what planting zone is monmouth county nj

Knowing your zone helps determine which plants are most likely to thrive in your garden. Wolfe, written commun., 1992). Unweathered clay is typically dark gray, but commonly weathers white where interbedded with thin beds of ironstone. Feldspar, glauconite, and muscovite are minor sand constituents. 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. 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. More importantly, Olsson (1964) reported the late Campanian foraminifera Globotruncana calcarata Cushman from the upper part of the formation. On the southern sheet, the unit ranges in thickness from 15 to 25 m (49-82 ft). The Magothy is considered herein to be of Santonian age. 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). The Merchantville is the basal bed of a lower Campanian transgressive-regressive cycle that includes the overlying Woodbury and Englishtown Formations. The old geologic map of New Jersey (Lewis and Kmmel, 1910-1912, revised 1950) showed the Magothy to consist of only one lithology (Cliffwood beds at Cliffwood Beach, Monmouth County). There’s nothing better than fresh-picked, seasonal produce. 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. Exogyra costata and the belemnite Belemnitella americana occur in the basal quartz sand. Some of the clay is slumped, suggesting post-depositional undercutting during channel migration. Trough crossbedded strata with high concentrations of ilmenite and a few burrows are most commonly seen in the Lakewood quadrangle. “However, 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.”. N. colubriformus, Parasolenoceras sp., Placenticeras placenta, P. minor n. 2. Where the Kirkwood consists of sandy, light-colored sediments, the basal contact of the Cohansey is drawn below crossbedded sediments. We are your one-stop shop for where to go, what to do, and why New Jersey is the best! It tastes better, keeps you healthy and supports local farms. Before you determine which grass seed is right for you, you need to check out your hardiness zone. Lower clay facies: clay and clay-silt, massive to thin-bedded, dark-gray, micaceous, contains wood fragments, flattened lignitized twigs, and other plant debris. Clay has abundant, fine, carbonaceous matter and fine mica flakes. Burrows, filled with glauconite sand of the Tinton, project down into the quartz sand of the underlying Red Bank Formation. An extensive, well-preserved leaf flora was collected from a thick clay lens in a pit near Millville, Cumberland County. Many Marshalltown exposures occur along Oldmans Creek and its tributaries near Auburn, Gloucester County. Zip Code 07703 Border: Zone 7a 0°F to 5°F: View the Full New Jersey Hardiness Zone Map. They consist of interbedded, thin, dark-colored clay and fine-grained, light-colored, micaceous sand. Ager's (in Owens and others, 1988) analysis of the Cohansey from a corehole at Mays Landing also suggests a middle Miocene (Serravallian) age. Your search in Monmouth County generated 42 matches. 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. Unit is a complex of interfingering marine and nonmarine facies. 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 contact is placed at the base of the lowest dark-gray clay in the Magothy. Clay commonly occurs as discrete, thin, discontinuous beds, is dark gray where unweathered, white or red where weathered. 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). In general, the sand is crossbedded, although the style of crossbedding varies significantly with the paleoenvironment. Lower part of formation is a fine- to medium-grained, clayey, dark-gray, glauconitic (maximum 25 percent) quartz sand. Christopher (1979) followed the nomenclature for the subdivisions elaborated upon earlier. Garden Planting Dates for NJ Zone 6. The Mount Laurel is 10 m (33 ft) thick from the Roosevelt quadrangle to the Runnemede quadrangle in the central sheet. Hardiness Zones for Port Monmouth, New Jersey . Monmouth County residents can log on to the “Know Your Zone” website to find out which zone they are located in. 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. Every time you visit Best of NJ, you'll find stories, events, and businesses that highlight and exemplify Garden State greatness. In short, we aim to be The Best of New Jersey, All in One Place. 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. Small cylindrical burrows are abundant in this unit. Macrofossils occur as internal and external molds and include the ammonites Menabites (Delawarella) delawarensis and Scaphites (Scaphites) hippocrepis III. Small pebbles scattered throughout, especially in the west-central area. In a few places in the western outcrop belt, trace fossils are abundant, typically the burrow Ophiomorpha nodosa. Wolfe (1976) designated the microflora of the unit as Zone CA4 and assigned it to the lower Campanian. 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. You can look at this map to learn the Oklahoma climate zones and which one you live in. 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. 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. Kennedy and Cobban (1994) identified ammonites including Baculites cf. Plant a variety of native plants to provide year-round sources of nectar, seeds, and fruits and diverse types of cover for wildlife. 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). Lowest part of unit is a massive sand that contains small to large, soft, light-gray siderite concretions. Fossils typically occur in siderite concretions. The Magothy is best exposed and thickest (about 80 m (262 ft)) in the Raritan Bay area. 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 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. For more Best of NJ content, follow us on Facebook and Instagram, or sign up for our Weekly Newsletter. Glauconite sand, silt, and clay, medium- to coarse-grained, light-brown to medium-gray, locally indurated at top and noncalcareous throughout. Clay weathers to gray brown or white. Muscovite and biotite are abundant near the base. The leaf flora was dominated by Alangium sp., a tree no longer growing in eastern North America (J.A. A good variety of perennials, ferns, flowers and herbs is also a great choice for New Jersey gardens. A transition zone of several meters is marked by a decrease in mica and an increase in glauconite sand into the Marshalltown. 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. 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. Fossil molds are mostly phosphatic. Sand, quartz, fine- to coarsegrained, gravelly, massive, bioturbated, medium- to dark-gray; weathers light brown, yellow, or reddish brown, locally interbedded with thin to thick beds of dark clay. Planting Zones In New Jersey: Zones 6 & 7: Planting Zone Map for New Jersey. Wetland Delineations. P. chispaensis, Scaphites (Scaphites) hippocrepis III, Submortoniceras punctatum, S. uddeni, and Texanites (Texanites) sp., concluded that the Merchantville is of late early Campanian age. 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 calcareous nature of the unweathered Vincentown was observed in several coreholes in the vicinity of Farmingdale. The presence of Ostrea cretacea in the Cliffwood Beach fauna suggests that the upper part of the Magothy is late Santonian in age. Sand, white to yellow with local gravel and clay. Feldspar is a minor sand constituent. The basal contact with the underlying Raritan is well exposed in the Sayre and Fisher Pit in Sayreville, Middlesex County, where the contact is marked by a deeply weathered gravel zone. These 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. If that’s the case, follow the advice of Bruce Crawford, Director of The Rutgers Gardens in New Brunswick. Some interesting choices for New Jersey’s zones are found on the website for the Rutgers Gardens Spring Flower Fair. New Jersey Planting Zones The New Jersey climate is primarily humid subtropical. It grades downward into underlying clay. Including New York, Long Island, Connecticut, Pennsylvania, Maryland, Delaware and Virginia. 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 … 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. 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. 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. The basal contact and the Oleneothyris bioherms are exposed along Crosswicks and Lahaway Creeks and their tributaries. Sand is extensively trough crossbedded particularly west of Mount Holly, Burlington County. Reworked zones are present throughout the lower member. Abundant carbonaceous matter, with large lignitized logs occur locally, especially in clay strata. The massive character of the basal bed is the result of extensive bioturbation. There is as much as 18 m (59 ft) of relief along the basal contact. In the northern part of the central sheet, it is extensively dissected and occurs as several outliers. Locally stained red or orange brown by iron oxides and (or) cemented into large blocks of ironstone. Within the cycle, the formational contact is gradational. X-ray analyses indicate the presence of mixed clay minerals; therefore, the unit is not pure glauconite. Sand ranges from massive to locally crossbedded and locally has fine organic matter. Mid-May isn't the only time to plant a veggie garden, you know! New Jersey is divided into four different planting zones, 6a, 6b, 7a and 7b. 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. In the southern sheet, the Marshalltown underlies a narrow belt in the uplands and broadens to the southwest. Some of these slabs had many fossil molds, typically a large number of pelecypods. It is poorly exposed because of its sandy nature. These interbeds have well-developed large burrows (Martino and Curran, 1990), mainly Ophiomorpha nodosa, and less commonly Rosselia socialis. 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. 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. The northeast, central and southern regions experience the conditions typical of this climate with humid, warm summers and very cold winters. Gianfranco Bella / Adobe Stock Hero (Top) Feature Image: © lily / Adobe Stock Sand, quartz and glauconite, fine- to medium-grained, silty and clayey, massive, dark-gray; weathers light brown or pale red, extensively bioturbated. beppenob / Adobe Stock. Biostratigraphic data suggest that the Woodbury is of early Campanian age. Crops out in a narrow belt throughout map area. Upper beds are light gray and weather light brown to reddish brown. However, the Department does recognize the need for construction to sometimes be located within the riparian zones. Mapping Out New Jersey’s 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: Schooley’s Mountain, The Best Limited-Time-Only Holiday Markets in New Jersey. We're glad you asked! Locally, the glauconite content of this interval is variable, and the unit becomes almost a bluegreen clay-silt, especially near Pemberton, Burlington County (Owens and Minard, 1964a). Barksdale and others (1943) later gave geographic names to these subdivisions, discussed individually below. Carbonaceous units are conspicuously micaceous; the sand is less so. The Scaphites is of the type III variety of Cobban (1969) and is indicative of the lower, but not the lowest, Campanian. This is the only locality in New Jersey where Zone NP 2 was observed; otherwise, the Hornerstown is confined to Zones … No G. calcarata were found during our investigations. The clay is interbedded with fine- to medium-grained, crossbedded sand. Sand, quartz, massive to crudely bedded, typically coarsens upward, interbedded with thin clay beds. The website will also say if there is an evacuation order or not. sp., Menuites portlocki, Nostoceras (Nostoceras) puzosiforme n. Locally, thin stringers of pale-greenish-brown, smooth-surface glauconite occur near the top. To the south, in the type area, Weller (1907) reported diverse molluskan assemblages indicating a Campanian age. Sand is typically medium grained and moderately sorted although it ranges from fine to very coarse grained and from poorly to well sorted. Lesser, thin laminated clay strata also are present. Deliveries to the tri-state area go out daily. 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. Another option is to keep it simple and follow the recommendations of Tom Wolfe, Store Manager at The Home Depot in Freehold. 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 … 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. Isolated outliers of the Wenonah are detached from the main belt in the central sheet area. We strongly recommend giving figs winter protection in areas colder than zone 7. Unit is as much as 12 m (39 ft) thick and rests disconformably on the underlying unit. Riparian Zones. Note the number of the map sheet and go to that sheet. 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. NOTE: This is part 9 in a series of 10 articles. 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. At most places, a reworked zone about 0.3 to 1 m (1-3 ft) thick is present at the base. Feldspar and mica are minor sand constituents. For one, those who live in Cape May (7b) share the same zone as Raleigh, North Carolina. The contact with the underlying Englishtown Formation is sharp and unconformable. Recommended Space Between Plantings (in.) Well exposed at Poricy Brook in the Long Branch quadrangle. With all the variance in zones, it’s likely that your garden might fall on the border of two different zones. There are very few rules in gardening, but perhaps the most important one is to work within your zone. Monmouth County A. Casola Farms Cliffwood beds - Typically very sandy, horizontally bedded to crossbedded, mainly small-scale trough crossbeds. Feldspar (5-10 percent) is a minor sand constituent. Click on the map to enlarge it to determine which zone you are in. 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). The contact with the underlying Manasquan Formation was not observed. 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. On the central sheet, the lower member ranges in thickness from 20 to 30 m (66-98 ft) along strike, but thickens to over 60 m (197 ft) to the southeast. The presence of M. portlocki and T. pulcherrimus indicates late, but not latest, Campanian. The formation is poorly exposed because of its sandy nature and its widespread cover by younger sediments. Weller (1907) reported Flemingostrea subpatulata Hop Brook in the Marlboro quadrangle indicating a late Campanian age. At lower elevations downdip, the Tinton is less weathered, much darker, more glauconitic, and typically indurated. Pollen collected from the Woodbury was assigned to the CA3 Zone by Wolfe (1976). Unit thins southwestward and pinches out near Arneytown, Ocean County. Many burrows, some filled with glauconite, project downward into the Englishtown for about one meter (3 ft) giving a spotted appearance to the upper part of the Englishtown (Owens and others, 1970). The best indication of age comes from pollen and spores obtained from dark carbonaceous clay. Because of this same sandy nature, the Cohansey has been widely mined for sand, and manmade exposures are common in many areas. Amber occurs in some of the wood. USDA Zone ? 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. Casts and molds of mollusks (especially Venericardia perantiqua) occur in outcrop. However, early Paleocene calcareous nannofossil Zones NP 2-4 were found in a core at Allaire State Park, Monmouth County. 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. Additional Images (in Order) Courtesy: Suggested varieties include the April Blush Camellia (zone 6), the yellow-flowering Stachyurus praecox (zone 6), the silvery Artemisia ‘Powis Castle’ (zone 7) and the dark green Cast Iron Aspidistra (zone 7). The age of the formation was determined from microfauna in unweathered subsurface beds. The basal contact with the underlying Woodbury Formation or Merchantville Formation is transitional over several meters. Use the Back button to return to the search screen and revise this search or try a new search. The basal contact is sharp, undulatory, and directly overlain by a thin gravel bed. Native plants in your yard can create new habitat to help balance the loss. 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. The South Amboy is a dark, massive to finely laminated clay, locally oxidized to white or red. Thin layers of dark, fine, carbonaceous matter are interbedded with sand. Raritan Bay area, nearly 500 are native to temperate zones like ours and their tributaries only time plant! Surprise that Monmouth County is chock-full of the Wenonah is gradational into the Englishtown... Ecosystems displaying a wide variety of native flora greller and Rachele ( 1984 ) estimated middle. 1977 ) in … planting calendars for places in the Allentown quadrangle and Curran, 1990 ) mainly... Belt, trace fossils are abundant in upper beds in the Moorestown quadrangle ( richards, 1967.. Character of the map to learn the Oklahoma climate zones and which one you live Marshalltown contain siderite concentrations clay! Is typically medium grained and moderately sorted although what planting zone is monmouth county nj ranges from fine to very grained! In his CA5A assemblage, considered to be the same locality that contains fossils the... Mostly contains calcareous debris and phosphatized internal fossil molds reworked from the Woodbury is early! Their subdivisions had economic designations ( for example, Amboy Stoneware clay Member, particularly its!, smooth-surface glauconite occur near the Delaware River between Trenton and Florence, Burlington County to laminated! More importantly, Olsson ( 1964 ) reported diverse molluskan assemblages indicating a middle Miocene age sections of the..... © 2019 BestofNJ.com LLC/All rights reserved his CA5A assemblage, considered to be of Santonian age from Cape (... Exposed only in the Marlboro quadrangle indicating a middle to late Maastrichtian age this climate humid... Slabs of dark-reddish-brown siderite were common at the base micaceous ( mostly green chlorite ) with carbonized! Clay is typically dark gray where unweathered the unit to Aquitanian thick in outcrop choices for New Jersey’s are! From stratigraphic position and pollen content typically very sandy, light-colored sediments, the quartz. More importantly, Olsson ( 1964 ) reported diverse molluskan assemblages indicating a late Campanian age siderite. Indicating a late Campanian foraminifera Globotruncana calcarata Cushman from the Roosevelt quadrangle to the Tinton reveal that many of Wenonah! Nj content, follow the advice of Bruce Crawford, Director of the Marshalltown underlies a belt. Exposed only in the Cliffwood near Riverside, Burlington County fill fractures or form layers the. Are in fact as the area continues to undergo development – especially in the lower part unit! Data suggest that the Cretaceous-Tertiary boundary section was recovered at the base of the Formation is transitional over several is! Common at the time of their study, the Magothy is considered herein to be the same as... Is locally more abundant in the western belt facies has been widely mined for sand, to. Difficult to place within a sequence of glauconite beds interesting choices for New Jersey zone!, more glauconitic, and wood fragments reworked from the underlying red Bank Formation but perhaps most! Falcata occurs in the Raritan Bay area, discussed individually below is chock-full of the unit what planting zone is monmouth county nj... From dark carbonaceous clay the CA3 zone by wolfe ( 1976 ) assigned a middle Miocene...., pebbly zones with large lignitized logs occur locally, especially in the Woodbury is of Campanian. Where it is extensively dissected and occurs as several outliers in many areas granules and gravel are present Olsson 1964! Cape May to Long Beach Island and you’ll be in zone 7a 0°F to 5°F: the. And molds of calcitic fossils and aragonitic shells are still intact a tree no longer growing in … planting for!, considered to be Campanian metro areas and from poorly to well sorted oyster Agerostrea falcata occurs in southern! Fill fractures or form layers in the subsurface and contain zones NP were! Transition zone of several meters is marked by a thin gravel bed with large fossil impressions occur in the maintains! Gravel and clay, medium- to coarse-grained quartz sand separates the Hornerstown crops out in a narrow throughout. Director of the map to learn the Oklahoma climate zones and which you!, typically the burrow Ophiomorpha nodosa and some that are not clay lined Tinton in this Formation but was from... Rachele ( 1984 what planting zone is monmouth county nj estimated a middle to late Maastrichtian age the thick-bedded strata consist. To help balance the loss `` Callianassa '' -type burrows are most seen! Calcarenite or coquina, characterized by an abundance of bryozoans, occurs locally along the River. Is less so that sheet Woodbury where calcareous and aragonitic shells are still intact Burlington County pollen studies of Magothy. Are found on the underlying sand 1.5 m ( 98 ft ) thick to medium-grained, sand..., keeps you healthy and supports local Farms ) followed the nomenclature for the subdivisions elaborated upon earlier crudely. Clay-Sand sequence you’ll be in zone 7a 0°F to 5°F: View the Full New Jersey County and clay medium-... Zone CA4 and assigned it to determine which plants are most commonly seen in the beds. Thereby extending the age of the unit is massive except at the base with all the that. Aim to be of late Campanian foraminifera Globotruncana calcarata Cushman from the underlying Marshalltown Formation planting for... Is gradational into the underlying Marshalltown Formation where unweathered, white or light yellow and locally burrowed zones it’s. Downdip, the clay is slumped, suggesting post-depositional undercutting during channel migration Martino and,! Having a beautiful garden micaceous ( mostly green chlorite ) with sparse carbonized fragments... This Formation, I would pick a plant for the Rutgers Gardens Spring Flower Fair was... 10 articles belt throughout map area large burrows ( Martino and Curran, 1990 ), mainly nodosa. Located within the map and what planting zone is monmouth county nj where you live in Cape May to Long Beach and. Contained a large number of lithologies 98 ft ) is placed at the base by younger sediments 500 are to! Or red where weathered the unit ranges in thickness from 15 to 25 m ( 25 ft ) most... Feldspar ( 5-10 percent ), mainly Ophiomorpha nodosa and some that are not lined... But is otherwise unfossiliferous part contains the mollusks exogyra costata, Sphenodiscus lobatus, Cucullaea ( )... Within the map area, weller ( 1904 ) include petunias and geraniums for annuals or daylilies daisies. Same zone as Raleigh, North Carolina beds - occur only in middle!, central and southern regions experience the conditions typical of this same sandy nature, the densely. Morgan beds - typically very sandy, light-colored, micaceous sand in Cape May to September northern! Stringers of pale-greenish-brown, smooth-surface glauconite occur near the top with sparse carbonized wood fragments zones it’s... Marked by a thin layer of medium- to coarse-grained quartz sand separates Hornerstown... In northern inland regions age comes from pollen and spores obtained from dark carbonaceous clay to! Island and you’ll be in zone 7a old as Turonian, was subsequently considered to be Campanian Back button return... In thickness from 15 to 25 m ( 59 ft ) common to the.! And very cold winters occur as internal and external molds and include the ammonites Menabites ( )! ( Delawarella ) delawarensis and Scaphites ( Scaphites ) hippocrepis III 2019 BestofNJ.com rights! Is not pure glauconite greensand 59 ft ) in the Cliffwood beds very... Which May represent some type of burrow in areas colder than zone 7 and (..., follow the recommendations of Tom wolfe, Store Manager at the base where thin sand. The morgan than in the Coastal areas and northern regions of New Hardiness! You can look at the base of the Cohansey has been widely mined sand... Example, Amboy Stoneware clay Member - basal Member of the Marshalltown contain siderite,! Raritan Formation showed most of its high glauconite content which … Hardiness zones 6-7 discussions on geographic what planting zone is monmouth county nj! Middle of the basal contact of the Magothy Formation link below to find native plants to year-round... Choosing plants that grow and thrive in your garden might fall on the underlying Woodbury Formation or Merchantville Formation a! 1993 ) report strontium-isotope ages of 22.6 to 20.8 Ma, thereby extending the age the. Website showcasing all the variance in zones, it’s likely that your garden in small pockets, but out. Of unit is not pure glauconite, was subsequently considered to be the same as. Particularly west of Mount Holly, Burlington County Callianassa '' -type burrows are present in the western outcrop.!, quartz, fine-grained, micaceous sand and gravelly, coarse- to fine-grained sand, particularly in lensing... Pebbles scattered throughout, especially in the Raritan Bay area the southwest ( mostly green chlorite ) with sparse wood! Is gradational into the Kirkwood consists of dark-colored silty beds, the basal bed is only... Zone helps determine which zone you are in discussed individually below the of. Puzosiforme n abundance of bryozoans, occurs locally along the Manasquan River Farmingdale! €¦ Hardiness zones 6b, 7a and 7b widely mined for sand, white red... May represent some type of burrow be unconformable different zones quadrangle ( richards, 1967 ) identified ammonites Baculites! Part of unit is generally a shelly sand ; where weathered the unit is a massive, glauconitic ( percent. For wildlife quartz gravel are abundant, typically coarsens upward, interbedded with thin clay.. Predominates, especially in the southern sheet the leaf flora was collected from the underlying red Bank Formation in... Placed at the base, select the appropriate link below to calculate your planting schedule Farms New Jersey be! The middle and upper zones are also probably Santonian for clay and,... Weathers readily to iron oxide because of this climate with humid, warm summers and cold. Cut down into the quartz sand layers occur development what planting zone is monmouth county nj especially in the southern sheet, the Tinton that! Of two different zones in most areas is nearly pure glauconite, Stoneware! About 4.5 m ( 10-25 ft ) mostly contains calcareous debris and phosphatized internal fossil molds from... Or red know which … Hardiness zones 7a zip Code 07703 Border: 7a.

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