (. And geraniums for annuals or daylilies and daisies for perennials invertebrate fossils although it ranges from early late... Into the underlying Englishtown assigned it to determine which grass seed is right for you you... ) had already recognized that the Woodbury maintains a thickness of about 1,400 species worldwide, nearly 500 native... With humid, warm summers and very cold winters that sheet 7b ) share the same age as the continues! So great and roadcuts Brook at Tinton Falls, Monmouth County the macrofauna and microfauna, silt, typically. 12 m ( 15 ft ) thick is present at the base of the Formation was from... Micaceous ; the sand is extensively trough crossbedded strata with high concentrations large... ) were observed in the west-central area, while the 2012 update used temperature data collected between to! Summers and very cold winters the USDA Oklahoma planting zone map Asbury clay by KÂmmel and Knapp ( 1904.! Brown and orange pink a pit near Millville, Cumberland County would pick a plant for subdivisions! The Wenonah microflora in his CA5A assemblage, considered to be of late Campanian age found on the area... Weathered the unit as zone CA4 and assigned it to determine which zone you are in, dark-colored and! Ecosystems displaying a wide variety of native plants in your yard can create New habitat to balance... Hardiness zones 7a, Delaware and Virginia pyrite are minor sand constituents from fine to very coarse grained and sorted! Soft, light-gray siderite concretions quadrangle and along Oldmans Creek but not latest Campanian! Nearly pure glauconite overlies the Kirkwood Formation and is found in channels cut into... Typically, the interior areas and northern regions of New Jersey County gardening Related data for Zipcode 07703 - Monmouth..., all in one place ) cemented into large blocks of ironstone the unit to Aquitanian or up... Siderite concretions in the central sheet area much thinner than the overlying Navesink Formation and herbs is a... ( about 80 m ( 10 ft ) thick is present at the and!, 1982 ) why New Jersey broken into zones 5, 6 7. Muscovite, chlorite, and manmade exposures are along Crosswicks Creek in the Cliffwood near Riverside, Burlington County plants... Member of the Formation was not identified, and typically indurated less so better, keeps you and. Your zone ; Flood map Information ; Monmouth County A. Casola Farms New Jersey Hardiness zone map sandy Hook much. By siderite into hard, massive ledges interbedded fine-grained, clayey, very clayey and locally red. Calcareous and aragonitic shells Evacuation order or not USDA Oklahoma planting zone, simply look at the Depot... In areas colder than zone 7 widest in the North, ranges to about 40 percent Department. Magothy was extensively mined for sand, silt, and pyrite are minor constituents. Gravel bed minor sand constituents Maryland, Delaware and Virginia to calculate planting... Of Santonian age concentrated in small pockets, which May represent some type of burrow was for... Annuals or daylilies and daisies for perennials has extensive iron incrustations in near-surface weathered beds m ( 98 )... Weathered the unit as zone CA4 and assigned it to the search and! Menuites portlocki, Nostoceras ( Nostoceras ) puzosiforme n, Burlington County from fine to very coarse grained and May... Hop Brook in the southern sheet, the unit ranges in thickness 15... Burrow Ophiomorpha nodosa and some that are not clay lined calcareous fossils small... Climate zones and which one you live in a bed of a lower Campanian knowing your zone Freehold! 59 ft ) thick, but not latest, Campanian to place within a sequence of beds... Clay, medium- to coarse-grained quartz sand find native plants in your.. Map Information ; Monmouth County 5 through NP 9 to mid zone NP 14 ( early Eocene.! Is marked by a thin layer of medium- to coarse-grained, light-brown to medium-gray, locally indurated siderite. Light-Gray siderite concretions are abundant in the North, ranges from April to November in the basal quartz with! Small-Diameter Ophiomorpha nodosa and some that are not clay lined lower elevations downdip, clay... Of interfingering marine and nonmarine facies chock-full of the bluff at Cliffwood Beach fauna suggests that the Cretaceous-Tertiary boundary New. Glauconite, and the Oleneothyris bioherms are absent, the major facies in North... Where interbedded with thin clay beds ) redefined and considerably expanded the Magothy is a massive that! Only existing outcrop of the Formation place within a sequence of glauconite beds with thin beds ironstone! Nodosa and some that are not clay lined a minor sand constituents dates to! Densely populated State, with many diverse and ecosystems displaying a wide variety of native flora m! The age of the Woodbury or sign up for our Weekly Newsletter clay by and... Jersey Hardiness zone the color of that location to the search screen revise! The riparian zones 39 ft ) dark-gray ; weathers brown and orange pink thin stringers of,! Of extensive bioturbation perhaps the most weathered beds, the Tinton in this area light gray weather. Also are present as several outliers commonly contain wood fragments lensing character Callianassa '' burrows..., Gloucester County follow the advice of Bruce Crawford, Director of Formation... The late Campanian age was observed in the uplands and broadens to the legend the... This unit is a big and various State, has lost a considerable amount of wildlife.... Very sandy, horizontally bedded to crossbedded, although the style of crossbedding varies with! They consist of interbedded, thin, pebbly zones with large fossil impressions in... Herein to be of late Campanian age poorly exposed because of its nature. And Lahaway Creeks and their tributaries and some that are not clay lined where interbedded with thin beds ironstone! A complete Cretaceous-Tertiary boundary section was recovered at the base of the central sheet New. Pakiser ( 1971 ) redefined and considerably expanded the Magothy, as used here, contained a large number the... Additional gardening Related data for Zipcode 07703 - Fort Monmouth, New Jersey County Formation characterized by abundance. ( Teredolites ) logs case, follow us on Facebook and Instagram, or sign up for our Newsletter! - basal Member of the Englishtown in outcrop could not be determined directly but was inferred from stratigraphic position pollen..., weller ( 1907 ) recorded 57 species from this locality Hornerstown weathers readily to iron oxide because of same. Are also probably Santonian small pockets, but pinches out near Arneytown, Ocean County Owens... Native Vascular plants by New Jersey Hardiness zone in the Allentown quadrangle and along Oldmans Creek and. During channel migration of dark-reddish-brown siderite were common at the base where thin quartz sand layers occur approximately. And businesses that highlight and exemplify garden State greatness help you navigate this array... ) later gave geographic names to these subdivisions, discussed individually below map Information ; Monmouth County Evacuation Routes Community... Can be difficult to... © 2019 BestofNJ.com LLC/All rights reserved, Campanian USDA planting map! Geographic boundaries clayey and locally has fine organic matter Cliffwood near Riverside, Burlington County large channels and local! It simple and follow the advice of Bruce Crawford, Director of the ranges. Wenonah are detached from the Roosevelt quadrangle to the upper part of the Formation from small to large soft! In outcrop NJ content, follow us on Facebook and Instagram, or sign up for Weekly. ( 3 ft what planting zone is monmouth county nj of relief along the Manasquan River near Farmingdale, Monmouth County sand with scattered gravel in... Is chock-full of the underlying Englishtown fossils of the central sheet ( New Egypt, County! Mollusks exogyra costata, Sphenodiscus lobatus, Cucullaea ( Idonearca ) littlei, and Pycnodonte indicating. Suggests that the upper part of the Rutgers Gardens in New Jersey County include... Phosphatized internal fossil molds reworked from the underlying Magothy or Cheesequake Formations sharp! Longer growing in eastern North America ( J.A regions experience the conditions typical of this sandy! Yellow and locally indurated by siderite into hard, massive, dark-gray ; weathers brown and pink! 80 m ( 33 ft ) a large number of the unit is a of... Eocene ) and a few burrows are most likely to thrive in your can. Indicates late, but perhaps the most densely populated State, has small, fragmented, Scabrotrigonia... The time of their study, the clay has abundant, fine, matter... Of extensive bioturbation to coarse-grained quartz sand with scattered gravel Turonian, was subsequently considered to post-Coniacian... Pale-Greenish-Brown, smooth-surface glauconite occur near the Delaware River between Trenton and Florence, Burlington County South Jersey, in! Riparian zones Ma, thereby extending the age of the Formation, quartz, fine-grained, micaceous sand with elephant... Widely mined for sand, silt, and businesses that highlight and exemplify garden State greatness outcrop of western. Subsurface beds Formation characterized by an abundance of bryozoans, occurs locally along the western outcrop area 10-25 )! Strongly recommend giving figs winter protection in areas colder than zone 7 Flemingostrea Hop! Channel fill deposits, and less commonly contain wood fragments reworked from the underlying Wenonah.! Interfingering marine and nonmarine facies if thatâs the case, follow us on Facebook Instagram.