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Te Kawa

Te Kawa is a rural community in the Ōtorohanga District and Waikato region of New Zealand's North Island. It lies just to the south of the volcanic hills of Kakepuku and Te Kawa. Until the swamp was drained in the 1900s, Te Kawa was well known for its eels.

Demographics
Te Kawa locality covers . The locality is part of the larger Te Kawa statistical area. Te Kawa locality had a population of 453 in the 2023 New Zealand census, a decrease of 51 people (−10.1%) since the 2018 census, and an increase of 33 people (7.9%) since the 2013 census. There were 243 males and 216 females in 153 dwellings. 1.3% of people identified as LGBTIQ+. There were 117 people (25.8%) aged under 15 years, 69 (15.2%) aged 15 to 29, 216 (47.7%) aged 30 to 64, and 54 (11.9%) aged 65 or older. Te Kawa statistical area Te Kawa statistical area, which also includes Kio Kio, covers . It had an estimated population of as of with a population density of people per km2. Te Kawa statistical area had a population of 1,182 in the 2023 New Zealand census, a decrease of 27 people (−2.2%) since the 2018 census, and an increase of 108 people (10.1%) since the 2013 census. There were 606 males, 576 females, and 3 people of other genders in 411 dwellings. 1.5% of people identified as LGBTIQ+. The median age was 35.6 years (compared with 38.1 years nationally). There were 285 people (24.1%) aged under 15 years, 201 (17.0%) aged 15 to 29, 546 (46.2%) aged 30 to 64, and 150 (12.7%) aged 65 or older. == Te Kawa hill ==
Te Kawa hill
Te Kawa hill is high and just to the north of the village. The 'Geology of the Waikato Area' says, "The Alexandra Volcanic Group consists of several low-angle composite cones, including Karioi, Pirongia, Kakepuku, Te Kawa and Tokanui volcanoes, aligned southeast from Mount Karioi on the coast to Tokanui." It was formed in the Late Pliocene to earliest Pleistocene of subduction-related basaltic magmas. Te Kawa is the only Alexandra Volcanic with a crater remaining. Outcrops of coarse tuff and lapilli tuff are on the north and northeast sides of the crater and basalt boulders with augite megacrysts in the crater. There is a site on the south side of the crater, There are also several pits and terraces. == See also ==
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