Rosendale Trestle

Joppenbergh Mountain is a nearly 500-foot (152 m) mountain in Rosendale Village, a hamlet in the town of Rosendale, in Ulster County, New York. The mountain is composed of a carbonate bedrock overlain by glacially deposited material. It was named after Rosendale's founder, Jacob Rutsen, and mined throughout the late 19th century for dolomite that was used in the manufacture of natural cement. Extensive mining caused a large cave-in on December 19, 1899, that destroyed equipment and collapsed shafts within Joppenbergh. Though it was feared that several workers had been killed, the collapse happened while all the miners were outside, eating lunch. Since the collapse, the mountain has experienced shaking and periodic rockfalls. During the late 1930s, Joppenbergh became the site of several ski jumping competitions, which continued until the early 1940s. The original slope was designed by Harold Schelderup for Rosendale's first competition in 1937; Schelderup himself skied that July, after the slope was coated with borax for a summer competition. Several Olympic skiers participated in the competitions. Skiing began again in the 1960s, when a new slope was built on the mountain, and the revived competitions continued until 1971. The town of Rosendale considered buying land near the mountain in 2003 for parking, and the following year, the town leased a tract of land to build a municipal parking lot. Joppenbergh was put up for sale in 2009, and in March 2011, the Open Space Institute (OSI) offered to purchase the entire 117-acre (47 ha) property and sell it to the town. The Rosendale town board initially agreed to the deal the following month, with payment planned to come from a surplus fund. That June, however, the board found that the surplus fund had already been exhausted and could not cover the entire cost of the purchase. Ultimately, the OSI completed its purchase of Joppenbergh in October 2011, without town money.

Rosendale is a town in the center of Ulster County, New York, United States. It once contained a village Rosendale, primarily centered around Main Street, but which was dissolved through vote in 1977. The population was 5,782 at the 2020 census.

The Snyder Estate Natural Cement Historic District is located in the Town of Rosendale, New York, United States. It is a 275-acre (111 ha) tract roughly bounded by Rondout Creek, Binnewater and Cottekill roads and Sawdust Avenue. NY 213 runs through the lower portion of the district, paralleling the dry bed of the Delaware and Hudson Canal. Within the district's bounds are 122 contributing properties representing what remains of five plants that produced Rosendale cement, and the homes and dependencies of the Snyder family, who originally owned the land. They range in age from the bed of the canal, where the cement was discovered in 1825 during construction, to some of the last factories built before production was ended in 1970. Included are not just homes, barns, and factories but mines, reservoirs, and a rail siding. After an aborted attempt to secure National Historic Landmark District status in 1978, the district was added to the National Register of Historic Places in 1992.

Widow Jane Mine is a former cement mine located west of Rosendale, New York. The mine was active from 1825 to 1970 and is now part of the Snyder Estate Natural Cement Historic District. Dolomite extracted from the mine was used to make Rosendale cement which was widely used in the 19th century, contributing to the base of the Statue of Liberty among other structures. Since the closure of Widow Jane Mine in 1970, the unique acoustics of its chambers have led to its use as a performance venue. The Century House Historical Society, which oversees the property, hosts a summer concert series in the mine. An annual Subterranean Poetry Festival is held there as well. It has been used as a recording studio, a venue for plays, and an art exhibition space. 80% of the mine is underwater.

The Rosendale Library, formerly the All Saints' Chapel, is located on Main Street (NY 213) in Rosendale, New York, United States. It was originally built as a Gothic Revival Episcopal church from locally mined Rosendale cement, a material which covers the stonework exterior walls. After floods from nearby Rondout Creek damaged the building in the mid-1950s, the church abandoned it. It also survived a fire in the mid-1970s. A newly formed local library district was created to restore it for use as a library. In 1986 it was added to the National Register of Historic Places.

Rosendale is a hamlet located in the Town of Rosendale in Ulster County, New York, United States. The population was 1,285 at the 2020 census. It was also a census-designated place known as Rosendale Village until 2010, when the U.S. Census Bureau designated it Rosendale Hamlet. Some maps continue to list the place as just Rosendale. As of 2020, the "Hamlet" in the CDP name was dropped.The area was originally settled in the late 17th century by Jacob Rutsen, a merchant from Albany, but did not become a major population center until the 1825 discovery of Rosendale cement in the region; the development of the cement industry, and the growth of the Delaware and Hudson Canal along the Rondout Creek and Main Street, gave rise to substantial economic development in Rosendale. The town's cement was used in the construction of numerous national landmarks. The Wallkill Valley Railroad reached the village in 1871, and its depot in the village was the largest station on the Wallkill Valley line. Rosendale was formally incorporated as a village in 1890. An 1895 fire destroyed half the village, as it had no form of fire protection at that time. Throughout the 20th century, the decline of the natural cement industry caused Rosendale to suffer economically and lose population. The village was also battered by a series of severe floods, and the center of commerce began to shift from Main Street to Route 32. By the 1970s the village was having severe problems with its utilities and tax code, and was no longer producing cement. The hippie movement brought many artists to the village during this time, which led to ideological clashes between the newcomers and the more conservative, established residents. In 1976, the village voted to dissolve itself to solve its municipal problems, and on January 1, 1978, Rosendale became disincorporated. The village's mayor at the time of the vote viewed the dissolution as a work of conceptual art, and published a book on the matter. After the disincorporation, the commercial center of the former village was revitalized by artists and entrepreneurs, who purchased and restored Main Street buildings that had fallen into disrepair. Since the 1990s, Rosendale has hosted many street festivals. The former village has had a number of notable buildings, including four churches. Two notable bridges span the Rondout Creek in the village: a road bridge that carries Route 32, and the Rosendale trestle, a former railroad bridge that was renovated as a pedestrian walkway. Joppenbergh Mountain, named after Rosendale's founder, borders the village and has been the site of numerous ski jumping competitions and mine collapses.

The Binnewater Historic District is a national historic district located at Rosendale in Ulster County, New York, United States. The district originally included nine contributing buildings built during the late 19th and early 20th centuries. They were all frame structures and included a railroad depot, a privy, a general store that was also a post office, a livery stable, two houses, a wagon shed, and two barns. The general store served as an unofficial railroad depot for the Wallkill Valley Railroad from 1875 until 1883, when the railroad constructed the actual station. The station was located too close to Binnewater Road, and was hit repeatedly by trucks. In May 1989, a large piece of the building broke off and fell into the street. The structure was subsequently demolished.The district was listed on the National Register of Historic Places in 1982.Binnewater is known for its many lakes, including Williams Lake, Twin Lakes, and Fourth Lake. Williams Lake used to house Williams Lake Resort. This Resort included a hotel, a restaurant that was open to hotel guests and the public, and a private beach club membership.

Cottekill is a small hamlet in the northwest part of the Town of Rosendale, Ulster County, New York, United States. Located in the Rondout Valley, it is approximately 2.25 miles east of the hamlet of Stone Ridge, 2.5 miles northwest of Rosendale Village, 8.75 miles south of the city of Kingston and 10.9 miles north of the village of New Paltz. As of 2014, the population was listed at 451.

Tillson is a hamlet (and census-designated place) in Ulster County, New York, United States. The population was 1,516 at the 2020 census. Tillson is in the Town of Rosendale, along routes 32 and 213.

High Falls is a hamlet (and census-designated place) in Ulster County, New York, United States. The population was 700 at the 2020 census. Portions of High Falls are located in the towns of Marbletown, Rosendale, and Rochester.

DuBois-Deyo House is a historic home located at Rosendale in Ulster County, New York. It was built about 1750 and is composed of two sections. The main block is a two-story, four-by-two-bay stone and frame building with a two-story frame rear wing. Also on the property is a garage dated to about 1890.The house was purchased by artist Carolee Schneemann in 1964 and became her primary residence until her death in 2019. Many of her artworks were created and filmed in the house, including the film Fuses.It was listed on the National Register of Historic Places in 1994.

The Wallkill River, a tributary of the Hudson, drains Lake Mohawk in Sparta, New Jersey, flowing from there generally northeasterly 88.3 miles (142.1 km) to Rondout Creek in New York, just downstream of Sturgeon Pool, near Rosendale, with the combined flows reaching the Hudson at Kingston. The river is unusual because it flows north between two major south-flowing rivers, the Hudson and the Delaware River. It also has the unusual distinction of being a river that drains into a creek, due to being impounded shortly before the Rondout confluence into a small body of water called Sturgeon Pool near Rifton, and what reaches the Rondout from there is the lesser flow.