The Mantoloking plate. Relief from Copernicus GLO-30; rivers and lakes from USGS NHD; watersheds from the USGS Watershed Boundary Dataset; roads and city limits from Census TIGER 2024.
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3.00 inches of rain fell in two days, the most for this week of the year since records began in 1907. The next wettest, 2.83 inches, fell in 1920.
Mantoloking’s center stands about 7 ft above sea level. Within three miles the land runs from 0 ft to 50 ft, a difference of 50 ft: nearly flat ground. Open water lies within three miles.
The section below crosses 2 rock units mapped at the surface.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 64×. The colored band under the surface is the rock the state geologic map shows at the surface, not a picture of what lies beneath.
Clay, sand. Age: Early Miocene, 16 to 23 million years old. About 10 mi of the line.
Sand. Age: Middle Miocene, 12 to 14 million years old. About 1 mi of the line.
From the USGS State Geologic Map Compilation (Horton and others, 2017), the states’ geologic maps joined at a common scale.
Heights from Copernicus GLO-90 (a surface model: it includes buildings and tree canopy); summits from USGS GNIS; rivers from USGS NHDPlus HR; rock from the USGS State Geologic Map Compilation.
Rain that falls on Mantoloking runs straight into the Atlantic Ocean.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Mantoloking; river miles along the main stem, rounded.
Mantoloking has a humid subtropical climate. Summer afternoons average 84° in July; winter nights fall to about 25° in January. About 52 inches of rain fall in a normal year.
On November 14 Mantoloking normally reaches 56° and falls to 38°. The record high is 72°, in 1973; the record low 18°, in 1986. The most rain on this date, 2.24 in, fell in 1972.
Normals 1991–2020 and records since 1907 at Long Branch-Oakhurst, 18 miles north. NOAA, through RCC-ACIS.
